232 results on '"Gusev Y."'
Search Results
2. Effects of frozen soil on soil temperature, spring infiltration, and runoff: Results from the PILPS 2(d) experiment at Valdai, Russia
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Luo, L F, Robock, A, Vinnikov, K Y, Schlosser, C A, Slater, A G, Boone, A, Braden, H, Cox, P, de Rosnay, P, Dickinson, R E, Dai, Y J, Duan, Q Y, Etchevers, P, Henderson-Sellers, A, Gedney, N, Gusev, Y M, Habets, F, Kim, J W, Kowalczyk, E, Mitchell, K, Nasonova, O N, Noilhan, J, Pitman, A J, Schaake, J, Shmakin, A B, Smirnova, T G, Wetzel, P, Xue, Yongkang K, Yang, Z L, and Zeng, Q C
- Abstract
The Project for Intercomparison of Land-Surface Parameterization Schemes phase 2(d) experiment at Valdai, Russia, offers a unique opportunity to evaluate land surface schemes, especially snow and frozen soil parameterizations. Here, the ability of the 21 schemes that participated in the experiment to correctly simulate the thermal and hydrological properties of the soil on several different timescales was examined. Using observed vertical profiles of soil temperature and soil moisture, the impact of frozen soil schemes in the land surface models on the soil temperature and soil moisture simulations was evaluated. It was found that when soil-water freezing is explicitly included in a model, it improves the simulation of soil temperature and its variability at seasonal and interannual scales. Although change of thermal conductivity of the soil also affects soil temperature simulation, this effect is rather weak. The impact of frozen soil on soil moisture is inconclusive in this experiment due to the particular climate at Valdai, where the top 1 m of soil is very close to saturation during winter and the range for soil moisture changes at the time of snowmelt is very limited. The results also imply that inclusion of explicit snow processes in the models would contribute to substantially improved simulations. More sophisticated snow models based on snow physics tend to produce better snow simulations, especially of snow ablation. Hysteresis of snow-cover fraction as a function of snow depth is observed at the catchment but not in any of the models.
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- 2003
3. FEATURES OF VENTILATION OF ARC WELDING WORKPLACES IN SMALL ROOMS
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Shaptala, V., primary, Hukalenko, E., primary, Severin, N., primary, and Gusev, Y., primary
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- 2022
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4. On the integral law of thermal radiation
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Gusev, Y. V.
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- 2014
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5. The Rhône-Aggregation Land Surface Scheme Intercomparison Project : An Overview
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Boone, A., Habets, F., Noilhan, J., Clark, D., Dirmeyer, P., Fox, S., Gusev, Y., Haddeland, I., Koster, R., Lohmann, D., Mahanama, S., Mitchell, K., Nasonova, O., Niu, G.-Y., Pitman, A., Polcher, J., Shmakin, A. B., Tanaka, K., van den Hurk, B., Vérant, S., Verseghy, D., Viterbo, P., and Yang, Z.-L.
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- 2004
6. Magnetized boxes for housing polarized spins in homogeneous fields
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Hiebel, S., Großmann, T., Kiselev, D., Schmiedeskamp, J., Gusev, Y., Heil, W., Karpuk, S., Krimmer, J., Otten, E.W., and Salhi, Z.
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- 2010
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7. Cabauw Experimental Results from the Project for Intercomparison of Land-Surface Parameterization Schemes
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Chen, T. H., Henderson-Sellers, A., Milly, P. C. D., Pitman, A. J., Beljaars, A. C. M., Polcher, J., Abramopoulos, F., Boone, A., Chang, S., Chen, F., Dai, Y., Desborough, C. E., Dickinson, R. E., Dümenil, L., Ek, M., Garratt, J. R., Gedney, N., Gusev, Y. M., Kim, J., Koster, R., Kowalczyk, E. A., Laval, K., Lean, J., Lettenmaier, D., Liang, X., Mahfouf, J.-F., Mengelkamp, H.-T., Mitchell, K., Nasonova, O. N., Noilhan, J., Robock, A., Rosenzweig, C., Schaake, J., Schlosser, C. A., Schulz, J.-P., Shao, Y., Shmakin, A. B., Verseghy, D. L., Wetzel, P., Wood, E. F., Xue, Y., Yang, Z.-L., and Zeng, Q.
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- 1997
8. Performance studies of a full-length prototype for the CASTOR forward calorimeter at the CMS experiment
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Andreev, V., Aslanoglou, X., Azman, A., Bakirci, M. N., Başeğmez, S., Beaumont, W., Blocki, J., Borras, K., Campbell, A., Çerçi, S., d’Enterria, D., de Silva, M., Dumanoğlu, I., Erturk, S., Eskut, E., Ershov, Y., Göttlicher, P., Gouskos, L., Onengut, G., Gusev, Y., Jung, H., Katkov, I., Katsas, P., Khein, L., Kisoglu, F., Knutsson, A., Kuleshov, S., Kuznetsov, A., Lebeau, M., McCauley, T., Muhl, C., Musienko, Y., Ochesanu, S., Oroku, M., Ozdemir, K., Ozturk, S., Panagiotou, A. D., Reucroft, S., Ripert, M., Shileev, K., Sogut, K., Swain, J., Tiflov, V., Kayis-Topaksu, A., Van Haevermaet, H., Van Mechelen, P., and de Wolf, E.
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- 2010
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9. MATS and LaSpec: High-precision experiments using ion traps and lasers at FAIR
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Rodríguez, D., Blaum, K., Nörtershäuser, W., Ahammed, M., Algora, A., Audi, G., Äystö, J., Beck, D., Bender, M., Billowes, J., Block, M., Böhm, C., Bollen, G., Brodeur, M., Brunner, T., Bushaw, B.A., Cakirli, R.B., Campbell, P., Cano-Ott, D., Cortés, G., Crespo López-Urrutia, J.R., Das, P., Dax, A., De, A., Delheij, P., Dickel, T., Dilling, J., Eberhardt, K., Eliseev, S., Ettenauer, S., Flanagan, K.T., Ferrer, R., García-Ramos, J.-E., Gartzke, E., Geissel, H., George, S., Geppert, C., Gómez-Hornillos, M.B., Gusev, Y., Habs, D., Heenen, P.-H., Heinz, S., Herfurth, F., Herlert, A., Hobein, M., Huber, G., Huyse, M., Jesch, C., Jokinen, A., Kester, O., Ketelaer, J., Kolhinen, V., Koudriavtsev, I., Kowalska, M., Krämer, J., Kreim, S., Krieger, A., Kühl, T., Lallena, A.M., Lapierre, A., Le Blanc, F., Litvinov, Y.A., Lunney, D., Martínez, T., Marx, G., Matos, M., Minaya-Ramirez, E., Moore, I., Nagy, S., Naimi, S., Neidherr, D., Nesterenko, D., Neyens, G., Novikov, Y.N., Petrick, M., Plaß, W.R., Popov, A., Quint, W., Ray, A., Reinhard, P.-G., Repp, J., Roux, C., Rubio, B., Sánchez, R., Schabinger, B., Scheidenberger, C., Schneider, D., Schuch, R., Schwarz, S., Schweikhard, L., Seliverstov, M., Solders, A., Suhonen, M., Szerypo, J., Taín, J.L., Thirolf, P.G., Ullrich, J., Van Duppen, P., Vasiliev, A., Vorobjev, G., Weber, C., Wendt, K., Winkler, M., Yordanov, D., and Ziegler, F.
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- 2010
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10. Radiation-hard photodetectors based on fine-mesh phototubes for calorimetry in very forward rapidity
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Gusev, Y., Lukianov, V., Mamaeva, G., Musienko, Y., Reucroft, S., Seliverstov, D., Shusterman, L., and Swain, J.
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- 2007
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11. In silico evaluation of the integration of Agrobacterium VirE2 protein into a lipid membrane: SW06.W29–17
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Gusev, Y., Masilov, S., Volokhina, I., and Chumakov, M.
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- 2013
12. DEVICES AND VENTILATION PROCESS DURING EXECUTION ELECTRIC WELDING
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Shaptala, V., primary, Hukalenko, E., primary, Severin, N., primary, and Gusev, Y., primary
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- 2020
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13. Ras oncogene-transformed and nontransformed cell populations are each heterogeneous but respond differently to the chemotherapeutic drug cytosine arabinoside (Ara-C)
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Axelrod, D. E., Gusev, Y., and Gamel, John W.
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- 1997
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14. Using Battery Energy Storage Systems for Load Balancing and Reactive Power Compensation in Distribution Grids
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Gusev, Y. P., primary and Subbotin, P. V., additional
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- 2019
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15. Cabauw Experimental Results from the Project for Intercomparison of Land-Surface Parameterization Schemes
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Chen, Tian Hong, Henderson-Sellers, A, Milly, P. C. D, Pitman, A. J, Beljaars, A. C. M, Polcher, J, Abramopoulos, F, Boone, A, Chang, S, Chen, F, Dai, Y, Desborough, C. E, Dickinson, R. E, Duemenil, L, Ek, M, Garratt, J. R, Gedney, N, Gusev, Y. M, Kim, J, and Koster, R
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Meteorology And Climatology - Abstract
In the Project for Intercomparison of Land-Surface Parameterization Schemes phase 2a experiment, meteorological data for the year 1987 from Cabauw, the Netherlands, were used as inputs to 23 land-surface flux schemes designed for use in climate and weather models. Schemes were evaluated by comparing their outputs with long-term measurements of surface sensible heat fluxes into the atmosphere and the ground, and of upward longwave radiation and total net radiative fluxes, and also comparing them with latent heat fluxes derived from a surface energy balance. Tuning of schemes by use of the observed flux data was not permitted. On an annual basis, the predicted surface radiative temperature exhibits a range of 2 K across schemes, consistent with the range of about 10 W/m in predicted surface net radiation. Most modeled values of monthly net radiation differ from the observations by less than the estimated maximum monthly observational error (+/- 10 W/sq m). However, modeled radiative surface temperature appears to have a systematic positive bias in most schemes; this might be explained by an error in assumed emissivity and by models' neglect of canopy thermal heterogeneity. Annual means of sensible and latent heat fluxes, into which net radiation is partitioned, have ranges across schemes of 30 W/sq m and 25 W/sq m, respectively. Annual totals of evapotranspiration and runoff, into which the precipitation is partitioned, both have ranges of 315 mm. These ranges in annual heat and water fluxes were approximately halved upon exclusion of the three schemes that have no stomatal resistance under non-water-stressed conditions. Many schemes tend to underestimate latent heat flux and overestimate sensible heat flux in summer, with a reverse tendency in winter. For six schemes, root-mean-square deviations of predictions from monthly observations are less than the estimated upper bounds on observation errors (5 W/m for sensible beat flux and 10 W/m for latent heat flux). Actual runoff at the site is believed to be dominated by vertical drainage to ground water, but several schemes produced significant amounts of runoff as overland flow or interflow. There is a range across schemes of 184 mm (40% of total pore volume) in the simulated annual mean root-zone soil moisture. Unfortunately, no measurements of soil moisture were available for model evaluation. A theoretical analysis suggested that differences in boundary conditions used in various schemes are not sufficient to explain the large variance in soil moisture. However, many of the extreme values of soil moisture could be explained in terms of the particulars of experimental setup or excessive evapotranspiration.
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- 1997
16. Long-term dynamics of chromosomal instability in cancer: A transition probability model
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Gusev, Y., Kagansky, V., and Dooley, W.C.
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- 2001
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17. Electrochemical Sensors for Vanadium Determination
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Gogol E., Denisov E., Lunev I., Egorova O., Sharipova L., and Gusev Y.
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Voltammogram ,Volume Glassy-Carbon Electrode ,Vadium (V) ,Screen Printed Carbon Electrode - Abstract
© Published under licence by IOP Publishing Ltd. This paper is dedicated to the problem of vanadium (V) determination by the means of voltammetry. The comparison of results obtained for two types of sensor: volume glassy-carbon electrode and screen printed carbon electrode are presented. The experimental data is recorded using the hardware and software of Novocontrol (Germany): electrochemical interface POT/GAL 15V 10A, frequency response analyzer Alpha-A, and software for data collection and data processing WinDETA. Two three-electrode cells has been studied: for the first one the bulk glassy carbon electrode, and for the second one the screen printed electrodes has been used as the working electrode. In the first case the reference electrode has been made from silver chloride and the counter electrode from steel wire. In case of the screen printed electrodes, the electrodes were placed on the same plate. The peak of vanadium (V) was obtained under the potential of 1.3 V. It was found that the growth of the vanadium concentration increases magnitude of the cathode current measured then the mentioned potential is applied. The screen printed carbon electrodes provides better sensitivity in comparison with the volume glassy-carbon electrodes due to the more explicit vanadium potential peak.
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- 2017
18. Modeling Surface Runoff and Water Fluxes over Contrasted Soils in the Pastoral Sahel : Evaluation of the ALMIP2 Land Surface Models over the Gourma Region in Mali
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Grippa, Manuela, Gal, Laetitia, Anderson, Martha, Ait-Mesbah, S., Polcher, Jan, Balsamo, G., Boussetta, S., Dutra, Emanuel, Pappenberger, F., Hain, Christopher, Boone, Aaron, Favot, F., Guichard, F., Kaptue, A., Roujean, Jean-Louis, Cappelaere, Bernard, Demarty, Jérôme, Peugeot, Christophe, Séguis, L., Velluet, C., Chaffard, V., Cohard, J. M., Gascon, T., Galle, S., Hector, B., Lebel, T., Pellarin, T., Richard, A., Quantin, G., Vischel, T., Chan, E., Verseghy, D., Ducharne, Agnès, Magand, C., Getirana, A., Hiernaux, Pierre, Kergoat, Laurent, Mougin, Éric, Pierre, Caroline, Gusev, Y., Nasonova, O., Harris, P., He, X., Yorozu, K., Kotsuki, S., Tanaka, K., Kim, H., Oki, T., Kumar, S., Lo, M.-H., Mahanama, S., Maignan, F., Ottlé, C., Mamadou, O., Shmakin, A., Sokratov, V., Turkov, D., Working Group, Almip2, Géosciences Environnement Toulouse (GET), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), United States Department of Agriculture, European Centre for Medium-Range Weather Forecasts (ECMWF), Laboratoire de mesure du carbone 14 (LMC14 - UMS 2572), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut de Radioprotection et de Sûreté Nucléaire (IRSN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS), Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Hydrosciences Montpellier (HSM), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS), Structure et fonctionnement des systèmes hydriques continentaux (SISYPHE), Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Mines Paris - PSL (École nationale supérieure des mines de Paris), Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Centre d'études spatiales de la biosphère (CESBIO), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Modélisation des Surfaces et Interfaces Continentales (MOSAIC), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS)-Observatoire Midi-Pyrénées (OMP), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Institut de Recherche pour le Développement (IRD)-Centre National d'Études Spatiales [Toulouse] (CNES), Groupe d'étude de l'atmosphère météorologique (CNRM-GAME), Institut national des sciences de l'Univers (INSU - CNRS)-Météo France-Centre National de la Recherche Scientifique (CNRS), Institut de Recherche pour le Développement (IRD)-Université Montpellier 2 - Sciences et Techniques (UM2)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Université Fédérale Toulouse Midi-Pyrénées-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS), Université Pierre et Marie Curie - Paris 6 (UPMC)-École pratique des hautes études (EPHE)-MINES ParisTech - École nationale supérieure des mines de Paris-Centre National de la Recherche Scientifique (CNRS), NASA Goddard Space Flight Center (GSFC), Centre National d'Études Spatiales [Toulouse] (CNES)-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), Institut de Recherche pour le Développement (IRD)-Université Montpellier 2 - Sciences et Techniques (UM2)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Météo France-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Université Montpellier 2 - Sciences et Techniques (UM2)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS), Université Pierre et Marie Curie - Paris 6 (UPMC)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-MINES ParisTech - École nationale supérieure des mines de Paris, Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Université Fédérale Toulouse Midi-Pyrénées-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Météo France-Centre National de la Recherche Scientifique (CNRS), Earth Systems Science Interdisciplinary Center, University of Maryland [College Park], University of Maryland System-University of Maryland System, and Institut de Recherche pour le Développement (IRD)-Université Montpellier 2 - Sciences et Techniques (UM2)-Centre National de la Recherche Scientifique (CNRS)-Université de Montpellier (UM)
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Atmospheric Science ,010504 meteorology & atmospheric sciences ,0208 environmental biotechnology ,Mesoscale meteorology ,02 engineering and technology ,Monsoon ,01 natural sciences ,Evapotranspiration ,[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences ,2. Zero hunger ,Hydrology ,Multidisciplinary analysis ,15. Life on land ,[SDE.ES]Environmental Sciences/Environmental and Society ,6. Clean water ,020801 environmental engineering ,Water resources ,13. Climate action ,Soil water ,[SDE]Environmental Sciences ,Environmental science ,Surface runoff ,Surface water - Abstract
Land surface processes play an important role in the West African monsoon variability. In addition, the evolution of hydrological systems in this region, and particularly the increase of surface water and runoff coefficients observed since the 1950s, has had a strong impact on water resources and on the occurrence of floods events. This study addresses results from phase 2 of the African Monsoon Multidisciplinary Analysis (AMMA) Land Surface Model Intercomparison Project (ALMIP2), carried out to evaluate the capability of different state-of-the-art land surface models to reproduce surface processes at the mesoscale. Evaluation of runoff and water fluxes over the Mali site is carried out through comparison with runoff estimations over endorheic watersheds as well as evapotranspiration (ET) measurements. Three remote-sensing-based ET products [ALEXI, MODIS, and Global Land Evaporation Amsterdam Model (GLEAM)] are also analyzed. It is found that, over deep sandy soils, surface runoff is generally overestimated, but the ALMIP2 multimodel mean reproduces in situ measurements of ET and water stress events rather well. However, ALMIP2 models are generally unable to distinguish among the two contrasted hydrological systems typical of the study area. Employing as input a soil map that explicitly represents shallow soils improves the representation of water fluxes for the models that can account for their representation. Shallow soils are shown to be also quite challenging for remote-sensing-based ET products, even if their effect on evaporative loss was captured by the diagnostic thermal-based ALEXI. A better representation of these soils, in soil databases, model parameterizations, and remote sensing algorithms, is fundamental to improve the estimation of water fluxes in this part of the Sahel.
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- 2017
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19. The low-temperature dynamic crossover in the dielectric relaxation of ice Ih
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Popov I., Lunev I., Khamzin A., Greenbaum A., Gusev Y., and Feldman Y.
- Abstract
© 2017 the Owner Societies. Based on the idea of defect migration as the principal mechanism in the dielectric relaxation of ice I h , the concept of low-temperature dynamic crossover was proposed. It is known that at high temperatures, the diffusion of Bjerrum and ionic defects is high and their movement may be considered to be independent. Simple switching between these two mechanisms leads to a dynamic crossover at ∼235 K. By introducing coupling between the Bjerrum and ionic defects, it is possible to describe the smooth bend in the relaxation time at low temperatures in ice I h . However, because the mobility of Bjerrum orientation defects slows down at low temperatures, they may create blockages for proton hopping. The trapping of ionic defects by L-D defects for a long period of time leads to an increase in the relaxation time and causes a low-temperature crossover. This model was validated by experimental dielectric measurements using various temperature protocols.
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- 2017
20. A stochastic model of chromosome segregation errors with reference to cancer cells
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Gusev, Y, Kagansky, V, and Dooley, W.C
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- 2000
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21. Influence of Out-of-Phase of Synchronous Generators on Short-Circuit Currents in Power Systems
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Kayumov, A. G., primary, Gusev, Y. P., additional, and Govorin, V. V., additional
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- 2018
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22. Generation of an oscillating chemical reaction in a heterogeneous system by the oxidation of an alkaline solution of luminol with sodium(vi) ferrate in the presence of copper ions
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Stoupine, D. Yu., Gusev, Y. K., and Lachkova, D. V.
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- 2001
- Full Text
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23. Recent upgrades of the SHIPTRAP setup : On the finish line towards direct mass spectroscopy of superheavy elements
- Author
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Giacoppo, F., Blaum, K., Block, M, Poudyal Chhetri, Meen, Düllmann, Ch. E., Droese, C., Eliseev, S., Filianin, P., Götz, Sebastian, Gusev, Y., Herfurth, F., Hessberger, F. P., Kaleja, O., Khuyagbaatar, J., Laatiaoui, M., Lautenschläger, F., Lorenz, C., Marx, G., Minaya Ramirez, E., Mistry, A. K., Novikov, Yu. N., Plass, W. R., Raeder, S., Rodríguez, D., Rudolph, D., Sarmiento, L. G., Scheidenberger, C, Schweikhard, L., Thirolf, P., Yakushev, A., Giacoppo, F., Blaum, K., Block, M, Poudyal Chhetri, Meen, Düllmann, Ch. E., Droese, C., Eliseev, S., Filianin, P., Götz, Sebastian, Gusev, Y., Herfurth, F., Hessberger, F. P., Kaleja, O., Khuyagbaatar, J., Laatiaoui, M., Lautenschläger, F., Lorenz, C., Marx, G., Minaya Ramirez, E., Mistry, A. K., Novikov, Yu. N., Plass, W. R., Raeder, S., Rodríguez, D., Rudolph, D., Sarmiento, L. G., Scheidenberger, C, Schweikhard, L., Thirolf, P., and Yakushev, A.
- Abstract
With the Penning-trap mass spectrometer SHIPTRAP at GSI, Darmstadt, it is possible to investigate exotic nuclei in the region of the heaviest elements. Few years ago, challenging experiments led to the direct measurements of the masses of neutron-deficient isotopes with Z = 102; 103 around N = 152. Thanks to recent advances in cooling and ion-manipulation techniques, a major technical upgrade of the setup has been recently accomplished to boost its efficiency. At present, the gap to reach more rare and shorter-lived species at the limits of the nuclear landscape has been narrowed.
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- 2017
24. Study of polylactic acid electret by dielectric spectroscopy
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Galikhanov E., Lounev I., Guzhova A., Gusev Y., Galikhanov M., and Vasilyeva M.
- Abstract
© 2016 AIP Publishing LLC.Correlation between the electret and dielectric properties of the PLA samples charged at different conditions was studied. Electret state of polylactic acid characterized by macromolecule segmental orientation is reflected on dielectric spectra that were used to calculate relaxation energy.
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- 2016
25. Dielectric spectroscopy of amino alcohols at low temperatures
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Solonina I., Vasilyeva M., Greenbaum A., Gusev Y., Lounev I., Rodnikova M., and Feldman Y.
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activation energy ,spatial network of hydrogen bonds ,glass transition ,conductivity ,amino alcohols ,relaxation processes ,dielectric spectroscopy - Abstract
© 2016 Pleiades Publishing, Ltd. The dielectric properties of three vicinal amino alcohols are studied at temperatures in the range of -140-70°C and the frequency interval of 0.1 Hz to 1 MHz. The temperature dependences of the observed relaxation processes indicate both glass transition and melting processes. The relatively high conductivity of the samples was considered from the viewpoint of proton conductivity through a network of hydrogen bonds of amino alcohol molecules.
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- 2016
26. Study of electret state in polylactic acid with nanosized filler by dielectric spectroscopy
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Guzhova A., Lounev I., Galikhanov M., Gusev Y., Vasilyeva M., and Galikhanov E.
- Abstract
© 2016 Author(s).Dielectric spectroscopy method was implemented to study electret state in both polylactic acid and its composites with nano-sized aerosil. Two components of the activation energy for the dielectric relaxation process, related to glass transition and segmental mobility of the macromolecules, were obtained. The lifetime and thermal stability of the electret state increased due to the addition of the filler. The optimal SiO2 content for negative corona electrets was found to be 4 wt. %.
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- 2016
27. Recent Upgrades of the SHIPTRAP Setup: On the Finish Line Towards Direct Mass Spectroscopy of Superheavy Elements
- Author
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Giacoppo, F., primary, Blaum, K., additional, Block, M., additional, Chhetri, P., additional, Düllmann, Ch.E., additional, Droese, C., additional, Eliseev, S., additional, Filianin, P., additional, Götz, S., additional, Gusev, Y., additional, Herfurth, F., additional, Hessberger, F.P., additional, Kaleja, O., additional, Khuyagbaatar, J., additional, Laatiaoui, M., additional, Lautenschläger, F., additional, Lorenz, C., additional, Marx, G., additional, Minaya Ramirez, E., additional, Mistry, A., additional, Novikov, Yu.N., additional, Plass, W.R., additional, Raeder, S., additional, Rodríguez, D., additional, Rudolph, D., additional, Sarmiento, L.G., additional, Scheidenberger, C., additional, Schweikhard, L., additional, Thirolf, P., additional, and Yakushev, A., additional
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- 2017
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28. The percolation phenomenon and fractal dimension of natural silicates
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Vasilyeva M., Gusev Y., Shtyrlin V., and Osin Y.
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Dielectric spectroscopy ,Adsorbed water ,Silicates ,Exchangeable cations ,Percolation ,Fractal dimension - Abstract
© (2015) Trans Tech Publications, Switzerland. Many physical effects, such as dc conductivity and percolation, depend on the morphology of the silicate structure and its relationship to adsorbed water. These effects play an important role in numerous technological applications, in geology, oil-extracting industry, and other practical fields. In this study, all the samples: natural montmorillonite, kaolinite, and ?linoptilolite with different exchangeable cations in their structures, - were stored in ambient air humidity. The investigation was carried by using two separate techniques, namely Dielectric Spectroscopy and a fractal analysis of electron micrographs. The aims of this work were to analyze the complex relaxation behavior of the relaxation process in temperature range -70°C ÷ 70°C and to determine the fractal dimensions of silicates from the dielectric response at percolation. Dielectric measurements in the frequency range of 1 Hz ÷ 1 MHz were performed using a BDS 80 Dielectric Spectrometer based on an Alpha Impedance Analyzer (Novocontrol). The micrographs were analyzed using a special Matlab based program. The analysis of aspects of the dielectric relaxation spectra related to percolation was used for the determination of the numerical characteristics of geometric heterogeneity of natural silicates. The percolation temperatures of the studied samples were determined. The percolation phenomenon in the silicates is related to the transfer of the electric excitation within the developed network of open pores due to the migration of protons and ions along the surface of connected pores on the outer surfaces of the granules. The analysis of these processes allows one to extract the fractal dimensions associated with the migration of charge carriers within the porous medium. Fractal dimensions of the silicates calculated in two ways: from dielectric spectroscopy study and from fractal analysis of the micrographs, - are in good agreement with each other. It was demonstrated that conventional method of the spatial fractal dimension determination using fractal analysis of electron micrographs leads to overestimation in the case of spatial fractal bounded by a surface fractal. The dielectric spectroscopy method is free from such overestimation.
- Published
- 2015
29. Dielectric relaxation of water in clay minerals
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Vasilyeva M., Gusev Y., Shtyrlin V., Greenbaum Gutina A., Puzenko A., Ishai P., and Feldman Y.
- Subjects
Dielectric Spectroscopy ,Kaolinite ,Adsorbed Water ,Fractal Dimension ,Exchangeable Cations ,Montmorillonite - Abstract
The study of confined water dynamics in clay minerals is a very important topic in aluminosilicate-surface chemistry. Aluminosilicates are among the most technologically versatile materials in industry today. Dielectric spectroscopy is a very useful method for investigating the structure and dynamics of water adsorbed on solid matrix surfaces and water in the vicinity of ions in solutions. Use of this method for the study of clay minerals has been underutilized to date, however. The main goal of the present research was to understand the relaxation mechanisms of water molecules interacting with different hydration centers in clay minerals, with a view to eventually control this interaction. Two types of natural layered aluminosilicates (clay minerals) montmorillonite with exchangeable K+, Co2+, and Ni2+ cations and kaolinite with exchangeable K+ and Ba2+ cations were examined by means of dielectric spectroscopy over wide ranges of temperature (from -121°C to +300°C) and frequency (1 Hz-1 MHz). An analysis of the experimental data is provided in terms of four distributed relaxation processes. The low-temperature relaxation was observed only in montmorillonites and could be subdivided into two processes, each related to a specific hydration center. The cooperative behavior of water at the interface was observed in the intermediate temperature region, together with a proton percolation. The dielectric properties of ice-like and confined water structures in the layered clay minerals were compared with the dielectric response observed in porous glasses. The spatial fractal dimensions of the porous aluminosilicates were calculated by two separate methods - from an analysis of the fractality found in photomicrographs and from the dielectric response.
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- 2014
30. The variety of states of adsorbed water in heterogeneous materials and their dielectric response
- Author
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Feldman Y., Puzenko A., Ishai P., Greenbaum A., Segev Y., Vasilyeva M., and Gusev Y.
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Porous Glasses ,Adsorbed Water ,Cole-Cole Spectral Function ,Anomalous Diffusion ,Dielectric Relaxation - Abstract
Whenever water interacts with another dipolar or charged entity, there exists a broadening of its dielectric relaxation peak. Often this broadening can be described by the phenomenological Cole-Cole (CC) spectral function. A new approach has been recently presented (A. Puzenko, P. Ben Ishai, and Y. Feldman, Phys. Rev. Letters 105, 037601-4 (2010)), which is based on the fractal nature of the time set of the interaction of the relaxing water dipoles with their encompassing matrix. It demonstrates a fundamental connection between the relaxation time, τ, the broadening parameter, α, and the Kirkwood-Froehlich correlation function B. The parameters B, τ and α were chosen as the coordinates of the new 3D space, wherein the evolution of the relaxation process, as a result of the variation of external macroscopic parameters (temperature, pressure etc.), will depict a trajectory. This trajectory is a result of the connection between the kinetic and the structural properties of water in the complex system. © 2013 American Institute of Physics.
- Published
- 2013
31. Two types of adsorbed water in natural montmorillonites at low temperatures by dielectric spectroscopy
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Vasilyeva M., Gusev Y., and Shtyrlin V.
- Abstract
Dielectric spectroscopy was applied to natural clay mineral - montmorillonite with the exchangeable K+ and Ni2+ cations where the effect of water adsorption in the samples on the dielectric response was examined in the temperature from -115°C to -75°C and frequency from 1 Hz to 1 MHz ranges. Two relaxation processes (1 and 2) were revealed. The process 1 was related to the adsorbed ordered water structures formed on the interior surface of interlayer channels while the relaxation process 2 was attributed to the disordered water structures built between two surface water monolayers.
- Published
- 2012
32. Ability of a land surface model to predict climate induced changes in northern Russian river runoff during the 21st century
- Author
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Nasonova, O. N., primary, Gusev, Y. M., additional, Volodin, E. M., additional, and Kovalev, E. E., additional
- Published
- 2015
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33. Performance studies of a full-length prototype for the CASTOR forward calorimeter at the CMS experiment
- Author
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Andreev, V. Aslanoglou, X. Azman, A. Bakirci, M.N. Başeǧmez, S. Beaumont, W. Blocki, J. Borras, K. Campbell, A. Çerçi, S. d'Enterria, D. de Silva, M. Dumanoǧlu, I. Erturk, S. Eskut, E. Ershov, Y. Göttlicher, P. Gouskos, L. Onengut, G. Gusev, Y. Jung, H. Katkov, I. Katsas, P. Khein, L. Kisoglu, F. Knutsson, A. Kuleshov, S. Kuznetsov, A. Lebeau, M. McCauley, T. Muhl, C. Musienko, Y. Ochesanu, S. Oroku, M. Ozdemir, K. Ozturk, S. Panagiotou, A.D. Reucroft, S. Ripert, M. Shileev, K. Sogut, K. Swain, J. Tiflov, V. Kayis-Topaksu, A. Van Haevermaet, H. Van Mechelen, P. de Wolf, E.
- Subjects
Physics::Instrumentation and Detectors ,Physics::Accelerator Physics ,High Energy Physics::Experiment - Abstract
We present performance studies of a full-length prototype for the CASTOR quartz-tungsten sampling calorimeter, installed in the very forward region of the CMS experiment at the LHC. The response linearity and energy resolution, the uniformity, as well as the showers' spatial properties in the prototype have been studied with electrons, pions and muons of various energies. A special study was also carried out for testing the light-output with a 90-degree cut of the quartz plates of the calorimeter. The data were taken during the CASTOR test beam at CERN/SPS in 2007. © 2010 The Author(s).
- Published
- 2010
34. The AMMA Land Surface Model Intercomparison Project (ALMIP)
- Author
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Boone , A., De Rosnay , P., Balsamo , G., Beljaars , A., Chopin , F., Decharme , B., Delire , C., Ducharne , Agnès, Gascoin , S., Guichard , F., Gusev , Y., Harris , P., Jarlan , L., Kergoat , L., Mougin , E., Nasonova , O., Norgaard , A., Orgeval , T., Ottlé , C., Poccard-Leclercq , Isabelle, Polcher , J., Sandholt , I., Saux-Picart , S., M. Taylor , C., Xue , Y., Groupe d'étude de l'atmosphère météorologique ( CNRM-GAME ), Institut national des sciences de l'Univers ( INSU - CNRS ) -Météo France-Centre National de la Recherche Scientifique ( CNRS ), European Centre for Medium-Range Weather Forecasts ( ECMWF ), Centre d'études spatiales de la biosphère ( CESBIO ), Université Paul Sabatier - Toulouse 3 ( UPS ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -Observatoire Midi-Pyrénées ( OMP ) -Centre National d'Etudes Spatiales ( CNES ) -Centre National de la Recherche Scientifique ( CNRS ), Laboratoire de Météorologie Dynamique (UMR 8539) ( LMD ), Université Pierre et Marie Curie - Paris 6 ( UPMC ) -Institut national des sciences de l'Univers ( INSU - CNRS ) -École polytechnique ( X ) -École des Ponts ParisTech ( ENPC ) -Centre National de la Recherche Scientifique ( CNRS ) -Département des Géosciences - ENS Paris, École normale supérieure - Paris ( ENS Paris ) -École normale supérieure - Paris ( ENS Paris ), Centre de Recherches de Climatologie ( CRC ), Université de Bourgogne ( UB ) -Centre National de la Recherche Scientifique ( CNRS ), Littoral, Environnement, Télédétection, Géomatique ( LETG - Nantes ), Université de Caen Normandie ( UNICAEN ), Normandie Université ( NU ) -Normandie Université ( NU ) -École pratique des hautes études ( EPHE ) -Université de Brest ( UBO ) -Université de Rennes 2 ( UR2 ), Université de Rennes ( UNIV-RENNES ) -Université de Rennes ( UNIV-RENNES ) -Centre National de la Recherche Scientifique ( CNRS ) -Institut de Géographie et d'Aménagement ( IGARUN ), Université de Nantes ( UN ) -Université de Nantes ( UN ), Department of Geography [Los Angeles], University of California at Los Angeles [Los Angeles] ( UCLA ), and ALMIP - AMMA
- Subjects
[ SDE.MCG ] Environmental Sciences/Global Changes ,[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology ,west african monsson ,land surface/atmosphere interactions - Abstract
International audience; A high priority goal of the AMMA project is to better understand and model the influence of the spatio-temporal variability of surface processes on the atmospheric circulation patterns and the regional water cycle related to the West African Monsoon. This issue is being addressed under the auspices of the AMMA Land surface Model Intercomparison Project (ALMIP). The idea is to force state-of-the-art land surface models with the best quality and highest (space and time) resolution data available in order to better understand the key processes and their corresponding scales. In this paper, an overview of the ALMIP project objectives is presented, along with a description of input forcing data, some preliminary results, and a discussion of ongoing evaluation efforts. In terms of forcing, satellite-based data is used to reduce errors in data derived from atmospheric models which suffer from systematic biases: errors in the placement of the active monsoon precipitation zone are shown to be significantly reduced using such data. This is shown to have a significant impact on the LSM (land surface model) evapotranspiration, especially in the Sahel. The inter-model scatter in evapotranspiration and soil moisture storage change over the Sahel was found to be on the order of 20% of the multi-model mean values during the monsoon season, thus the models were in fairly good agreement and have far better agreement than such estimates from coupled land-atmosphere models. In terms of evaluation of simulations, indirect methods are required on large scales: the LSMs were able to produce spatial and temporal soil moisture patterns consistent with remotely sensed brightness temperature data over this region. At the grid scale, ALMIP surface sensible heat flux estimates had the same basic response (amplitude and phase) to the wet season as seen in aggregated fluxes from local scale observational sites. Finally, ALMIP is an ongoing project and perspectives for the next phase (at finer spatial scales) are presented.
- Published
- 2008
35. Voda v pôde - hlavný zdroj vody pre suchozemské systémy biosféry
- Author
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Gusev, Y. and Novák, V.
- Subjects
TA Engineering (General). Civil engineering (General) - Abstract
Water resources are usually treated as potential resources, directly exploitable by human population on the Earth. Among them, surface water and groundwater can be effectively managed for operational use. Soil water which belongs to the class of subsurface water represents the major volume of terrestrial water resources. The concept of soil water resources as a water source for biosphere was introduced recently by Budagovsky (1985) and is related to the fact, that the soil water is the most important factor of the existence and development of terrestrial vegetation. As a measure of soil water resources, Budagovsky proposed the evapotranspiration rate from the land surface during the frostless period representing the sum of water evaporation by soil and transpiration from stomata of the leaves of terrestrial plants. The primary importance of soil water is in its role as a source of water for biosphere, for the first stage of trophic chain on the Earth. In this review, the role of soil water in biotic and abiotic cycle on the Earth is discussed. Possible directions of the future study of soil water resources in relation to the environment are proposed.
- Published
- 2007
36. CMS TriDAS project: Technical Design Report, Volume 1: The Trigger Systems
- Author
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Bayatyan, G L, Grigorian, N, Khachatrian, V G, Margarian, A T, Sirunyan, A M, Stepanian, S, Adam, W, Brugger, M, Erö, J, Fierro, M, Friedl, M, Frühwirth, Rudolf, Hrubec, Josef, Jeitler, Manfred, Krammer, Manfred, Pernicka, Manfred, Porth, Paul, Rohringer, Herbert, Rurua, L, Taurok, Anton, Walzel, G, Wedenig, R, Wulz, Claudia Elisabeth, Baryshevsky, V G, Fedorov, A, Gorodishenin, N L, Korzhik, M V, Missevitch, O V, Panov, V, Zuyeuski, R, Zalessky, V B, Ermalitsky, F, Kuchinskii, P, Lomako, V M, Prosolovich, V, Devroede, O, Goorens, R, Lemonne, J, Tavernier, Stefaan, Udo, Fred, Van Doninck, W K, Van Lancker, L, Bertrand, D, De Lentdecker, G, Stefanescu, J, Van der Velde, C, Vanlaer, P, Favart, D, Govaerts, J, Grégoire, G, Lemaître, V, Ninane, A, Piotrzkowski, K, van der Aa, O, Boulogne, I, Daubie, Evelyne, Herquet, P, Beaumont, W, Beckers, T, De Langhe, E, Moortgat, F, Verbeure, F, Zhukov, V, Abadjiev, K, Anguelov, T, Atanasov, I H, Damgov, J, Dimitrov, L, Genchev, V, Georgiev, G, Iaydjiev, P, Kounov, B, Penchev, L, Raykov, P, Sultanov, G G, Vankov, I, Vankov, P, Darmenov, N, Gritskov, A, Jordanov, A, Litov, L, Mateev, M, Petev, P, Spassov, V, Tchijov, M, Tsenov, R V, Velev, G V, Bian, J G, Chen, C, Chen, G M, Guo, Y N, He, J T, Jiang, C H, Jin, B N, Ke, Z J, Li, J, Li, W G, Li Xiao Nan, Qiu, J F, Shen, B W, Shen, X Y, Sheng, H Y, Wang, Y Y, Xu Rong Sheng, Yang, M, Zhang Bing Yun, Zhang, J W, Zhang, S Q, Zhao Wei Ren, Zhao, Z, Zheng Jian Ping, Zhu, G Y, Zhu, Y S, Ban, Y, Cai, J, Chen Jia Erh, Liu Hong Tao, Liu Song Qiu, Lou Bin Qiao, Qian, S J, Ye Yan Lin, An, Q, Bian, Z, Chen, H, Gong, Z F, Li Chuan, Shri, C S, Sun, L Z, Wang, X L, Wang, Z M, Wu, J, Ye Shu Wei, Zhang, Z P, Deng, Q, Li, P J, Shen, D Z, Xue, Z L, Yuan, H B, Chang, Y H, Chen, A E, Go, A, Lin, W, Chang, P, Hou, G W S, Ueno, K, Godinovic, N, Milin, M, Puljak, I, Soric, I, Stipcevic, M, Tudoric-Ghemo, J, Antunovic, Z, Dzelalija, M, Marasovic, K, Hasan, A, Razis, P A, Vorvolakos, A, Hall, A, Lippmaa, E, Lippmaa, J, Raidal, Martti, Subbi, J, Aarnio, Pertti A, Banzuzi, K, Heikkinen, A M, Heinonen, J V, Honkanen, A, Karimäki, V, Katajisto, H M, Kinnunen, Ritva, Lassila-Perini, K M, Lefébure, V, Pietarinen, E, Tuominen, E, Tuominiemi, Jorma, Ungaro, D, Vanhala, T P, Williams, C, Lehti, S, Lindén, T, Äystö, J, Julin, R, Ruuskanen, P V, Kallijärvi, S, Keränen, A, Palmu, L, Remes, K, Suhonen, E, Tuuva, T, Niittylahti, J, Vainio, O, Baek, Y W, Boget, D, Ditta, J, Drobychev, G Yu, Guillaud, J P, Maire, M, Mendiburu, J P, Nédélec, P, Peigneux, J P, Schneegans, M, Sillou, D, Anfreville, M G, Bonamy, P, Bouchand, C, Chipaux, Rémi, Dejardin, M, Denegri, Daniel, Gentit, F X, Givernaud, Alain, Kircher, F, Lemoigne, Y, Locci, E, Lottin, J P, Nguyen, M C, Pansart, J P, Payn, A, Rander, J, Reymond, J M, Rondeaux, F, Rosowsky, A, Roth, P, Verrecchia, P, Badier, J, Bercher, M, Bourotte, J, Busson, P, Chamont, D, Charlot, C, Dobrzynski, Ludwik, Gilly, J, Haguenauer, Maurice, Karar, A, Kim, G B, Kluberg, L, Lecouturier, D, Matricon, P, Milleret, G, Miné, P, Morano, R, Paganini, P, Poilleux, P, Romanteau, T, Albert, A, Berst, J D, Blaes, R, Brom, J M, Charles, F, Coffin, J, Didierjean, François, Drouhin, F, Ernenwein, J P, Fontaine, J C, Geist, Walter M, Goerlach, U, Helleboid, J M, Huss, D, Illinger, C, Juillot, P, Lounis, A, Maazouzi, C, Moreau, S, Riahi, Y, Ripp-Baudot, I, Todorov, T, Vintache, D, Zghiche, A, Ageron, M, Bedjidian, Marc, Chabanat, E, Combaret, C, Contardo, D, Depasse, P, Drapier, O, Dupanloup, M, El-Mamouni, H, Fay, J, Gascon-Shotkin, S M, Giraud, N, Girerd, C, Goyot, M, Haroutounian, R, Ille, B, Lebrun, P, Lethuillier, M, Martin, J P, Mathez, H, Mirabito, L, Muanza, G S, Perriès, S, Sahuc, P, Smadja, G, Tissot, S, Walder, J P, Zach, F, Amaglobeli, N S, Bagaturia, Yu S, Glonti, L, Kartvelishvili, V G, Kvatadze, R A, Mzhavia, D A, Sakhelashvili, T M, Shanidze, R G, Tsamalaidze, Z B, Djaoshvili, N, Iashvili, I, Kharchilava, A I, Roinishvili, N N, Roinishvili, V N, Berger, C, Braunschweig, W, Breibach, J, Gu, W H, Heister, A, Karpinski, W, Kirn, T, König, S, Kukulies, C, Ostapchuk, A Ya, Pandoulas, D, Pierschel, G, Raupach, F, Schael, S, Schmitz, D, Schultz von Dratzig, A, Siedling, R, Wallraff, W, Wittmer, B, Banicz, K, Bechstein, S, Böhm, A, Bosseler, K, Faissner, Helmut, Fesefeldt, H S, Hermann, S, Ivannikov, A, Rein, D, Reithler, H, Szczesny, H, Tonutti, M, Wegner, M, Axer, M, Beissel, F, Commichau, V, Flügge, G, Hangarter, K, Macke, D, Mnich, J, Nowak, A, Petertill, M, Schmitz, P, Schulte, R, Sonnenschein, L, Zander, A, Grünewald, M W, Hebbeker, T, Höpfner, K, Rosca, A, Bartsch, V, Blüm, H P, de Boer, Wim, Dierlamm, A, Dirkes, G, Drollinger, V, Erdmann, M, Feindt, Michael, Grigoriev, E, Hartmann, F, Hauler, F, Heiss, A, Müller, T, Röderer, F, Simonis, H J, Skiba, A, Theel, A, Thümmel, W H, Weiler, Thomas J, Weseler, S, Resvanis, L K, Adzic, P, Barone, M, Bozovic-Jelisavcic, I, Fanourakis, G K, Geralis, T, Harissopoulos, S V, Kokkinias, P, Kyriakis, A, Loukas, D, Markou, A, Markou, C, Mastroyiannopoulos, N, Mousa, J, Siotis, I, Spyropoulou-Stassinaki, M, Staveris-Polykalas, A, Tsirigotis, A G, Tzamarias, S, Vayaki, Anna, Zachariadou, K, Zupan, M, Asimidis, A, Evangelou, I, Kokkas, P, Manthos, N, Mitropoulos, O, Prouskas, K, Triantis, F A, Tzoulis, N, Bagoly, Z, Bencze, G L, Csilling, Akos, Hajdu, C, Hidas, P, Horváth, D, Ódor, G, Ster, A, Urbàn, L, Vesztergombi, G, Zálán, P, Zsenei, M, Dajkó, G, Fenyvesi, A, Molnár, J, Pálinkás, J, Sohler, D, Trócsányi, Z L, Vamosi, J, Végh, J, Baksay, L, Bondar, T, Juhász, S, Marian, G, Nagy, S, Raics, P, Szabó, J, Szabó, Z, Szegedi, S, Szillási, Z, Sztaricskai, T, Tarjan, P, Zilizi, G, Bala, S B, Bhatnagar, V, Kaur, M, Kohli, J M, Singh, J, Borkar, S, Chandratre, V, Chaudhury, R K, Dixit, M Y, Ghodgaonkar, M, John, B, Kataria, S K, Mohanty, A K, Topkar, A, Aziz, T, Banerjee, Sunanda, Chendvankar, S R, Deshpande, P V, Ganguli, S N, Gurtu, A, Katta, S, Maity, M, Mazumdar, K, Patil, M R, 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A S, Cooper, A, Fountain, M, McCliment, E, Merlo, J P, Miller, M J, Önel, Y M, Schmidt, I, Barnett, B A, Chien, C Y, Cho Hyo Sung, Liang, G, Swartz, M, Xie, X, Abdullin, S, Arcelli, S, Baden, D, Bard, R L, Eno, S, Fong, D, Grassi, T, Hadley, N J, Kellogg, R G, Kunori, S, Sharma, A, Skuja, A, Carey, R, Hazen, E S, Kearns, E T, Machado, E, Miller, J, Osborne, D, Roberts, B L, Rohlf, J, Sulak, Lawrence R, Sullivan, J D, Wu, S, Alverson, G, Fenker, H C, Gaponenko, I A, Moromisato, J H, Musienko, Yu V, Nicol, S, Paul, T, Reucroft, S, Swain, J D, Taylor, L, von Goeler, E, Yasuda, T, Bauer, G, Friedman, J, Paus, C, Pavlon, S, Rosenson, L, Sumorok, Konstanty, Tether, S, Tseng, J, Cushman, P B, Heering, A H, Kronkvist, I J, Rusack, R W, Singovsky, A V, Vikas, P, Bhatt, K, Booke, M, Cremaldi, L M, Kroeger, R A, Reidy, J, Sanders, D, Summers, D, Campbell, W B, Claes, D R, Lundstedt, C, Snow, G R, Bartz, E, Conway, J, Devlin, T, Doroshenko, J, Jacques, P F, Kalelkar, M S, Koeth, T W, Lath, A, 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Kim, G, Koblik, Yu N, Rakhmatov, N, Rustamov, I, Shukrullo, I, Urkinbaev, A R, and Yuldashev, B S
- Subjects
Detectors and Experimental Techniques - Published
- 2004
37. Bacterial Growth, Division, and Mutation
- Author
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Gusev, Y., primary and Armitage, Peter, additional
- Published
- 2014
- Full Text
- View/download PDF
38. Photostimulated phenomena in relaxors
- Author
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Mamin R., Migachev S., Sadykov M., Lunev I., Izotov V., and Gusev Y.
- Abstract
The action of illumination on the conducting and dielectric properties of lead magnoniobate was investigated. The photostimulated currents were examined and the spectral dependence of photoconductivity in the region of diffuse phase transition was obtained. It was found that the illumination affects the dielectric properties and that its action is memorized at temperatures below room temperature. The role of defect states in the formation of relaxor properties is discussed on the basis of the obtained data. © 2003 MAIK "Nauka/Interperiodica".
- Published
- 2003
39. Analysis of dielectric relaxation data in water-saturated sands and clays
- Author
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Lounev I., Nigmatullin R., Zavidonov A., Gusev Y., Manurov I., Kaumov S., and Muslimov R.
- Abstract
The measurements of the imaginary part of the complex susceptibility in water-saturated sands and clays have been conducted. To explain the experimental data obtained the fractal model of medium has been used [Laboratory Humidity Ovens (Non-injection Type), BS (1964) 3718; Fleches du temps et geometric fractale, Paris Hermes, 1998]. In the range of humidity not exceeding 12%, the main contribution to the dipole relaxation is provided has bound water [A Wetting Ability Clays and Clay Minerals, Kiev, 1961, p. 292], that is reflected in the power-law exponent behavior. © 2002 Elsevier Science B.V. All rights reserved.
- Published
- 2002
40. The effect of clay morphology on water relaxation
- Author
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Lunev I., Nigmatullin R., Zavidonov A., Gusev Y., and Manyurov I.
- Abstract
The frequency dependence of the permittivity of water in calcium kaolinite (clay) is measured. It is shown that two mechanisms contribute to dipole relaxation of water. One refers to water in the free volume of pores in the clay. The other is associated with bound water covering the porous surface. Experimental data are treated in terms of a fractal model of the medium. The frequency dependence of the permittivity in a wide range of water content in the clay is accounted for theoretically. © 2001 MAIK "Nauka/Interperiodica".
- Published
- 2001
41. CMS : the TriDAS Project Technical Design Report; v.1, the Trigger Systems
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L. Bayatyan, G., Grigorian, N., G. Khachatrian, V., T. Margarian, A., M. Sirunyan, A., Adam, W., Brügger, M., Erö, J., Fierro, M., Friedl, M., Frühwirth, R., Hrubec, J., Jeitler, A., Krammer, M., Pernicka, M., Porth, P., Rohringer, H., Rurua, L., Taurok, A., Walzel, G., Wedenig, R., E. Wulz, C., G. Baryshevsky, V., Fedorov, A., L. Gorodishenin, N., V. Korzhik, M., V. Missevitch, O., Panov, V., Zuyeuski, R., B. Zalessky, V., Ermalitsky, F., Kuchinskii, P., M. Lomako, V., Prosolovich, V., Devroede, O., Goorens, R., Lemonne, J., Tavernier, S., Udo, F., W. K. Van, Doninck, L. Van, Lancker, Bertrand, D., G. De, Lentdecker, Stefanescu, J., Velde C. Van, Der, Vanlaer, P., Favart, D., Govaerts, J., Grégoire, G., Lemaître, V., Ninane, A., Piotrzkowski, K., Aa O. Van, Der, Boulogne, I., Daubie, E., Herquet, P., Beaumont, W., Beckers, T., E. De, Langhe, Moortgat, F., Verbeure, F., Zhukov, V., Abadjiev, K., Anguelov, T., H. Atanasov, I., Damgov, J., Dimitrov, L., Genchev, V., Georgiev, G., Iaydjiev, P., Kounov, B., Penchev, L., Raykov, P., G. Sultanov, G., Vankov, I., Vankov, P., Darmenov, N., Gritskov, A., Jordanov, A., B. Litov, L., Mateev, M., Petev, P., Spassov, V., Tchijov, M., Tsenov, R., V. Velev, G., G. Bian, J., Chen, C., M. Chen, G., N. Guo, Y., T. He, J., H. Jiang, C., N. Jin, B., J. Ke, Z., Li, J., G. Li, W., Nan Li, Xiao, F. Qiu, J., W. Shen, B., Y. Shen, X., Y. Sheng, H., Wang, Y.Y., Sheng Xu, Rong, Yang, M., Yun Zhang, Bing, W. Zhang, J., Q. Zhang, S., Ren Zhao, Wei, Zhao, Z., Ping Zheng, Jian, Y. Zhu, G., S. Zhu, Y., Ban, Y., Cai, J., Erh Chen, Jia, Tao Liu, Hong, Qiu Liu, Song, Qiao Lou, Bin, J. Qian, S., Lin Ye, Yan, An, Q., Bian, Z., Chen, H., F. Gong, Z., Li, Chuan, S. Shri, C., Z. Sun, L., L. Wang, X., M. Wang, Z., Wu, J., Wei Ye, Shu, P. Zhang, Z., Deng, Q., J. Li, P., Z. Shen, D., L. Xue, Z., B. Yuan, H., H. Chang, Y., E. Chen, A., Go, A., Lin, W., Chang, P., W. S. 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Kim, G., Kluberg, L., Lecouturier, D., Matricon, P., Milleret, G., Miné, P., Morano, R., Paganini, P., Poilleux, P., Romanteau, T., Albert, A., Berst, J.D., Blaes, R., Brom, J.M., Charles, F., Coffin, J., Didierjean, F., Drouhin, F., Ernenwein, J.-P., Fontaine, J.C., Geist, W., Goerlach, U., Helleboid, J.M., Huss, D., Illinger, C., Juillot, P., Lounis, A., Maazouzi, C., Moreau, S., Riahi, Y., Ripp-Baudot, I., Todorov, T., Vintache, D., Zghiche, A., Ageron, M., Bedjidian, M., Chabanat, E., Combaret, C., Contardo, D., Depasse, P., Drapier, O., Dupanloup, M., El-Mamouni, H., Fay, J., Gascon-Shotkin, S., Giraud, N., Girerd, C., Goyot, M., Haroutunian, R., Ille, B., Lebrun, P., Lethuillier, M., Martin, J.-P., Mathez, H., Mirabito, L., Muanza, G.-S., Perriès, S., Sahuc, P., Smadja, G., Tissot, S., Walder, J.-P., Zach, F., S. Amaglobeli, N., S. Bagaturia, Yu, Glonti, L., G. Kartvelishvili, V., A. Kvatadze, R., Mzhavia, D.A., M. Sakhelashvili, T., G. Shanidze, R., B. 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Hazen, E., T. Kearns, E., Machado, E., Miller, J., Osborne, D., L. Roberts, B., Rohlf, J., Sulak, L.R., D. Sullivan, J., Wu, S., Alverson, G., C. Fenker, H., A. Gaponenko, I., H. Moromisato, J., V. Musienko, Yu, Nicol, S., Paul, T., Reucroft, S., D. Swain, J., Taylor, L., E. Von, Goeler, Yasuda, T., Bauer, G., Friedman, J., Paus, C., Pavlon, S., Rosenson, L., Sumorok, S., Tether, S., Tseng, J., B. Cushman, P., H. Heering, A., J. Kronkvist, I., W. Rusack, R., V. Singovsky, A., Vikas, P., Bhatt, K., Booke, M., M. Cremaldi, L., Kroeger, R.A., Reidy, J., Sanders, D., Summers, D., B. Campbell, W., R. Claes, D., Lundstedt, C., R. Snow, G., Bartz, E., Conway, J., Devlin, T., Doroshenko, J., F. Jacques, P., S. Kalelkar, M., W. Koeth, T., Lath, A., P. Perera, L., Schnetzer, S., V. Somalwar, S., Stone, R., Thomson, G., L. Watts, T., M. Bussat, J., Denes, P., Gupta, V., Mans, J., Marlow, D., A. Piroué, P., P. Stickland, D., Tully, C., Wildish, T., R. Blusk, S., Bodek, A., Budd, H., P. 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Yuldashev, B., Laboratoire d'Annecy de Physique des Particules (LAPP/Laboratoire d'Annecy-le-Vieux de Physique des Particules), Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS), Laboratoire Leprince-Ringuet (LLR), Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-École polytechnique (X)-Centre National de la Recherche Scientifique (CNRS), Institut de Recherches Subatomiques (IReS), Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Cancéropôle du Grand Est-Université Louis Pasteur - Strasbourg I-Centre National de la Recherche Scientifique (CNRS), Institut de Physique Nucléaire de Lyon (IPNL), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS), CMS, Laboratoire d'Annecy de Physique des Particules (LAPP), Centre National de la Recherche Scientifique (CNRS)-École polytechnique (X)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3), Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3), Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3), and Flores, Sylvie
- Subjects
[PHYS.HEXP] Physics [physics]/High Energy Physics - Experiment [hep-ex] ,[PHYS.PHYS.PHYS-INS-DET] Physics [physics]/Physics [physics]/Instrumentation and Detectors [physics.ins-det] ,[PHYS.HEXP]Physics [physics]/High Energy Physics - Experiment [hep-ex] ,[PHYS.PHYS.PHYS-INS-DET]Physics [physics]/Physics [physics]/Instrumentation and Detectors [physics.ins-det] - Abstract
CMS
- Published
- 2000
42. Fragmentation of Be induced by 1 GeV protons
- Author
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Andronenko, L. N., Andronenko, M. N., Gusev, Y. I., Kotov, A. A., Neubert, W., Petrov, G. E., Seliverstov, D. M., Strakovski, I. I., Vaishnene, L. A., Yatsoura, V. I., and Zalite, A. Y.
- Subjects
cross section ,fragmentation ,isotope ,proton - Abstract
Fragment yields and energy spectra of He, Li and Be isotopes have been measured in p+9Be interactions at 1 GeV incident energy at 30 deg. and 126 deg. using a two-arm spectrometer based on Bragg chambers. The obtained yield ratio of the low abundant 8He to 8Li in the spectator momentum range is compared with published data.
- Published
- 1999
43. Water structure analysis considering dielectric spectrum in microwave range
- Author
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Arkhipov V., Gusev Y., and Lounev I.
- Abstract
In this paper the analysis of the water dielectric spectrum in the relaxation (1 cm) and microwave (100 mu) range on the basis of the theoretical results presented in Ref. was made. The absorption spectrum in the microwave range as well as the relaxation spectrum are shown to be the results of the orientational polarization. In the framework of the existing water structure models this result corresponds to the models in which one assume two types of the molecules for the fixed time moment. They are the molecules having a hydrogen bonds and ones free from them. Free molecules either can be located in the voids or can make the exchange between the clasters. In the analysis suggested we do not use the definite water structure model. The dielectric spectrum parameters allow us estimate the value of the abnormal water expansion within the freezing process. Our results agree well with the experimental data.
- Published
- 1999
44. The Project for Intercomparison of Land-surface Parameterization Schemes (PILPS) phase 2(c) Red–Arkansas River basin experiment: 3. Spatial and temporal analysis of water fluxes
- Author
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Lohmann, D., Lettenmaier, D. P., Liang, X., Wood, E. F., Boone, A., Chang, S., Chen, F., Dai, Y. J., Desborough, C., Dickinson, R. E., Duan, Q. Y., Ek, M., Gusev, Y. M., Habets, F., Irannejad, P., Koster, R., Mitchell, K. E., Nasonova, O. N., Noilhan, J., Schaake, J., Schlosser, A., Shao, Y. P., Shmakin, A. B., Verseghy, D., Warrach, K., Wetzel, P., Xue, Y. K., Zong-Liang Yang, and Zeng, Q. C.
- Subjects
water balance ,Earth Sciences ,routing model ,continental river basin modeling ,Red-Arkansas River basin ,PILPS ,Networking & Telecommunications - Abstract
The water-balance components of 16 Soil-Vegetation Atmospheric Transfer (SVAT) schemes were evaluated by comparing predicted and observed streamflow, predicted evapotranspiration and evapotranspiration inferred from an atmospheric moisture budget analysis, and soil moisture storage changes for a seven-year period (1980-1986) using data from the Red-Arkansas River basins of the Southern Great Plains of the USA. The evaluations support the following suggestions: (a) The mean annual runoff of all models follows, at least generally, the strong climatic East-West gradient of precipitation, although most models predict too much runoff in the dry part of the basin. (b) The mean monthly storage change tends to be underestimated, even though all models capture reasonably well the seasonality of the evapotranspiration. (c) The wide range of conceptualizations used for generation of surface and subsurface runoff strongly affect runoff generation on seasonal, and shorter, time scales. Model responses to summer precipitation ranged from almost no summer runoff (one model) to the (more common) situation of persistent overprediction of summer runoff, especially in the driest part of the basin. (d) All models tended to underpredict evapotranspiration in summer and overpredict in winter. (e) Model-derived mean seasonal cycles of changes in soil moisture storage are qualitatively similar to those inferred from observations, but most models do not predict the decrease in April soil moisture storage and the increase in October that is inferred from observations.
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- 1998
- Full Text
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45. The project for intercomparison of land-surface parameterization schemes (PILPS) phase 2(c) Red-Arkansas River basin experiment: 1. Experiment description and summary intercomparisons
- Author
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Wood, E. F., Lettenmaier, D. P., Liang, X., Lohmann, D., Boone, A., Chang, S., Chen, F., Dai, Y. J., Dickinson, R. E., Duan, Q. Y., Ek, M., Gusev, Y. M., Habets, F., Irannejad, P., Koster, R., Mitchel, K. E., Nasonova, O. N., Noilhan, J., Schaake, J., Schlosser, A., Shao, Y. P., Shmakin, A. B., Verseghy, D., Warrach, K., Wetzel, P., Xue, Y. K., Zong-Liang Yang, and Zeng, Q. C.
- Subjects
land-surface parameterization ,energy/water balance ,calibration of land-surface schemes ,Life on Land ,Earth Sciences ,continental river basin modeling ,Red-Arkansas River basin ,PILPS ,Networking & Telecommunications - Abstract
Sixteen land-surface schemes participating in the project for the Intercomparison of Land-surface Schemes (PILPS) Phase 2(c) were run using 10 years (1979-1988) of forcing data for the Red-Arkansas River basins in the Southern Great Plains region of the United States. Forcing data (precipitation, incoming radiation and surface meteorology) and land-surface characteristics (soil and vegetation parameters) were provided to each of the participating schemes. Two groups of runs are presented. (1) Calibration-validation runs, using data from six small catchments distributed across the modeling domain. These runs were designed to test the ability of the schemes to transfer information about model parameters to other catchments and to the computational grid boxes. (2) Base-runs, using data for 1979-1988, designed to evaluate the ability of the schemes to reproduce measured energy and water fluxes over multiple seasonal cycles across a climatically diverse, continental-scale basin. All schemes completed the base-runs but five schemes chose not to calibrate. Observational data (from 1980-1986) including daily river flows and monthly basin total evaporation estimated through an atmospheric budget analysis, were used to evaluate model performance. In general, the results are consistent with earlier PILPS experiments in terms of differences among models in predicted water and energy fluxes. The mean annual net radiation varied between 80 and 105 W m-2 (excluding one model). The mean annual Bowen ratio varied from 0.52 to 1.73 (also excluding one model) as compared to the data-estimated value of 0.92. The run-off ratios varied from a low of 0.02 to a high of 0.41, as compared to an observed value of 0.15. In general, those schemes that did not calibrate performed worse, not only on the validation catchments, but also at the scale of the entire modeling domain. This suggests that further PILPS experiments on the value of calibration need to be carried out.
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- 1998
- Full Text
- View/download PDF
46. The Project for Intercomparison of Land-surface Parameterization Schemes (PILPS) phase 2(c) Red-Arkansas River basin experiment: 2. Spatial and temporal analysis of energy fluxes
- Author
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Liang, X., Wood, E. F., Lettenmaier, D. P., Lohmann, D., Boone, A., Chang, S., Chen, F., Dai, Y. J., Desborough, C., Dickinson, R. E., Duan, Q. Y., Ek, M., Gusev, Y. M., Habets, F., Irannejad, P., Koster, R., Mitchell, K. E., Nasonova, O. N., Noilhan, J., Schaake, J., Schlosser, A., Shao, Y. P., Shmakin, A. B., Verseghy, D., Warrach, K., Wetzel, P., Xue, Y. K., Zong-Liang Yang, and Zeng, Q. C.
- Subjects
land-surface models ,Earth Sciences ,Red-Arkansas River basin ,PILPS ,Networking & Telecommunications ,energy balance ,Physics::Atmospheric and Oceanic Physics - Abstract
The energy components of sixteen Soil-Vegetation Atmospheric Transfer (SVAT) schemes were analyzed and intercompared using 10 years of surface meteorological and radiative forcing data from the Red-Arkansas River basin in the Southern Great Plains of the United States. Comparisons of simulated surface energy fluxes among models showed that the net radiation and surface temperature generally had the best agreement among the schemes. On an average (annual and monthly) basis, the estimated latent heat fluxes agreed (to within approximate estimation errors) with the latent heat fluxes derived from a radiosonde-based atmospheric budget method for slightly more than half of the schemes. The sensible heat fluxes had larger differences among the schemes than did the latent heat fluxes, and the model-simulated ground heat fluxes had large variations among the schemes. The spatial patterns of the model-computed net radiation and surface temperature were generally similar among the schemes, and appear reasonable and consistent with observations of related variables, such as surface air temperature. The spatial mean patterns of latent and sensible heat fluxes were less similar than for net radiation, and the spatial patterns of the ground heat flux vary greatly among the 16 schemes. Generally, there is less similarity among the models in the temporal (interannual) variability of surface fluxes and temperature than there is in the mean fields, even for schemes with similar mean fields.
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- 1998
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47. Catalogue of the models used in MOPEX 2004/2005
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Andreassian, V., Hall, A., Schaake, J., Bergstrom, S., Chahinian, N., Duan, Q., Gusev, Y. M., Littlewood, I., Mathevet, T., Michel, C., Montanari, A., Moretti, G., Moussa, R., Nasonova, O. N., O'Connor, K., Paquet, E., Perrin, C., Rousseau, A., Wagener, T., Xie, Z., Andreassian, V., Hall, A., Schaake, J., Bergstrom, S., Chahinian, N., Duan, Q., Gusev, Y. M., Littlewood, I., Mathevet, T., Michel, C., Montanari, A., Moretti, G., Moussa, R., Nasonova, O. N., O'Connor, K., Paquet, E., Perrin, C., Rousseau, A., Wagener, T., and Xie, Z.
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- 2006
48. The Rhone-aggregation land surface scheme intercomparison project: An overview
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Boone, A, Habets, F, Noilhan, J, Clark, D, Dirmeyer, P, Fox, S, Gusev, Y, Haddeland, I, Koster, R, Lohmann, D, Mahanama, S, Mitchell, K, Nasonova, O, Niu, GY, Pitman, A, Polcher, J, Shmakin, AB, Tanaka, K, van den Hurk, B, Verant, S, Verseghy, D, Viterbo, P, Yang, ZL, Boone, A, Habets, F, Noilhan, J, Clark, D, Dirmeyer, P, Fox, S, Gusev, Y, Haddeland, I, Koster, R, Lohmann, D, Mahanama, S, Mitchell, K, Nasonova, O, Niu, GY, Pitman, A, Polcher, J, Shmakin, AB, Tanaka, K, van den Hurk, B, Verant, S, Verseghy, D, Viterbo, P, and Yang, ZL
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- 2004
49. The Rhone-aggregation land surface scheme intercomparison project: An overview
- Author
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30283625, Boone, A, Habets, F, Noilhan, J, Clark, D, Dirmeyer, P, Fox, S, Gusev, Y, Haddeland, I, Koster, R, Lohmann, D, Mahanama, S, Mitchell, K, Nasonova, O, Niu, GY, Pitman, A, Polcher, J, Shmakin, AB, Tanaka, K, van den Hurk, B, Verant, S, Verseghy, D, Viterbo, P, Yang, ZL, 30283625, Boone, A, Habets, F, Noilhan, J, Clark, D, Dirmeyer, P, Fox, S, Gusev, Y, Haddeland, I, Koster, R, Lohmann, D, Mahanama, S, Mitchell, K, Nasonova, O, Niu, GY, Pitman, A, Polcher, J, Shmakin, AB, Tanaka, K, van den Hurk, B, Verant, S, Verseghy, D, Viterbo, P, and Yang, ZL
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- 2004
50. ChemInform Abstract: Generation of an Oscillating Chemical Reaction in a Heterogeneous System by the Oxidation of an Alkaline Solution of Luminol with Sodium(VI) Ferrate in the Presence of Copper Ions.
- Author
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Stoupine, D. Yu., primary, Gusev, Y. K., additional, and Lachkova, D. V., additional
- Published
- 2010
- Full Text
- View/download PDF
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