1,452 results on '"Burrows, J"'
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2. The use of satellite and ground based measurements for estimating and reducing uncertainties in the spatial distribution of emissions of nitrogen oxides
- Author
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Konovalov, I. B., Beekmann, M., Richter, A., and Burrows, J. P.
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Physics - Atmospheric and Oceanic Physics ,Physics - Data Analysis, Statistics and Probability - Abstract
We explore possibilities of improving the spatial structure of NOx emissions employed in a continental scale chemistry transport model (CTM) by using satellite measurements of nitrogen dioxide and ground-based observations of near surface ozone. In this study, we combine the tropospheric NO2 columns derived from SCIAMACHY measurements, the data from the EMEP ozone-monitoring network and the calculations performed with the CHIMERE CTM in the framework of an advanced inverse modelling scheme. All data used in the study correspond to the period of June-August 2003. The main distinctive feature of our inversion scheme is that, in contrast to more common inverse modelling approaches, the magnitudes of uncertainties in the input data are not explicitly predefined but rather estimated consistently with the a posteriori emissions as a result of the inversion. While the tropospheric NO2 columns are used for fitting the spatial distribution of the emission parameters of the model, the ozone observations are only used to estimate the averaged levels of uncertainties in a priori emissions. We use our method in order to estimate and to reduce uncertainties in the gridded (with the resolution of 1 degree) NOx emission data for Europe, Middle East and Northern Africa. It is found that the a priori emission estimates used in the standard version of CHIMERE are probably biased in several regions. On average, the uncertainties in total NOx emissions are estimated to be about 1.7 in terms of the geometric standard deviation in Europe and about 2.1 outside of Europe. The corrected emission estimates provide better agreement of the modelled results with observations for both NO2 columns and near surface concentrations of ozone.
- Published
- 2006
3. State of the climate in 2012
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Achberger, C, Ackerman, SA, Albanil, A, Alexander, P, Alfaro, EJ, Allan, R, Alves, LM, Amador, JA, Ambenje, P, Andrianjafinirina, S, Antonov, J, Aravequia, JA, Arendt, A, Arévalo, J, Arndt, DS, Ashik, I, Atheru, Z, Banzon, V, Baringer, MO, Barreira, S, Barriopedro, DE, Beard, G, Becker, A, Behrenfeld, MJ, Bell, GD, Benedetti, A, Bernhard, G, Berrisford, P, Berry, DI, Bhatt, U, Bidegain, M, Bindoff, N, Bissolli, P, Blake, ES, Blunden, J, Booneeady, R, Bosilovich, M, Box, JE, Boyer, T, Braathen, GO, Bromwich, DH, Brown, R, Brown, L, Bruhwiler, L, Bulygina, ON, Burgess, D, Burrows, J, Calderón, B, Camargo, SJ, Campbell, J, Cao, Y, Cappelen, J, Carrasco, G, Chambers, DP, Chang'A, L, Chappell, P, Chehade, W, Cheliah, M, Christiansen, HH, Christy, JR, Ciais, P, Coelho, CAS, Cogley, JG, Colwell, S, Cross, JN, Crouch, J, Cunningham, SA, Dacic, M, De Jeu, RAM, Dekaa, FS, Demircan, M, Derksen, C, Diamond, HJ, Dlugokencky, EJ, Dohan, K, Dolman, AJ, Domingues, CM, Dong, S, Dorigo, WA, Drozdov, DS, Duguay, CR, Dunn, RJH, Dúran-Quesada, AM, Dutton, GS, Ehmann, C, Elkins, JW, Euscátegui, C, Famiglietti, JS, Fang, F, Fauchereau, N, Feely, RA, Fekete, BM, Fenimore, C, and Fioletov, VE
- Abstract
For the first time in several years, the El Nino-Southern Oscillation did not dominate regional climate conditions around the globe. A weak La Niña dissipated to ENSO-neutral conditions by spring, and while El Nino appeared to be emerging during summer, this phase never fully developed as sea surface temperatures in the eastern equatorial Pacific uncharacteristically returned to neutral conditions. Nevertheless, other large-scale climate patterns and extreme weather events impacted various regions during the year. A negative phase of the Arctic Oscillation from mid-January to early February contributed to frigid conditions in parts of northern Africa, eastern Europe, and western Asia. A lack of rain during the 2012 wet season led to the worst drought in at least the past three decades for northeastern Brazil. Central North America also experienced one of its most severe droughts on record. The Caribbean observed a very wet dry season and it was the Sahel's wettest rainy season in 50 years. Overall, the 2012 average temperature across global land and ocean surfaces ranked among the 10 warmest years on record. The global land surface temperature alone was also among the 10 warmest on record. In the upper atmosphere, the average stratospheric temperature was record or near-record cold, depending on the dataset. After a 30-year warming trend from 1970 to 1999 for global sea surface temperatures, the period 2000-12 had little further trend. This may be linked to the prevalence of La Niña-like conditions during the 21st century. Heat content in the upper 700 m of the ocean remained near record high levels in 2012. Net increases from 2011 to 2012 were observed at 700-m to 2000-m depth and even in the abyssal ocean below. Following sharp decreases in global sea level in the first half of 2011 that were linked to the effects of La Niña, sea levels rebounded to reach records highs in 2012. The increased hydrological cycle seen in recent years continued, with more evaporation in drier locations and more precipitation in rainy areas. In a pattern that has held since 2004, salty areas of the ocean surfaces and subsurfaces were anomalously salty on average, while fresher areas were anomalously fresh. Global tropical cyclone activity during 2012 was near average, with a total of 84 storms compared with the 1981-2010 average of 89. Similar to 2010 and 2011, the North Atlantic was the only hurricane basin that experienced above-normal activity. In this basin, Sandy brought devastation to Cuba and parts of the eastern North American seaboard. All other basins experienced either near- or below-normal tropical cyclone activity. Only three tropical cyclones reached Category 5 intensity-all in the Western North Pacific basin. Of these, Super Typhoon Bopha became the only storm in the historical record to produce winds greater than 130 kt south of 7°N. It was also the costliest storm to affect the Philippines and killed more than 1000 residents. Minimum Arctic sea ice extent in September and Northern Hemisphere snow cover extent in June both reached new record lows. June snow cover extent is now declining at a faster rate (-17.6% per decade) than September sea ice extent (-13.0% per decade). Permafrost temperatures reached record high values in northernmost Alaska. A new melt extent record occurred on 11-12 July on the Greenland ice sheet; 97% of the ice sheet showed some form of melt, four times greater than the average melt for this time of year. The climate in Antarctica was relatively stable overall. The largest maximum sea ice extent since records begain in 1978 was observed in September 2012. In the stratosphere, warm air led to the second smallest ozone hole in the past two decades. Even so, the springtime ozone layer above Antarctica likely will not return to its early 1980s state until about 2060. Following a slight decline associated with the global financial crisis, global CO2 emissions from fossil fuel combustion and cement production reached a record 9.5 ± 0.5 Pg C in 2011 and a new record of 9.7 ± 0.5 Pg C is estimated for 2012. Atmospheric CO2 concentrations increased by 2.1 ppm in 2012, to 392.6 ppm. In spring 2012, for the first time, the atmospheric CO2 concentration exceeded 400 ppm at 7 of the 13 Arctic observation sites. Globally, other greenhouse gases including methane and nitrous oxide also continued to rise in concentration and the combined effect now represents a 32% increase in radiative forcing over a 1990 baseline. Concentrations of most ozone depleting substances continued to fall.
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- 2013
4. Atmospheric and Surface Processes, and Feedback Mechanisms Determining Arctic Amplification: A Review of First Results and Prospects of the (AC)3 Project
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Wendisch, M., Brückner, M., Crewell, Susanne, Ehrlich, A., Notholt, J., Lüpkes, C., Macke, A., Burrows, J. P., Rinke, A., Quaas, J., Maturilli, M., Schemann, V., Shupe, M. D., Akansu, E. F., Barrientos-Velasco, C., Bärfuss, K., Blechschmidt, A.-M., Block, K., Bougoudis, I., Bozem, H., Böckmann, C., Bracher, A., Bresson, H., Bretschneider, L., Buschmann, M., Chechin, D. G., Chylik, J., Dahlke, S., Deneke, H., Dethloff, K., Donth, T., Dorn, W., Dupuy, R., Ebell, K., Egerer, U., Engelmann, R., Eppers, O., Gerdes, R., Gierens, R., Gorodetskaya, I. V., Gottschalk, M., Griesche, H., Gryanik, V. M., Handorf, D., Harm-Altstädter, B., Hartmann, J., Hartmann, M., Heinold, B., Herber, A., Herrmann, H., Heygster, G., Höschel, I., Hofmann, Z., Hölemann, J., Hünerbein, A., Jafariserajehlou, S., Jäkel, E., Jacobi, C., Janout, M., Jansen, F., Jourdan, O., Jurányi, Z., Kalesse-Los, H., Kanzow, T., Käthner, R., Kliesch, L. L., Klingebiel, M., Knudsen, E. M., Kovács, T., Körtke, W., Krampe, D., Kretzschmar, J., Kreyling, D., Kulla, B., Kunkel, D., Lampert, A., Lauer, M., Lelli, L., von Lerber, A., Linke, O., Löhnert, U., Lonardi, M., Losa, S. N., Losch, M., Maahn, M., Mech, M., Mei, L., Mertes, S., Metzner, E., Mewes, D., Michaelis, J., Mioche, G., Moser, Manuel, Nakoudi, K., Neggers, R., Neuber, R., Nomokonova, T., Oelker, J., Papakonstantinou-Presvelou, I., Pätzold, F., Pefanis, V., Pohl, C., van Pinxteren, M., Radovan, A., Rhein, M., Rex, Markus, Richter, A., Risse, N., Ritter, C., Rostosky, P., Rozanov, V. V., Ruiz Donoso, E., Saavedra-Garfias, P., Salzmann, M., Schacht, J., Schäfer, M., Schneider, J., Schnierstein, N., Seifert, P., Seo, S., Siebert, H., Soppa, M. A., Spreen, G., Stachlewska, I. S., Stapf, J., Stratmann, F., Tegen, I., Viceto, C., Voigt, Christiane, Vountas, M., Walbröl, A., Walter, M., Wehner, B., Wex, H., Willmes, S., Zanatta, M., Zeppenfeld, S., Laboratoire de Météorologie Physique (LaMP), and Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)
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Atmospheric Science ,[SDU]Sciences of the Universe [physics] ,clouds ,Arctic amplification - Abstract
Mechanisms behind the phenomenon of Arctic amplification are widely discussed. To contribute to this debate, the (AC)3 project was established in 2016 (www.ac3-tr.de/). It comprises modeling and data analysis efforts as well as observational elements. The project has assembled a wealth of ground-based, airborne, shipborne, and satellite data of physical, chemical, and meteorological properties of the Arctic atmosphere, cryosphere, and upper ocean that are available for the Arctic climate research community. Short-term changes and indications of long-term trends in Arctic climate parameters have been detected using existing and new data. For example, a distinct atmospheric moistening, an increase of regional storm activities, an amplified winter warming in the Svalbard and North Pole regions, and a decrease of sea ice thickness in the Fram Strait and of snow depth on sea ice have been identified. A positive trend of tropospheric bromine monoxide (BrO) column densities during polar spring was verified. Local marine/biogenic sources for cloud condensation nuclei and ice nucleating particles were found. Atmospheric–ocean and radiative transfer models were advanced by applying new parameterizations of surface albedo, cloud droplet activation, convective plumes and related processes over leads, and turbulent transfer coefficients for stable surface layers. Four modes of the surface radiative energy budget were explored and reproduced by simulations. To advance the future synthesis of the results, cross-cutting activities are being developed aiming to answer key questions in four focus areas: lapse rate feedback, surface processes, Arctic mixed-phase clouds, and airmass transport and transformation.
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- 2023
- Full Text
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5. STATE OF THE CLIMATE IN 2011 Special Supplement to the Bulletin of the American Meteorological Society Vol. 93, No. 7, July 2012
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Achberger, C, Ackerman, SA, Ahmed, FH, Albanil-Encarnacion, A, Alfaro, EJ, Alves, LM, Allan, R, Amador, JA, Ambenje, P, Antoine, MD, Antonov, J, Arevalo, J, Arndt, DS, Ashik, I, Atheru, Z, Baccini, A, Baez, J, Banzon, V, Baringer, MO, Barreira, S, Barriopedro, DE, Bates, JJ, Becker, A, Behrenfeld, MJ, Bell, GD, Benedetti, A, Bernhard, G, Berrisford, P, Berry, DI, Beszczynska-Moeller, A, Bhatt, US, Bidegain, M, Bieniek, P, Birkett, C, Bissolli, P, Blake, ES, Blunden, J, Boudet-Rouco, D, Box, JE, Boyer, T, Braathen, GO, Brackenridge, GR, Brohan, P, Bromwich, DH, Brown, L, Brown, R, Bruhwiler, L, Bulygina, ON, Burrows, J, Calderon, B, Camargo, SJ, Cappellen, J, Carmack, E, Carrasco, G, Chambers, DP, Christiansen, HH, Christy, J, Chung, D, Ciais, P, Coehlo, CAS, Colwell, S, Comiso, J, Cretaux, J-F, Crouch, J, Cunningham, SA, De Jeu, RAM, Demircan, M, Derksen, C, Diamond, HJ, Dlugokencky, EJ, Dohan, K, Dolman, AJ, Dorigo, WA, Drozdov, DS, Duguay, C, Dutton, E, Dutton, GS, Elkins, JW, Epstein, HE, Famiglietti, JS, Fanton d'Andon, OH, Feely, RA, Fekete, BM, Fenimore, C, Fernandez-Prieto, D, Fields, E, Fioletov, V, Fogt, RL, Folland, C, Foster, MJ, Frajka-Williams, E, Franz, BA, Frey, K, Frith, SH, Frolov, I, Frost, GV, Ganter, C, Garzoli, S, Gitau, W, and Gleason, KL
- Published
- 2012
6. State of the climate in 2010
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Achberger, C, Ackerman, SA, Ahlstrøm, A, Alfaro, EJ, Allan, RJ, Alves, L, Amador, JA, Amelie, V, Andrianjafinirina, S, Antonov, J, Arndt, DS, Ashik, I, Atheru, Z, Attaher, SM, Baez, J, Banzon, V, Baringer, MO, Barreira, S, Barriopedro, D, Barthia, PK, Beal, LM, Becker, A, Behrenfeld, MJ, Bell, GD, Belward, AS, Benedetti, A, Berrisford, P, Berry, DI, Beszczynska-Moeller, A, Bhatt, US, Bidegain, M, Bindoff, NL, Bissolli, P, Blake, ES, Blunden, J, Booneeady, P, Bosilovich, MG, Boudet, DR, Box, JE, Boyer, TP, Bromwich, DH, Brown, R, Bryden, HL, Bulygina, ON, Burrows, J, Butler, J, Cais, P, Calderon, B, Callaghan, TV, Camargo, SJ, Cappelen, J, Carmack, E, Chambers, DP, Chelliah, M, Chidichimo, MP, Christiansen, H, Christy, J, Coelho, CAS, Colwell, S, Comiso, JC, Compo, GP, Crouch, J, Cunningham, SA, Cutié, VC, Dai, A, Davydova-Belitskaya, V, De Jeu, R, Decker, D, Dee, D, Demircan, M, Derksen, C, Diamond, HJ, Dlugokencky, EJ, Dohan, K, Dolman, AJ, Dorigo, W, Drozdov, DS, Durack, PJ, Dutton, GS, Easterling, D, Ebita, A, Eischeid, J, Elkins, JW, Epstein, HE, Euscátegui, C, Faijka-Williams, E, Famiglietti, JS, Faniriantsoa, R, Feely, RA, Fekete, BM, Fenimore, C, and Fettweis, X
- Abstract
Several large-scale climate patterns influenced climate conditions and weather patterns across the globe during 2010. The transition from a warm El Niño phase at the beginning of the year to a cool La Niña phase by July contributed to many notable events, ranging from record wetness across much of Australia to historically low Eastern Pacific basin and near-record high North Atlantic basin hurricane activity. The remaining five main hurricane basins experienced below- to well-below-normal tropical cyclone activity. The negative phase of the Arctic Oscillation was a major driver of Northern Hemisphere temperature patterns during 2009/10 winter and again in late 2010. It contributed to record snowfall and unusually low temperatures over much of northern Eurasia and parts of the United States, while bringing above-normal temperatures to the high northern latitudes. The February Arctic Oscillation Index value was the most negative since records began in 1950. The 2010 average global land and ocean surface temperature was among the two warmest years on record. The Arctic continued to warm at about twice the rate of lower latitudes. The eastern and tropical Pacific Ocean cooled about 1°C from 2009 to 2010, reflecting the transition from the 2009/10 El Niño to the 2010/11 La Niña. Ocean heat fluxes contributed to warm sea surface temperature anomalies in the North Atlantic and the tropical Indian and western Pacific Oceans. Global integrals of upper ocean heat content for the past several years have reached values consistently higher than for all prior times in the record, demonstrating the dominant role of the ocean in the Earth's energy budget. Deep and abyssal waters of Antarctic origin have also trended warmer on average since the early 1990s. Lower tropospheric temperatures typically lag ENSO surface fluctuations by two to four months, thus the 2010 temperature was dominated by the warm phase El Niño conditions that occurred during the latter half of 2009 and early 2010 and was second warmest on record. The stratosphere continued to be anomalously cool. Annual global precipitation over land areas was about five percent above normal. Precipitation over the ocean was drier than normal after a wet year in 2009. Overall, saltier (higher evaporation) regions of the ocean surface continue to be anomalously salty, and fresher (higher precipitation) regions continue to be anomalously fresh. This salinity pattern, which has held since at least 2004, suggests an increase in the hydrological cycle. Sea ice conditions in the Arctic were significantly different than those in the Antarctic during the year. The annual minimum ice extent in the Arctic-reached in September-was the third lowest on record since 1979. In the Antarctic, zonally averaged sea ice extent reached an all-time record maximum from mid-June through late August and again from mid-November through early December. Corresponding record positive Southern Hemisphere Annular Mode Indices influenced the Antarctic sea ice extents. Greenland glaciers lost more mass than any other year in the decade-long record. The Greenland Ice Sheet lost a record amount of mass, as the melt rate was the highest since at least 1958, and the area and duration of the melting was greater than any year since at least 1978. High summer air temperatures and a longer melt season also caused a continued increase in the rate of ice mass loss from small glaciers and ice caps in the Canadian Arctic. Coastal sites in Alaska show continuous permafrost warming and sites in Alaska, Canada, and Russia indicate more significant warming in relatively cold permafrost than in warm permafrost in the same geographical area. With regional differences, permafrost temperatures are now up to 2°C warmer than they were 20 to 30 years ago. Preliminary data indicate there is a high probability that 2010 will be the 20th consecutive year that alpine glaciers have lost mass. Atmospheric greenhouse gas concentrations continued to rise and ozone depleting substances continued to decrease. Carbon dioxide increased by 2.60 ppm in 2010, a rate above both the 2009 and the 1980-2010 average rates. The global ocean carbon dioxide uptake for the 2009 transition period from La Niña to El Niño conditions, the most recent period for which analyzed data are available, is estimated to be similar to the long-term average. The 2010 Antarctic ozone hole was among the lowest 20% compared with other years since 1990, a result of warmer-than-average temperatures in the Antarctic stratosphere during austral winter between mid-July and early September.
- Published
- 2011
7. How Much CO₂ Is Taken Up by the European Terrestrial Biosphere?
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Reuter, M., Buchwitz, M., Hilker, M., Heymann, J., Bovensmann, H., Burrows, J. P., Houweling, S., Liu, Y. Y., Nassar, R., Chevallier, F., Ciais, P., Marshall, J., and Reichstein, M.
- Published
- 2017
8. Quantitative proteomic analysis of HER2 expression in the selection of gastric cancer patients for trastuzumab treatment
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An, E., Ock, C.-Y., Kim, T.-Y., Lee, K.-H., Han, S.-W., Im, S.-A., Liao, W.-L., Cecchi, F., Blackler, A., Thyparambil, S., Kim, W.H., Burrows, J., Hembrough, T., Catenacci, D.V.T., Oh, D.-Y., and Bang, Y.-J.
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- 2017
- Full Text
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9. Nucleon-Nucleon and Pion-Nucleon Potentials from Phase Shifts using Quantum Inversion
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Sander, M., Beck, C., Schroeder, B. C., Pyo, H. -B., Becker, H., Burrows, J., von Geramb, H. V., Wu, Y., and Ishikawa, S.
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Nuclear Theory - Abstract
NN and Pi-N partial wave radial potentials have been generated using the latest SM94-VPI(NN) and FA93-VPI(Pi-N) phase shifts. The potentials are used to determine the deuteron properties and to compute the 3H and 3He binding energies. The e_1 mixing angles of SM94-VPI and NY93-Nijmegen differ significantly and inversion potentials yield a P_d of 6.37% and 5.78%, respectively. Underbinding of 3H and 3He is enhanced by SM94, which signals more nonlocality and/or three-body potential effects than predicted from Nijmegen phase shifts and boson exchange models. The local pion-nucleon S_31, P_31 and P_33 channel potentials have been generated for guidance and to obtain a quantitative impression in r-space of what the Pi-N FA93-VPI phase shifts imply., Comment: Presented at the International Conference on Physics with GeV Particle Beams, August 22.-25., 1994, Juelich, Germany. 4 Pages LaTeX, 6 Pictures (you need epsfig.sty)
- Published
- 1994
10. Prey density and depth affect the fine-scale foraging behavior of humpback whales Megaptera novaeangliae in Sitka Sound, Alaska, USA
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Burrows, J. A., Johnston, D. W., Straley, J. M., Chenoweth, E. M., Ware, C., Curtice, C., DeRuiter, S. L., and Friedlaender, A. S.
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- 2016
11. Ability of the 4-D-Var analysis of the GOSAT BESD XCO2 retrievals to characterize atmospheric CO2 at large and synoptic scales
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Massart, S., Agustí-Panareda, A., Heymann, J., Buchwitz, M., Chevallier, F., Reuter, M., Hilker, M., Burrows, J., Hase, F., Desmet, F., Feist, D., Kivi, R., Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), and 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)
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[SDU]Sciences of the Universe [physics] - Abstract
This study presents results from the European Centre for Medium-RangeWeather Forecasts (ECMWF) carbon dioxide (CO2) analysis system where the atmospheric CO2 is controlled through the assimilation of columnaveraged dry-air mole fractions of CO2 (XCO2) from the Greenhouse gases Observing Satellite (GOSAT). The analysis is compared to a free-run simulation (without assimilation of XCO2), and they are both evaluated against XCO2 data from the Total Carbon Column Observing Network (TCCON). We show that the assimilation of the GOSAT XCO2 product from the Bremen Optimal Estimation Differential Optical Absorption Spectroscopy (BESD) algorithm during the year 2013 provides XCO2 fields with an improved mean absolute error of 0.6 parts per million (ppm) and an improved station-to-station bias deviation of 0.7 ppm compared to the free run (1.1 and 1.4 ppm, respectively) and an improved estimated precision of 1 ppm compared to the GOSAT BESD data (3.3 ppm). We also show that the analysis has skill for synoptic situations in the vicinity of frontal systems, where the GOSAT retrievals are sparse due to cloud contamination. We finally computed the 10-day forecast from each analysis at 00:00 UTC, and we demonstrate that the CO2 forecast shows synoptic skill for the largest-scale weather patterns (of the order of 1000 km) even up to day 5 compared to its own analysis.
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- 2023
12. Two Laws
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Burrows, J, Finn, J, Dorsett, S, Burrows, J, Finn, J, and Dorsett, S
- Published
- 2022
13. Immunotherapy: EPHRIN RECEPTOR A3–TARGETED CAR T CELL IMMUNOTHERAPY FOR GLIOBLASTOMA
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Martins, P., primary, Ranjankumar, M., additional, Burrows, J., additional, Smith, C., additional, and Khanna, R., additional
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- 2022
- Full Text
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14. A Review of the Literature on Computational Errors With Whole Numbers. Mathematics Education Diagnostic and Instructional Centre (MEDIC).
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British Columbia Univ., Vancouver. Faculty of Education. and Burrows, J. K.
- Abstract
Research on error patterns associated with whole number computation is reviewed. Details of the results of some of the individual studies cited are given in the appendices. In Appendix A, 33 addition errors, 27 subtraction errors, 41 multiplication errors, and 41 division errors are identified, and the frequency of these errors made by 352 children in grades three through six is tabulated. Appendix B records the 68 errors in multiplication made by 2100 students in grades four through six. Appendix C lists 57 errors in long division with a one-digit divisor made by 453 children in grades five through eight. In Appendix D, the twelve difficulties most often noted for each of the four operations are identified and responses of 516 children from grades four through eight are tabulated. Appendix E gives examples of six types of errors for addition, subtraction, and multiplication, and four types of errors for division. Appendix F records the persistence of errors made by a group of 221 fourth graders learning division when the divisor was a 2-digit number. Appendix G gives examples of 46 common computation errors which children make in computing with whole numbers. (DT)
- Published
- 1976
15. Quantification of CH4 coal mining emissions in Upper Silesia by passive airborne remote sensing observations with the Methane Airborne MAPper (MAMAP) instrument during the CO2 and Methane (CoMet) campaign
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Krautwurst, S., Gerilowski, K., Borchardt, J., Wildmann, N., Galkowski, M., Swolkien, J., Marshall, J., Fiehn, A., Roiger, A., Ruhtz, T., Gerbig, C., Necki, J., Burrows, J., Fix, A., and Bovensmann, H.
- Abstract
Methane (CH4) is the second most important anthropogenic greenhouse gas, whose atmospheric concentration is modulated by human-induced activities, and it has a larger global warming potential than carbon dioxide (CO2). Because of its short atmospheric lifetime relative to that of CO2, the reduction of the atmospheric abundance of CH4 is an attractive target for short-term climate mitigation strategies. However, reducing the atmospheric CH4 concentration requires a reduction of its emissions and, therefore, knowledge of its sources. For this reason, the CO2 and Methane (CoMet) campaign in May and June 2018 assessed emissions of one of the largest CH4 emission hot spots in Europe, the Upper Silesian Coal Basin (USCB) in southern Poland, using top-down approaches and inventory data. In this study, we will focus on CH4 column anomalies retrieved from spectral radiance observations, which were acquired by the 1D nadir-looking passive remote sensing Methane Airborne MAPper (MAMAP) instrument, using the weighting-function-modified differential optical absorption spectroscopy (WFM-DOAS) method. The column anomalies, combined with wind lidar measurements, are inverted to cross-sectional fluxes using a mass balance approach. With the help of these fluxes, reported emissions of small clusters of coal mine ventilation shafts are then assessed. The MAMAP CH4 column observations enable an accurate assignment of observed fluxes to small clusters of ventilation shafts. CH4 fluxes are estimated for four clusters with a total of 23 ventilation shafts, which are responsible for about 40 % of the total CH4 mining emissions in the target area. The observations were made during several overflights on different days. The final average CH4 fluxes for the single clusters (or sub-clusters) range from about 1 to 9 t CH4 h−1 at the time of the campaign. The fluxes observed at one cluster during different overflights vary by as much as 50 % of the average value. Associated errors (1σ) are usually between 15 % and 59 % of the average flux, depending mainly on the prevailing wind conditions, the number of flight tracks, and the magnitude of the flux itself. Comparison to known hourly emissions, where available, shows good agreement within the uncertainties. If only emissions reported annually are available for comparison with the observations, caution is advised due to possible fluctuations in emissions during a year or even within hours. To measure emissions even more precisely and to break them down further for allocation to individual shafts in a complex source region such as the USCB, imaging remote sensing instruments are recommended.
- Published
- 2021
16. Identification of RBCK1 as a novel regulator of FKBPL: implications for tumor growth and response to tamoxifen
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Donley, C, McClelland, K, McKeen, H D, Nelson, L, Yakkundi, A, Jithesh, P V, Burrows, J, McClements, L, Valentine, A, Prise, K M, McCarthy, H O, and Robson, T
- Published
- 2014
- Full Text
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17. Persistent Problems in System Development.
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Mitre Corp., Bedford, MA. and Burrows, J. H.
- Abstract
Technological innovation in the form of the introduction of a formal information system represents change to the people within the organization. This paper (presented to California Educational Administrators participating in the Executive Information Systems program of Operation PEP--Prepare Educational Planners) is directed to those managers who initiate the introduction of a new system and are responsible for the successful assimilation of it into their organization. Such a change presents problems, which if not approached correctly, can negate any anticipated benefits. Problems of organization involve the top management, middle managers and the bottom of the organizational structure. As institutors of a new information system, the top-level managers must be certain that those below them feel and derive benefits as active participants in the system design, development and use. Problems of change and growth encompass: (1) changes in information flow and availability, (2) personnel growth, (3) applications, (4) cost, and (5) new employees. The problems resulting from the consideration of standards versus adaptability when contemplating a new information system must be settled by top management in light of the particular needs of their organization so that it will be flexible and workable. (SG)
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- 1970
18. Information System Overview.
- Author
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Mitre Corp., Bedford, MA. and Burrows, J. H.
- Abstract
This paper was prepared for distribution to the California Educational Administrators participating in the "Executive Information Systems" Unit of Instruction as part of the instructional program of Operation PEP (Prepare Educational Planners). The purpose of the course was to introduce some basic concepts of information systems technology to administrators to provide them with a broader perspective on information systems as pertaining to organizational and educational needs and to acquaint them with some of the problems associated with computer-based information systems. (AB)
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- 1970
19. Atmospheric and Surface Processes, and Feedback Mechanisms Determining Arctic Amplification: A Review of First Results and Prospects of the (AC) 3 Project.
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Wendisch, M., Brückner, M., Crewell, S., Ehrlich, A., Notholt, J., Lüpkes, C., Macke, A., Burrows, J. P., Rinke, A., Quaas, J., Maturilli, M., Schemann, V., Shupe, M. D., Akansu, E. F., Barrientos-Velasco, C., Bärfuss, K., Blechschmidt, A.-M., Block, K., Bougoudis, I., and Bozem, H.
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CLOUD condensation nuclei ,ENERGY budget (Geophysics) ,ARCTIC climate ,ICE nuclei ,WINTER storms ,CLIMATE research ,SEA ice - Abstract
Mechanisms behind the phenomenon of Arctic amplification are widely discussed. To contribute to this debate, the (AC)3 project was established in 2016 (www.ac3-tr.de/). It comprises modeling and data analysis efforts as well as observational elements. The project has assembled a wealth of ground-based, airborne, shipborne, and satellite data of physical, chemical, and meteorological properties of the Arctic atmosphere, cryosphere, and upper ocean that are available for the Arctic climate research community. Short-term changes and indications of long-term trends in Arctic climate parameters have been detected using existing and new data. For example, a distinct atmospheric moistening, an increase of regional storm activities, an amplified winter warming in the Svalbard and North Pole regions, and a decrease of sea ice thickness in the Fram Strait and of snow depth on sea ice have been identified. A positive trend of tropospheric bromine monoxide (BrO) column densities during polar spring was verified. Local marine/biogenic sources for cloud condensation nuclei and ice nucleating particles were found. Atmospheric–ocean and radiative transfer models were advanced by applying new parameterizations of surface albedo, cloud droplet activation, convective plumes and related processes over leads, and turbulent transfer coefficients for stable surface layers. Four modes of the surface radiative energy budget were explored and reproduced by simulations. To advance the future synthesis of the results, cross-cutting activities are being developed aiming to answer key questions in four focus areas: lapse rate feedback, surface processes, Arctic mixed-phase clouds, and airmass transport and transformation. [ABSTRACT FROM AUTHOR]
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- 2023
- Full Text
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20. Immersive placement experiences promote rural intent in allied health students of urban and rural origin
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Wolfgang R, Wakely L, Smith T, Burrows J, Little A, and Brown LJ
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lcsh:R5-920 ,Australia ,rural health services ,career intentions ,lcsh:Medicine (General) ,mixed method ,student placements - Abstract
Rebecca Wolfgang,1 Luke Wakely,1 Tony Smith,2 Julie Burrows,1 Alexandra Little,1 Leanne J Brown11Tamworth Education Centre, University of Newcastle Department of Rural Health, Tamworth, NSW 2340, Australia; 2Manning Education Centre, University of Newcastle Department of Rural Health, Taree, NSW 2430, AustraliaCorrespondence: Rebecca WolfgangTamworth Education Centre, University of Newcastle Department of Rural Health, 114-148 Johnston Street, Tamworth, NSW 2340, AustraliaTel +61 26 755 3515Fax +61 26 761 2355Email rebecca.wolfgang@newcastle.edu.auIntroduction: Pre-vocational placement experiences are known to considerably influence the career preferences of health graduates and are a key factor in growing the rural allied health workforce. This paper explores the rural placement experiences and future work intentions of students who attended a placement with the University of Newcastle Department of Rural Health.Methods: Part of a larger longitudinal mixed methods study of students’ placement experiences and subsequent career choices, this study explored students’ placement evaluations responses. Following each placement, students were invited to complete an online survey which asked about their placement experiences and future work intentions. Counts and proportion tests were performed for frequencies of quantitative variables. Wilcoxon signed rank tests were conducted on the paired pre- and post-rural intent scores to determine any perceived differences in intent before and after placement for students both with and without a rural background. Qualitative data from short answer questions were analyzed thematically guided by qualitative content analysis. Data were comparatively analyzed for students of a rural or urban background.Results: Four hundred and forty end of placement surveys were completed by 275 students (response rate 69.8%). There was a positive shift in intention to work rurally for students of both rural and urban background post-placement, but this was only statistically significant in the group from an urban background (p≤0.001). From the qualitative analysis three themes emerged: immersed rural supported placement experience, immersed interaction in rural life with other students, and immersed interaction in the rural community. Students from both rural and urban backgrounds indicated similar benefits and challenges.Conclusion: While the positive impact of rural placement experiences and rural background on future rural practice is well known, this study highlights the importance of positive supported placement experience for students from both rural and urban backgrounds.Keywords: rural health services, student placements, mixed method, career intentions, Australia
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- 2019
21. Is Planning Really Necessary?: Discussion
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Balchin, W. G. V., Green, F. H. W., Burrows, J. W., Bridgeman, J., Munro, Neil, Blake, R. N. E., and Coleman, Alice
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- 1976
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22. Anna Boleyn and the Authenticity of Fielding's Feminine Narratives
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Burrows, J. F. and Hassall, Anthony J.
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- 1988
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23. Energetic Charged-Particle Phenomena in the Jovian Magnetosphere: First Results from the Ulysses COSPIN Collaboration
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Simpson, J. A., Anglin, J. D., Balogh, A., Burrows, J. R., Cowley, S. W. H., Ferrando, P., Heber, B., Hynds, R. J., Kunow, H., Marsden, R. G., McKibben, R. B., Müller-Mellin, R., Page, D. E., Raviart, A., Sanderson, T. R., Staines, K., Wilson, Margaret D., and Zhang, M.
- Published
- 1992
24. Atmospheric Reactions of the HO 2 Radical Studied by Laser Magnetic Resonance Spectroscopy
- Author
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Burrows, J. P., Cliff, D. I., Harris, G. W., Thrush, B. A., and Wilkinson, J. P. T.
- Published
- 1979
25. Contractual Co-operation and the Implied Term
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Burrows, J. F.
- Published
- 1968
26. Feedback of atmospheric composition and ocean colour to Arctic amplification
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Blechschmidt, A.-M., Bougoudis, I., Bracher, A., Burrows, J. P., Losa, S., Richter, A., Seo, S., Bösch, T., Zeising, M., Zilker, B., Blechschmidt, A.-M., Bougoudis, I., Bracher, A., Burrows, J. P., Losa, S., Richter, A., Seo, S., Bösch, T., Zeising, M., and Zilker, B.
- Published
- 2021
27. Retrieval And Monitoring of Atmospheric Trace Gas Concentrations in Nadir and Limb Geometry Using the Space-Borne Sciamachy Instrument
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Sierk, B., Richter, A., Rozanov, A., Savigny, Ch. Von, Schmoltner, A. M., Buchwitz, M., Bovensmann, H., and Burrows, J. P.
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- 2006
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28. Gender differences in mortality and quality of life after septic shock: A post-hoc analysis of the ARISE study
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Luethi, N, Bailey, M, Higgins, A, Howe, B, Peake, S, Delaney, A, Bellomo, R, Bennett, V, Board, J, McCracken, P, McGloughlin, S, Nanjayya, V, Teo, A, Hill, E, O'Brien, PJE, Sawtell, F, Schimanski, K, Wilson, D, Bolch, S, Eastwood, G, Kerr, F, Peak, L, Young, H, Edington, J, Fletcher, J, Smith, J, Ghelani, D, Nand, K, Sara, T, Cross, A, Flemming, D, Grummisch, M, Purdue, A, Fulton, E, Grove, K, Harney, A, Milburn, K, Millar, R, Mitchell, I, Rodgers, H, Scanlon, S, Coles, T, Connor, H, Dennett, J, Van Berkel, A, Barrington-Onslow, S, Henderson, S, Mehrtens, J, Dryburgh, J, Tankel, A, Braitberg, G, O'Bree, B, Shepherd, K, Vij, S, Allsop, S, Haji, D, Haji, K, Vuat, J, Bone, A, Elderkin, T, Orford, N, Ragg, M, Kelly, S, Stewart, D, Woodward, N, Harjola, V-P, Pettila, MO, Sutinen, S, Wilkman, E, Fratzia, J, Halkhoree, J, Treloar, S, Ryan, K, Sandford, T, Walsham, J, Jenkins, C, Williamson, D, Burrows, J, Hawkins, D, Tang, C, Dimakis, A, Holdgate, A, Micallef, S, Parr, M, White, H, Morrison, L, Sosnowski, K, Ramadoss, R, Soar, N, Wood, J, Franks, M, Williams, A, Hogan, C, Song, R, Tilsley, A, Rainsford, D, Wells, R, Dowling, J, Galt, P, Lamac, T, Lightfoot, D, Walker, C, Braid, K, DeVillecourt, T, Tan, HS, Seppelt, I, Chang, LF, Cheung, WS, Fok, SK, Lam, PK, Lam, SM, So, HM, Yan, W, Altea, A, Lancashire, B, Gomersall, CD, Graham, CA, Leung, P, Arora, S, Bass, F, Shehabi, Y, Isoardi, J, Isoardi, K, Powrie, D, Lawrence, S, Ankor, A, Chester, L, Davies, M, O'Connor, S, Poole, A, Soulsby, T, Sundararajan, K, Williams, J, Greenslade, JH, MacIsaac, C, Gorman, K, Jordan, A, Moore, L, Ankers, S, Bird, S, Fogg, T, Hickson, E, Jewell, T, Kyneur, K, O'Connor, A, Townsend, J, Yarad, E, Brown, S, Chamberlain, J, Cooper, J, Jenkinson, E, McDonald, E, Webb, S, Buhr, H, Coakley, J, Cowell, J, Hutch, D, Gattas, D, Keir, M, Rajbhandari, D, Rees, C, Baker, S, Roberts, B, Farone, E, Holmes, J, Santamaria, J, Winter, C, Finckh, A, Knowles, S, McCabe, J, Nair, P, Reynolds, C, Ahmed, B, Barton, D, Meaney, E, Nichol, A, Harris, R, Shields, L, Thomas, K, Karlsson, S, Kuitunen, A, Kukkurainen, A, Tenhunen, J, Varila, S, Ryan, N, Trethewy, C, Crosdale, J, Smith, JC, Vellaichamy, M, Furyk, J, Gordon, G, Jones, L, Senthuran, S, Bates, S, Butler, J, French, C, Tippett, A, Kelly, J, Kwans, J, Murphy, M, O'Flynn, D, Kurenda, C, Otto, T, Raniga, V, Williams, P, Ho, HF, Leung, A, Wu, H, Luethi, N, Bailey, M, Higgins, A, Howe, B, Peake, S, Delaney, A, Bellomo, R, Bennett, V, Board, J, McCracken, P, McGloughlin, S, Nanjayya, V, Teo, A, Hill, E, O'Brien, PJE, Sawtell, F, Schimanski, K, Wilson, D, Bolch, S, Eastwood, G, Kerr, F, Peak, L, Young, H, Edington, J, Fletcher, J, Smith, J, Ghelani, D, Nand, K, Sara, T, Cross, A, Flemming, D, Grummisch, M, Purdue, A, Fulton, E, Grove, K, Harney, A, Milburn, K, Millar, R, Mitchell, I, Rodgers, H, Scanlon, S, Coles, T, Connor, H, Dennett, J, Van Berkel, A, Barrington-Onslow, S, Henderson, S, Mehrtens, J, Dryburgh, J, Tankel, A, Braitberg, G, O'Bree, B, Shepherd, K, Vij, S, Allsop, S, Haji, D, Haji, K, Vuat, J, Bone, A, Elderkin, T, Orford, N, Ragg, M, Kelly, S, Stewart, D, Woodward, N, Harjola, V-P, Pettila, MO, Sutinen, S, Wilkman, E, Fratzia, J, Halkhoree, J, Treloar, S, Ryan, K, Sandford, T, Walsham, J, Jenkins, C, Williamson, D, Burrows, J, Hawkins, D, Tang, C, Dimakis, A, Holdgate, A, Micallef, S, Parr, M, White, H, Morrison, L, Sosnowski, K, Ramadoss, R, Soar, N, Wood, J, Franks, M, Williams, A, Hogan, C, Song, R, Tilsley, A, Rainsford, D, Wells, R, Dowling, J, Galt, P, Lamac, T, Lightfoot, D, Walker, C, Braid, K, DeVillecourt, T, Tan, HS, Seppelt, I, Chang, LF, Cheung, WS, Fok, SK, Lam, PK, Lam, SM, So, HM, Yan, W, Altea, A, Lancashire, B, Gomersall, CD, Graham, CA, Leung, P, Arora, S, Bass, F, Shehabi, Y, Isoardi, J, Isoardi, K, Powrie, D, Lawrence, S, Ankor, A, Chester, L, Davies, M, O'Connor, S, Poole, A, Soulsby, T, Sundararajan, K, Williams, J, Greenslade, JH, MacIsaac, C, Gorman, K, Jordan, A, Moore, L, Ankers, S, Bird, S, Fogg, T, Hickson, E, Jewell, T, Kyneur, K, O'Connor, A, Townsend, J, Yarad, E, Brown, S, Chamberlain, J, Cooper, J, Jenkinson, E, McDonald, E, Webb, S, Buhr, H, Coakley, J, Cowell, J, Hutch, D, Gattas, D, Keir, M, Rajbhandari, D, Rees, C, Baker, S, Roberts, B, Farone, E, Holmes, J, Santamaria, J, Winter, C, Finckh, A, Knowles, S, McCabe, J, Nair, P, Reynolds, C, Ahmed, B, Barton, D, Meaney, E, Nichol, A, Harris, R, Shields, L, Thomas, K, Karlsson, S, Kuitunen, A, Kukkurainen, A, Tenhunen, J, Varila, S, Ryan, N, Trethewy, C, Crosdale, J, Smith, JC, Vellaichamy, M, Furyk, J, Gordon, G, Jones, L, Senthuran, S, Bates, S, Butler, J, French, C, Tippett, A, Kelly, J, Kwans, J, Murphy, M, O'Flynn, D, Kurenda, C, Otto, T, Raniga, V, Williams, P, Ho, HF, Leung, A, and Wu, H
- Abstract
PURPOSE: To assess the impact of gender and pre-menopausal state on short- and long-term outcomes in patients with septic shock. MATERIAL AND METHODS: Cohort study of the Australasian Resuscitation in Sepsis Evaluation (ARISE) trial, an international randomized controlled trial comparing early goal-directed therapy (EGDT) to usual care in patients with early septic shock, conducted between October 2008 and April 2014. The primary exposure in this analysis was legal gender and the secondary exposure was pre-menopausal state defined by chronological age (≤ 50 years). RESULTS: 641 (40.3%) of all 1591 ARISE trial participants in the intention-to-treat population were females and overall, 337 (21.2%) (146 females) patients were 50 years of age or younger. After risk-adjustment, we could not identify any survival benefit for female patients at day 90 in the younger (≤50 years) (adjusted Odds Ratio (aOR): 0.91 (0.46-1.89), p = .85) nor in the older (>50 years) age-group (aOR: 1.10 (0.81-1.49), p = .56). Similarly, there was no gender-difference in ICU, hospital, 1-year mortality nor quality of life measures. CONCLUSIONS: This post-hoc analysis of a large multi-center trial in early septic shock has shown no short- or long-term survival effect for women overall as well as in the pre-menopausal age-group.
- Published
- 2020
29. Estimating local need for mental healthcare to inform fair resource allocation in the NHS in England: cross-sectional analysis of national administrative data linked at person level.
- Author
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Anselmi, L, Everton, A, Shaw, R, Suzuki, W, Burrows, J, Weir, R, Tatarek-Gintowt, R, Sutton, M, Lorrimer, S, Anselmi, L, Everton, A, Shaw, R, Suzuki, W, Burrows, J, Weir, R, Tatarek-Gintowt, R, Sutton, M, and Lorrimer, S
- Abstract
BACKGROUND: Equitable access to mental healthcare is a priority for many countries. The National Health Service in England uses a weighted capitation formula to ensure that the geographical distribution of resources reflects need.AimsTo produce a revised formula for estimating local need for secondary mental health, learning disability (intellectual disability) and psychological therapies services for adults in England. METHOD: We used demographic records for 43 751 535 adults registered with a primary care practitioner in England linked with service use, ethnicity, physical health diagnoses and type of household, from multiple data-sets. Using linear regression, we estimated the individual cost of care in 2015 as a function of individual- and area-level need and supply variables in 2013 and 2014. We sterilised the effects of the supply variables to obtain individual-need estimates. We aggregated these by general practitioner practice, age and gender to derive weights for the national capitation formula. RESULTS: Higher costs were associated with: being 30-50 years old, compared with 20-24; being Irish, Black African, Black Caribbean or of mixed ethnicity, compared with White British; having been admitted for specific physical health conditions, including drug poisoning; living alone, in a care home or in a communal environment; and living in areas with a higher percentage of out-of-work benefit recipients and higher prevalence of severe mental illness. Longer distance from a provider was associated with lower cost. CONCLUSIONS: The resulting needs weights were higher in more deprived areas and informed the distribution of some 12% (£9 bn in 2019/20) of the health budget allocated to local organisations for 2019/20 to 2023/24.Declaration of interestNone.
- Published
- 2020
30. A chronology of global air quality
- Author
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Fowler, D., Brimblecombe, P., Burrows, J., Heal, M.R., Grennfelt, P., Stevenson, D.S., Jowett, A., Nemitz, E., Coyle, M., Lui, X., Chang, Y., Fuller, G.W., Sutton, M.A., Klimont, Z., Unsworth, M.H., Vieno, M., Fowler, D., Brimblecombe, P., Burrows, J., Heal, M.R., Grennfelt, P., Stevenson, D.S., Jowett, A., Nemitz, E., Coyle, M., Lui, X., Chang, Y., Fuller, G.W., Sutton, M.A., Klimont, Z., Unsworth, M.H., and Vieno, M.
- Abstract
Air pollution has been recognized as a threat to human health since the time of Hippocrates, ca 400 BC. Successive written accounts of air pollution occur in different countries through the following two millennia until measurements, from the eighteenth century onwards, show the growing scale of poor air quality in urban centres and close to industry, and the chemical characteristics of the gases and particulate matter. The industrial revolution accelerated both the magnitude of emissions of the primary pollutants and the geographical spread of contributing countries as highly polluted cities became the defining issue, culminating with the great smog of London in 1952. Europe and North America dominated emissions and suffered the majority of adverse effects until the latter decades of the twentieth century, by which time the transboundary issues of acid rain, forest decline and ground-level ozone became the main environmental and political air quality issues. As controls on emissions of sulfur and nitrogen oxides (SO2 and NOx) began to take effect in Europe and North America, emissions in East and South Asia grew strongly and dominated global emissions by the early years of the twenty-first century. The effects of air quality on human health had also returned to the top of the priorities by 2000 as new epidemiological evidence emerged. By this time, extensive networks of surface measurements and satellite remote sensing provided global measurements of both primary and secondary pollutants. Global emissions of SO2 and NOx peaked, respectively, in ca 1990 and 2018 and have since declined to 2020 as a result of widespread emission controls. By contrast, with a lack of actions to abate ammonia, global emissions have continued to grow.
- Published
- 2020
31. Prognostic significance of Subjective Global Assessment (SGA) in advanced colorectal cancer
- Author
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Gupta, D, Lammersfeld, C A, Vashi, P G, Burrows, J, Lis, C G, and Grutsch, J F
- Published
- 2005
- Full Text
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32. Intercomparison of Stratospheric Chemistry Models under Polar Vortex Conditions
- Author
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Krämer, M., Müller, Ri., Bovensmann, H., Burrows, J., Brinkmann, J., Röth, E. P., Grooß, J.-U., Müller, Ro., Woyke, Th., Ruhnke, R., Günther, G., Hendricks, J., Lippert, E., Carslaw, K. S., Peter, Th., Zieger, A., Brühl, Ch., Steil, B., Lehmann, R., and McKenna, D. S.
- Published
- 2003
- Full Text
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33. Interpretation of Mid-Stratospheric Arctic Ozone Measurements Using a Photochemical Box-Model
- Author
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Sinnhuber, B.-M., Müller, R., Langer, J., Bovensmann, H., Eyring, V., Klein, U., Trentmann, J., Burrows, J. P., and Künzi, K. F.
- Published
- 1999
- Full Text
- View/download PDF
34. Slant Column Measurements of O3 and NO2 During the NDSC Intercomparison of Zenith-Sky UV-Visible Spectrometers in June 1996
- Author
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Roscoe, H. K., Johnston, P. V., Van Roozendael, M., Richter, A., Sarkissian, A., Roscoe, J., Preston, K. E., Lambert, J-C., Hermans, C., DeCuyper, W., Dzienus, S., Winterrath, T., Burrows, J., Goutail, F., Pommereau, J-P., D'Almeida, E., Hottier, J., Coureul, C., Didier, R., Pundt, I., Bartlett, L. M., McElroy, C. T., Kerr, J. E., Elokhov, A., Giovanelli, G., Ravegnani, F., Premuda, M., Kostadinov, I., Erle, F., Wagner, T., Pfeilsticker, K., Kenntner, M., Marquard, L. C., Gil, M., Puentedura, O., Yela, M., Arlander, D. W., Kastad Hoiskar, B. A., Tellefsen, C. W., Karlsen Tornkvist, K., Heese, B., Jones, R. L., Aliwell, S. R., and Freshwater, R. A.
- Published
- 1999
- Full Text
- View/download PDF
35. Study of Free Radical Reactions by Laser Magnetic Resonance
- Author
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Burrows, J. P.
- Subjects
543.5 - Published
- 1978
36. Spectroscopic investigation of sup(222,223)Th and sup(220)Ra using an evaporation residue detector
- Author
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Burrows, J. D.
- Subjects
539.7 ,Study of nuclei - Published
- 1984
37. Chemical ozone loss in the Arctic vortex in the winter 1995–96: HALOE measurements in conjunction with other observations
- Author
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Müller, R., Grooß, J.-U., McKenna, D. S., Crutzen, P. J., Brühl, C., Russell, III, J. M., Gordley, L. L., Burrows, J. P., and Tuck, A. F.
- Published
- 1998
- Full Text
- View/download PDF
38. Satellite-derived methane hotspot emission estimates using a fast data-driven method
- Author
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Buchwitz, M., Schneising, O., Reuter, M., Heymann, J., Krautwurst, S., Bovensmann, H., Burrows, J. P., Boesch, H., Parker, R. J., Somkuti, P., Detmers, R. G., Hasekamp, O. P., Aben, I., Butz, A., Frankenberg, C., Turner, A. J., Earth and Climate, Atoms, Molecules, Lasers, and LaserLaB - Physics of Light
- Subjects
lcsh:Chemistry ,lcsh:QD1-999 ,ddc:000 ,SDG 13 - Climate Action ,Computer science, information & general works ,lcsh:Physics ,lcsh:QC1-999 - Abstract
Methane is an important atmospheric greenhouse gas and an adequate understanding of its emission sources is needed for climate change assessments, predictions, and the development and verification of emission mitigation strategies. Satellite retrievals of near-surface-sensitive column-averaged dry-air mole fractions of atmospheric methane, i.e. XCH4, can be used to quantify methane emissions. Maps of time-averaged satellite-derived XCH4 show regionally elevated methane over several methane source regions. In order to obtain methane emissions of these source regions we use a simple and fast data-driven method to estimate annual methane emissions and corresponding 1σ uncertainties directly from maps of annually averaged satellite XCH4. From theoretical considerations we expect that our method tends to underestimate emissions. When applying our method to high-resolution atmospheric methane simulations, we typically find agreement within the uncertainty range of our method (often 100 %) but also find that our method tends to underestimate emissions by typically about 40 %. To what extent these findings are model dependent needs to be assessed. We apply our method to an ensemble of satellite XCH4 data products consisting of two products from SCIAMACHY/ENVISAT and two products from TANSO-FTS/GOSAT covering the time period 2003–2014. We obtain annual emissions of four source areas: Four Corners in the south-western USA, the southern part of Central Valley, California, Azerbaijan, and Turkmenistan. We find that our estimated emissions are in good agreement with independently derived estimates for Four Corners and Azerbaijan. For the Central Valley and Turkmenistan our estimated annual emissions are higher compared to the EDGAR v4.2 anthropogenic emission inventory. For Turkmenistan we find on average about 50 % higher emissions with our annual emission uncertainty estimates overlapping with the EDGAR emissions. For the region around Bakersfield in the Central Valley we find a factor of 5–8 higher emissions compared to EDGAR, albeit with large uncertainty. Major methane emission sources in this region are oil/gas and livestock. Our findings corroborate recently published studies based on aircraft and satellite measurements and new bottom-up estimates reporting significantly underestimated methane emissions of oil/gas and/or livestock in this area in EDGAR.
- Published
- 2017
- Full Text
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39. DOAS Zenith Sky Observations: 1. BrO Measurements over Bremen (53°N) 1993–1994
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EISINGER, M., RICHTER, A., LADSTÄTTER-WEIßENMAYER, A., and BURROWS, J. P.
- Published
- 1997
- Full Text
- View/download PDF
40. Inequalities and healthcare reform in Chile: equity of what?
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Burrows, J
- Published
- 2008
- Full Text
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41. A Novel Taxon of RNA Viruses Endemic to Planarian Flatworms
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Burrows J, Bret J. Pearson, Max L. Nibert, and Delphine Depierreux
- Subjects
RNA silencing ,Schmidtea mediterranea ,Host (biology) ,RNA interference ,Evolutionary biology ,Planarian ,Cellular differentiation ,Biology ,biology.organism_classification ,Virus ,Adult stem cell - Abstract
The phylum Platyhelminthes is composed of both parasitic and non-parasitic flatworms. While the parasitic species have drawn attention for their wide effects on human and livestock heath, free-living flatworms, such as freshwater planarians, have become molecular models of regeneration and stem cell biology in the laboratory. However, one aspect of planarian biology that remains understudied is the relationship between host and any endemic viruses. Here we used searches of multiple transcriptomes from Schmidtea mediterranea asexual strain CIW4 and detected a novel, double-stranded RNA (dsRNA) virus, named S. mediterranea tricladivirus (SmedTV), which represents a distinct taxon (proposed new genus) within a larger taxon of monosegmented dsRNA viruses of diverse hosts. Experimental evidence for SmedTV in S. mediterranea CIW4 was obtained through whole-mount in situ hybridization (WISH). SmedTV “expression” (detected by both sense and anti-sense probes) was discrete yet variable from worm to worm and cell type to cell type, suggesting a persistent infection. Single-cell RNA sequencing (scRNAseq) further supported that SmedTV expression was low in stem cells, but substantially higher in multiple, though not all, differentiated tissues, with notable neural enrichment.Interestingly, knockdown of SmedTV by RNA-interference resulted in a “cure” of SmedTV after 10 RNAi doses, and expression remained undetectable by WISH even after 90 days. Due to being able to evade host defenses and the endogenous RNAi pathway, we believe SmedTV represents a novel animal model to study host-virus evolution.Statement of significancePlanarians are freshwater flatworms and emerging models to study the molecular mechanisms of adult stem cell and regenerative biology. However, they also live in aquatic environments with high amounts of viruses, bacteria, fungi, and protist pathogens. How the planarian immune system copes with all of these is largely unknown and only 2 types of virus have been described. Here we find a novel dsRNA virus, endemic to multiple types of flatworms. We show that it is a persistent infection, and likely transmits from stem cell to differentiated cell in the planarian, while avoiding endogenous RNA-interference machinery and mechanisms used to suppress viruses. We present this as a new model to study host-virus defense and evolution.
- Published
- 2019
- Full Text
- View/download PDF
42. Airborne in-situ observations of SO2 in Europe and Asia during the EMeRGe field campaigns
- Author
-
Eirenschmalz, Lisa, Schlager, Hans, Ly, Jenny, Huntrieser, Heidi, Baumann, Robert, Ziereis, Helmut, Stock, Paul, Lichtenstern, Michael, Stratmann, Greta, Klausner, Theresa, Fiehn, Alina, Sauer, Daniel, Heckl, Christopher, Burrows, J., and Hernandez, Maria D.
- Subjects
mega cities ,sulphur dioxide ,Atmosphärische Spurenstoffe ,pollution plumes - Published
- 2019
43. Aircraft Measurements of SO2 in Pollution Plumes of Major Population Centers in Europe and East-Asia during EMeRGe
- Author
-
Eirenschmalz, Lisa, Schlager, Hans, Ly, Jenny, Huntrieser, Heidi, Baumann, Robert, Ziereis, Helmut, Stock, Paul, Lichtenstern, Michael, Stratmann, Greta, Klausner, Theresa, Fiehn, Alina, Sauer, Daniel, Heckl, Christopher, Hernandez, Maria D., and Burrows, J.
- Subjects
sulphur dioxide ,megacities ,Atmosphärische Spurenstoffe ,pollution plumes - Published
- 2019
44. Gas phase spectra of HOBr and Br2O and their atmospheric significance
- Author
-
Deters, B., Burrows, J. P., Himmelmann, S., and Blindauer, C.
- Published
- 1996
- Full Text
- View/download PDF
45. Lyrical drama and the “turbid mountebanks”: Styles of dialogue in romantic and renaissance tragedy
- Author
-
Burrows, J. F. and Craig, D. H.
- Published
- 1994
- Full Text
- View/download PDF
46. Atmospheric Deposition of Reactive Nitrogen Derived from Global Model Simulations and from Satellite Observations
- Author
-
ESA Living Planet Symposium, Kanakidou, M, Daskalakis, N, Hilboll, A, Richter, Andreas, Myriokefalitakis, S, Sfakianaki, M, Vrekoussis, Mihalis, Burrows, J, Clarisse, Lieven, Van Damme, Martin, Coheur, Pierre, Clerbaux, Cathy, ESA Living Planet Symposium, Kanakidou, M, Daskalakis, N, Hilboll, A, Richter, Andreas, Myriokefalitakis, S, Sfakianaki, M, Vrekoussis, Mihalis, Burrows, J, Clarisse, Lieven, Van Damme, Martin, Coheur, Pierre, and Clerbaux, Cathy
- Abstract
info:eu-repo/semantics/published
- Published
- 2019
47. Tunable diode laser measurements of trace gases during the 1988 Polarstern cruise and intercomparisons with other methods
- Author
-
Harris, G. W., Klemp, D., Zenker, T., Burrows, J. P., and Mathieu, B.
- Published
- 1992
- Full Text
- View/download PDF
48. A study of the formation of N2O in the reaction of NO3(A2E′) with N2
- Author
-
Marić, D., Burrows, J. P., and Moortgat, G. K.
- Published
- 1992
- Full Text
- View/download PDF
49. Satellite-pointing retrieval from atmospheric limb-scattering of solar UV-B radiation
- Author
-
Kaiser, J W, Savigny, C von, Eichmann, K-U, Noël, S, Bovensmann, H, Frerick, J, and Burrows, J P
- Published
- 2004
50. DOAS Zenith Sky Observations: 2. Seasonal Variation of BrO Over Bremen (53°N) 1994–1995
- Author
-
Richter, A., Eisinger, M., Ladstätter-weienmayer, A., and Burrows, J. P.
- Published
- 1999
Catalog
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