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215 results on '"Horne, E. A."'

2. Particle transport induced by internal wave beam streaming in lateral boundary layers

Author

Horne, E., Beckebanze, F., Micard, D., Odier, P., Maas, L. R. M., and Joubaud, S.

Subjects
Physics - Fluid Dynamics
Abstract

Quantifying the physical mechanisms responsible for the transport of sediments, nutrients and pollutants in the abyssal sea is a long-standing problem, with internal waves regularly invoked as the relevant mechanism for particle advection near the sea bottom. This study focuses on internal-wave induced particle transport in the vicinity of (almost) vertical walls. We report a series of laboratory experiments revealing that particles sinking slowly through a monochromatic internal wave beam experience significant horizontal advection. Extending the theoretical analysis by Beckebanze et al (2018a), we attribute the observed particle advection to a peculiar and previously unrecognized streaming mechanism originating at the lateral walls. This vertical boundary-layer streaming mechanism is most efficient for strongly inclined wave beams, when vertical and horizontal velocity components are of comparable magnitude. We find good agreement between our theoretical prediction and experimental results., Comment: 19 pages, 8 figures

Published
2018
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3. X-ray/UV/optical variability of NGC 4593 with Swift: Reprocessing of X-rays by an extended reprocessor

Author

McHardy, I M, Connolly, S D, Cackett, K Horne E M, Gelbord, J, Peterson, B M, Pahari, M, Gehrels, N, Edelson, R, Goad, M, Lira, P, Arevalo, P, Baldi, R D, Brandt, N, Breedt, E, Chand, H, Dewangan, G, Done, C, Elvis, M, Emmanoulopoulos, D, Fausnaugh, M M, Kaspi, S, Kochanek, C S, Korista, K, Papadakis, I E, Rao, A R, Uttley, P, Vestergaard, M, and Ward, M J

Subjects
Astrophysics - High Energy Astrophysical Phenomena
Abstract

We report the results of intensive X-ray, UV and optical monitoring of the Seyfert 1 galaxy NGC 4593 with Swift. There is no intrinsic flux-related spectral change in the the variable components in any band with small apparent variations due only to contamination by a second constant component, possibly a (hard) reflection component in the X-rays and the (red) host galaxy in the UV/optical bands. Relative to the shortest wavelength band, UVW2, the lags of the other UV and optical bands are mostly in agreement with the predictions of reprocessing of high energy emission from an accretion disc. The U-band lag is, however, far larger than expected, almost certainly because of reprocessed Balmer continuum emission from the more distant broad line region gas. The UVW2 band is well correlated with the X-rays but lags by ~6x more than expected if the UVW2 results from reprocessing of X-rays on the accretion disc. However, if the lightcurves are filtered to remove variations on timescales >5d, the lag approaches the expectation from disc reprocessing. MEMEcho analysis shows that direct X-rays can be the driver of most of the variations in the UV/optical bands as long as the response functions for those bands all have long tails (up to 10d) in addition to a strong peak (from disc reprocessing) at short lag (<1d). We interpret the tails as due to reprocessing from the surrounding gas. Comparison of X-ray to UVW2 and UVW2 to V-band lags for 4 AGN, including NGC 4593, shows that all have UVW2 to V-band lags which exceed the expectations from disc resprocessing by factor < 2. However the X-ray to UVW2 lags are, mostly, in greater excess from the expectations from disc reprocessing and differ between AGN. The largest excess is in NGC 4151. Absorption and scattering may be affecting X-ray to UV lags., Comment: 18 pages, 17 figures. Submitted to Monthly Notices of the Royal Astronomical Society

Published
2017
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6. Sign cancellation and scaling in the vertical component of velocity and vorticity in rotating turbulence

Author

Horne, E. and Mininni, P. D.

Subjects
Physics - Fluid Dynamics
Abstract

We study sign changes and scaling laws in the Cartesian components of the velocity and vorticity of rotating turbulence, in the helicity, and in the components of vertically-averaged fields. Data for the analysis is provided by high-resolution direct numerical simulations of rotating turbulence with different forcing functions, with up to 1536^3 grid points, with Reynolds numbers between ~1100 and ~5100, and with moderate Rossby numbers between ~0.06 and ~8. When rotation is negligible, all Cartesian components of the velocity show similar scaling, in agreement with the expected isotropy of the flow. However, in the presence of rotation only the vertical components of the fields show clear scaling laws, with evidence of possible sign singularity in the limit of infinite Reynolds number. Horizontal components of the velocity are smooth and do not display rapid fluctuations for arbitrarily small scales. The vertical velocity and vorticity, as well as the vertically-averaged vertical velocity and vorticity, show the same scaling within error bars, in agreement with theories that predict that these quantities have the same dynamical equation for very strong rotation., Comment: 9 pages, 5 figures

Published
2013

7. Durability of ChAdOx1 nCoV-19 (AZD1222) vaccine and hybrid humoral immunity against variants including omicron BA.1 and BA.4 6 months after vaccination (COV005): a post-hoc analysis of a randomised, phase 1b–2a trial

Author

Madhi, SA, Kwatra, G, Richardson, SI, Koen, AL, Baillie, V, Cutland, CL, Fairlie, L, Padayachee, SD, Dheda, K, Barnabas, SL, Bhorat, QE, Briner, C, Ahmed, K, Aley, PK, Bhikha, S, Bhorat, AE, Esmail, A, Horne, E, Kaldine, H, Mukendi, CK, Madzorera, VS, Manamela, NP, Masilela, M, Hermanus, ST, Motlou, T, Mzindle, N, Oelofse, S, Patel, F, Rhead, S, Rossouw, L, Taoushanis, C, van Eck, S, Lambe, T, Gilbert, SC, Pollard, AJ, Moore, PL, and Izu, A

Subjects
Infectious Diseases
Abstract

Background COVID-19 vaccine rollout is lagging in Africa, where there has been a high rate of SARS-CoV-2 infection. We aimed to evaluate the effect of SARS-CoV-2 infection before vaccination with the ChAdOx-nCoV19 (AZD1222) vaccine on antibody responses through to 180 days. Methods We did an unmasked post-hoc immunogenicity analysis after the first and second doses of AZD1222 in a randomised, placebo-controlled, phase 1b–2a study done in seven locations in South Africa. AZD1222 recipients who were HIV-uninfected, were stratified into baseline seropositive or seronegative groups using the serum anti-nucleocapsid (anti-N) immunoglobulin G (IgG) electroluminescence immunoassay to establish SARS-CoV-2 infection before the first dose of AZD1222. Binding IgG to spike (anti-S) and receptor binding domain (anti-RBD) were measured before the first dose (day 0), second dose (day 28), day 42, and day 180. Neutralising antibody (NAb) against SARS-CoV-2 variants D614G, beta, delta, gamma, and A.VOI.V2, and omicron BA1 and BA.4 variants, were measured by pseudovirus assay (day 28, day 42, and day 180). This trial is registered with ClinicalTrials.gov, NCT04444674, and the Pan African Clinicals Trials Registry, PACTR202006922165132. Findings Of 185 individuals who were randomly assigned to AZD1222, we included 91 individuals who were baseline seropositive and 58 who were baseline seronegative, in the final analysis. In the seropositive group, there was little change of anti-S IgG (and anti-RBD IgG) or neutralising antibody (NAb) titres at day 42 compared with at day 28. Anti-S (and anti-RBD) IgG geometric mean concentrations (GMCs) were higher throughout in the seropositive compared with the seronegative group, including at day 180 (GMCs 517·8 [95% CI 411·3–651·9] vs 82·1 [55·2–122·3] BAU/mL). Also D614G NAb geometric mean titres (GMTs) were higher in the seropositive group than the seronegative group, as was the percentage with titres of at least 185 (80% putative risk reduction threshold [PRRT] against wild-type–alpha COVID-19), including at day 180 (92·0% [74·0–99·0] vs 18·2% [2·3–51·8). Similar findings were observed for beta, A.VOI.V2, and gamma. For delta, BA.1, and BA.4, NAb GMTs and the proportion with titres above the PRRT were substantially higher in the seropositive compared with seronegative group at day 28 and day 42, but no longer differed between the groups by day 180. Interpretation A single dose of AZD1222 in the general African population, where COVID-19 vaccine coverage is low and SARS-CoV-2 seropositivity is 90%, could enhance the magnitude and quality of antibody responses to SARS-CoV-2. Funding The Bill & Melinda Gates Foundation, the South African Medical Research Council, the UK Research and Innovation, the UK National Institute for Health Research, and the South African Medical Research Council. Translation For the Zulu translation of the abstract see Supplementary Materials section.

Published
2023

16. Particle transport induced by internal wave beam streaming in lateral boundary layers

Author

Horne, E., Beckebanze, F., Micard, D., Odier, P., Maas, L. R.M., Joubaud, S., Sub Mathematical Modeling, Sub Physical Oceanography, Mathematical Modeling, Sub Mathematical Modeling, Sub Physical Oceanography, Mathematical Modeling, Laboratoire d'hydrodynamique (LadHyX), École polytechnique (X)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Physique de l'ENS Lyon (Phys-ENS), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Centre National de la Recherche Scientifique (CNRS), Utrecht Mathematical Institute, Universiteit Utrecht, Laboratoire de Mecanique des Fluides et d'Acoustique (LMFA), École Centrale de Lyon (ECL), Université de Lyon-Université de Lyon-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Institut National des Sciences Appliquées de Lyon (INSA Lyon), Université de Lyon-Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-Centre National de la Recherche Scientifique (CNRS), Institute for Marine and Atmospheric Research [Utrecht] (IMAU), Utrecht University [Utrecht], Centre National de la Recherche Scientifique (CNRS)-École polytechnique (X), École normale supérieure - Lyon (ENS Lyon)-Centre National de la Recherche Scientifique (CNRS)-Université Claude Bernard Lyon 1 (UCBL), and Université de Lyon-Université de Lyon

Subjects
010504 meteorology & atmospheric sciences, Boundary (topology), Magnitude (mathematics), FOS: Physical sciences, 01 natural sciences, boundary layer structure, 010305 fluids & plasmas, sediment transport, Physics::Fluid Dynamics, 0103 physical sciences, Taverne, [PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph], ComputingMilieux_MISCELLANEOUS, 0105 earth and related environmental sciences, Advection, Mechanical Engineering, Fluid Dynamics (physics.flu-dyn), Mechanics, Physics - Fluid Dynamics, Internal wave, Condensed Matter Physics, Boundary layer, internal waves, Mechanics of Materials, Particle, Sediment transport, Geology, Beam (structure)
Abstract

Quantifying the physical mechanisms responsible for the transport of sediments, nutrients and pollutants in the abyssal sea is a long-standing problem, with internal waves regularly invoked as the relevant mechanism for particle advection near the sea bottom. This study focuses on internal-wave induced particle transport in the vicinity of (almost) vertical walls. We report a series of laboratory experiments revealing that particles sinking slowly through a monochromatic internal wave beam experience significant horizontal advection. Extending the theoretical analysis by Beckebanze et al (2018a), we attribute the observed particle advection to a peculiar and previously unrecognized streaming mechanism originating at the lateral walls. This vertical boundary-layer streaming mechanism is most efficient for strongly inclined wave beams, when vertical and horizontal velocity components are of comparable magnitude. We find good agreement between our theoretical prediction and experimental results., 19 pages, 8 figures

Published
2019

17. Body composition in anorexia nervosa: Meta-analysis and meta-regression of cross-sectional and longitudinal studies

Author

Breithaupt, L., Bulik, C.M., Hübel, C., Hunjan, A., O'Reilly, P.F., Breen, G., Yilmaz, Z., Schaumberg, K.E., Horne, E., and García-González, J.

Abstract

Objective: Clinically, anorexia nervosa (AN) presents with altered body composition. We quantified these alterations and evaluated their relationships with metabolites and hormones in patients with AN longitudinally. Method: In accordance with PRISMA guidelines, we conducted 94 meta-analyses on 62 samples published during 1996–2019, comparing up to 2,319 pretreatment, posttreatment, and weight-recovered female patients with AN with up to 1,879 controls. Primary outcomes were fat mass, fat-free mass, body fat percentage, and their regional distribution. Secondary outcomes were bone mineral density, metabolites, and hormones. Meta-regressions examined relationships among those measures and moderators. Results: Pretreatment female patients with AN evidenced 50% lower fat mass (mean difference [MD]: −8.80 kg, 95% CI: −9.81, −7.79, Q = 1.01 × 10−63) and 4.98 kg (95% CI: −5.85, −4.12, Q = 1.99 × 10−28) lower fat-free mass, with fat mass preferentially stored in the trunk region during early weight restoration (4.2%, 95% CI: −2.1, −6.2, Q = 2.30 × 10−4). While the majority of traits returned to levels seen in healthy controls after weight restoration, fat-free mass (MD: −1.27 kg, 95% CI: −1.79, −0.75, Q = 5.49 × 10−6) and bone mineral density (MD: −0.10 kg, 95% CI: −0.18, −0.03, Q = 0.01) remained significantly altered. Discussion: Body composition is markedly altered in AN, warranting research into these phenotypes as clinical risk or relapse predictors. Notably, the long-term altered levels of fat-free mass and bone mineral density suggest that these parameters should be investigated as potential AN trait markers.

Published
2019
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18. Particle transport induced by internal wave beam streaming in lateral boundary layers

Author

Sub Mathematical Modeling, Sub Physical Oceanography, Mathematical Modeling, Horne, E., Beckebanze, F., Micard, D., Odier, P., Maas, L. R.M., Joubaud, S., Sub Mathematical Modeling, Sub Physical Oceanography, Mathematical Modeling, Horne, E., Beckebanze, F., Micard, D., Odier, P., Maas, L. R.M., and Joubaud, S.

Published
2019

22. Spatio-temporal variability of the CO2 system on the Scotian Shelf

Author

Shadwick, E. H., Thomas, H., Prowe, A. E. F., and Horne, E.

Abstract

Relative to their surface areas, coastal oceans and continental shelves host a disproportionately large fraction of ocean productivity. The Scotian Shelf is a biologically productive coastal region of the Northwestern Atlantic Ocean. This subpolar region is influenced by the outflow of the St. Lawrence Estuary system and acts as an annual source for atmospheric CO2. As part of the Atlantic Zone Monitoring Program, dissolved inorganic carbon (DIC), total alkalinity, and surface CO2 partial pressure measurements were made throughout the Scotian Shelf in 2007. A shelf-wide assessment of the spatio-temporal variability of the inorganic carbon system was made relying on observations in April and September. Between these periods, biological production results in a significant drawdown of inorganic nutrients and DIC in the surface mixed-layer, while hydrographic controls also influence seasonal changes in DIC. Net community production (NCP) over the spring and summer seasons was estimated on the basis of inorganic carbon data. We find significant spatial variability in NCP with the largest values in the Southwestern Browns Bank region and a general trend of increasing NCP with distance offshore. A bulk seasonal carbon budget suggests that along-shore and cross-shelf transport may result in the export of subsurface DIC from this region.

Published
2018

24. X-ray/UV/optical variability of NGC 4593 with Swift:Reprocessing of X-rays by an extended reprocessor

Author

McHardy, I M, Connolly, S D, Cackett, K Horne E M, Gelbord, J, Peterson, B M, Pahari, M, Gehrels, N, Edelson, R, Goad, M, Lira, P, Arevalo, P, Baldi, R D, Breedt, E, Chand, H, Dewangan, G, Done, C, Elvis, M, Emmanoulopoulos, D, Fausnaugh, M M, Kaspi, S, Kochanek, C S, Korista, K, Papadakis, I E, Rao, A R, Uttley, P, Vestergaard, M, Ward, M J, McHardy, I M, Connolly, S D, Cackett, K Horne E M, Gelbord, J, Peterson, B M, Pahari, M, Gehrels, N, Edelson, R, Goad, M, Lira, P, Arevalo, P, Baldi, R D, Breedt, E, Chand, H, Dewangan, G, Done, C, Elvis, M, Emmanoulopoulos, D, Fausnaugh, M M, Kaspi, S, Kochanek, C S, Korista, K, Papadakis, I E, Rao, A R, Uttley, P, Vestergaard, M, and Ward, M J

Abstract

We report the results of intensive X-ray, UV and optical monitoring of the Seyfert 1 galaxy NGC 4593 with Swift. There is no intrinsic flux-related spectral change in the the variable components in any band with small apparent variations due only to contamination by a second constant component, possibly a (hard) reflection component in the X-rays and the (red) host galaxy in the UV/optical bands. Relative to the shortest wavelength band, UVW2, the lags of the other UV and optical bands are mostly in agreement with the predictions of reprocessing of high energy emission from an accretion disc. The U-band lag is, however, far larger than expected, almost certainly because of reprocessed Balmer continuum emission from the more distant broad line region gas. The UVW2 band is well correlated with the X-rays but lags by ~6x more than expected if the UVW2 results from reprocessing of X-rays on the accretion disc. However, if the lightcurves are filtered to remove variations on timescales >5d, the lag approaches the expectation from disc reprocessing. MEMEcho analysis shows that direct X-rays can be the driver of most of the variations in the UV/optical bands as long as the response functions for those bands all have long tails (up to 10d) in addition to a strong peak (from disc reprocessing) at short lag (

Published
2018

25. Expedition report CCGS Hudson 2011036: Bay of Fundy

Author

Todd, B J, primary, Bossey, S E, additional, Boutilier, R R, additional, Brown, A O, additional, Bryk, J L, additional, Bugden, G L, additional, Currie, C G, additional, Hayward, S E, additional, Horne, E P, additional, Jarrett, C A, additional, LeBlanc, K W G, additional, Li, M Z, additional, Manning, DJ, additional, Mesling, P, additional, Murphy, RJ, additional, Neelands, P J, additional, Potter, D P, additional, Robertson, A G, additional, Spencer, PL, additional, and Standen, G B, additional

Published
2012
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32. An enhanced linear model edge detector

Author

Assal, M. H. A., Horne, E., Fairhurst, M. C., Goos, G., editor, Hartmanis, J., editor, Barstow, D., editor, Brauer, W., editor, Brinch Hansen, P., editor, Gries, D., editor, Luckham, D., editor, Moler, C., editor, Pnueli, A., editor, Seegmüller, G., editor, Stoer, J., editor, Wirth, N., editor, and Kittler, J., editor

Published
1988
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33. About moment normalization and complex moment descriptors

Author

Abo-Zaid, A., Hinton, O. R., Horne, E., Goos, G., editor, Hartmanis, J., editor, Barstow, D., editor, Brauer, W., editor, Brinch Hansen, P., editor, Gries, D., editor, Luckham, D., editor, Moler, C., editor, Pnueli, A., editor, Seegmüller, G., editor, Stoer, J., editor, Wirth, N., editor, and Kittler, J., editor

Published
1988
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36. Maritime aerosol network as a component of AERONET - first results and comparison with global aerosol models and satellite retrievals

Author

Smirnov, Alexander, Holben, B. N., Giles, D. M., Slutsker, I., O'Neill, N. T., Eck, T. F., Macke, A., Croot, P., Courcoux, Y., Sakerin, S. M., Smyth, T. J., Zielinski, T., Zibordi, G., Goes, J. I., Harvey, M. J., Quinn, P. K., Nelson, N. B., Radionov, V. F., Duarte, C. M., Losno, R., Sciare, J., Voss, K. J., Kinne, S., Nalli, N. R., Joseph, E., Moorthy, K. Krishna, Covert, D. S., Gulev, S. K., Milinevsky, G., Larouche, P., Belanger, S., Horne, E., Chin, M., Remer, L. A., Kahn, R. A., Reid, J. S., Schulz, M., Heald, C. L., Zhang, J., Lapina, K., Kleidman, R. G., Griesfeller, J., Gaitley, B. J., Tan, Q., Diehl, T. L., Smirnov, Alexander, Holben, B. N., Giles, D. M., Slutsker, I., O'Neill, N. T., Eck, T. F., Macke, A., Croot, P., Courcoux, Y., Sakerin, S. M., Smyth, T. J., Zielinski, T., Zibordi, G., Goes, J. I., Harvey, M. J., Quinn, P. K., Nelson, N. B., Radionov, V. F., Duarte, C. M., Losno, R., Sciare, J., Voss, K. J., Kinne, S., Nalli, N. R., Joseph, E., Moorthy, K. Krishna, Covert, D. S., Gulev, S. K., Milinevsky, G., Larouche, P., Belanger, S., Horne, E., Chin, M., Remer, L. A., Kahn, R. A., Reid, J. S., Schulz, M., Heald, C. L., Zhang, J., Lapina, K., Kleidman, R. G., Griesfeller, J., Gaitley, B. J., Tan, Q., and Diehl, T. L.

Abstract

The Maritime Aerosol Network (MAN) has been collecting data over the oceans since November 2006. Over 80 cruises were completed through early 2010 with deployments continuing. Measurement areas included various parts of the Atlantic Ocean, the Northern and Southern Pacific Ocean, the South Indian Ocean, the Southern Ocean, the Arctic Ocean and inland seas. MAN deploys Microtops hand-held sunphotometers and utilizes a calibration procedure and data processing traceable to AERONET. Data collection included areas that previously had no aerosol optical depth (AOD) coverage at all, particularly vast areas of the Southern Ocean. The MAN data archive provides a valuable resource for aerosol studies in maritime environments. In the current paper we present results of AOD measurements over the oceans, and make a comparison with satellite AOD retrievals and model simulations.

Published
2011
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37. EXPERIMENTAL THERAPEUTICS AND PHARMACOLOGY

Author

Aaberg-Jessen, C., primary, Fogh, L., additional, Halle, B., additional, Jensen, V., additional, Brunner, N., additional, Kristensen, B. W., additional, Abe, T., additional, Momii, Y., additional, Watanabe, J., additional, Morisaki, I., additional, Natsume, A., additional, Wakabayashi, T., additional, Fujiki, M., additional, Aldaz, B., additional, Fabius, A. W. M., additional, Silber, J., additional, Harinath, G., additional, Chan, T. A., additional, Huse, J. T., additional, Anai, S., additional, Hide, T., additional, Nakamura, H., additional, Makino, K., additional, Yano, S., additional, Kuratsu, J.-i., additional, Balyasnikova, I. V., additional, Prasol, M. S., additional, Kanoija, D. K., additional, Aboody, K. S., additional, Lesniak, M. S., additional, Barone, T., additional, Burkhart, C., additional, Purmal, A., additional, Gudkov, A., additional, Gurova, K., additional, Plunkett, R., additional, Barton, K., additional, Misuraca, K., additional, Cordero, F., additional, Dobrikova, E., additional, Min, H., additional, Gromeier, M., additional, Kirsch, D., additional, Becher, O., additional, Pont, L. B., additional, Kloezeman, J., additional, van den Bent, M., additional, Kanaar, R., additional, Kremer, A., additional, Swagemakers, S., additional, French, P., additional, Dirven, C., additional, Lamfers, M., additional, Leenstra, S., additional, Balvers, R., additional, Kleijn, A., additional, Lawler, S., additional, Gong, X., additional, Andres, A., additional, Hanson, J., additional, Delashaw, J., additional, Bota, D., additional, Chen, C.-C., additional, Yao, N.-W., additional, Chuang, W.-J., additional, Chang, C., additional, Chen, P.-Y., additional, Huang, C.-Y., additional, Wei, K.-C., additional, Cheng, Y., additional, Dai, Q., additional, Morshed, R., additional, Han, Y., additional, Auffinger, B., additional, Wainwright, D., additional, Zhang, L., additional, Tobias, A., additional, Rincon, E., additional, Thaci, B., additional, Ahmed, A., additional, He, C., additional, Lesniak, M., additional, Choi, Y. A., additional, Pandya, H., additional, Gibo, D. M., additional, Fokt, I., additional, Priebe, W., additional, Debinski, W., additional, Chornenkyy, Y., additional, Agnihotri, S., additional, Buczkowicz, P., additional, Rakopoulos, P., additional, Morrison, A., additional, Barszczyk, M., additional, Hawkins, C., additional, Chung, S., additional, Decollogne, S., additional, Luk, P., additional, Shen, H., additional, Ha, W., additional, Day, B., additional, Stringer, B., additional, Hogg, P., additional, Dilda, P., additional, McDonald, K., additional, Moore, S., additional, Hayden-Gephart, M., additional, Bergen, J., additional, Su, Y., additional, Rayburn, H., additional, Edwards, M., additional, Scott, M., additional, Cochran, J., additional, Das, A., additional, Varma, A. K., additional, Wallace, G. C., additional, Dixon-Mah, Y. N., additional, Vandergrift, W. A., additional, Giglio, P., additional, Ray, S. K., additional, Patel, S. J., additional, Banik, N. L., additional, Dasgupta, T., additional, Olow, A., additional, Yang, X., additional, Mueller, S., additional, Prados, M., additional, James, C. D., additional, Haas-Kogan, D., additional, Dave, N. D., additional, Desai, P. B., additional, Gudelsky, G. A., additional, Chow, L. M. L., additional, LaSance, K., additional, Qi, X., additional, Driscoll, J., additional, Ebsworth, K., additional, Walters, M. J., additional, Ertl, L. S., additional, Wang, Y., additional, Berahovic, R. D., additional, McMahon, J., additional, Powers, J. P., additional, Jaen, J. C., additional, Schall, T. J., additional, Eroglu, Z., additional, Portnow, J., additional, Sacramento, A., additional, Garcia, E., additional, Raubitschek, A., additional, Synold, T., additional, Esaki, S., additional, Rabkin, S., additional, Martuza, R., additional, Wakimoto, H., additional, Ferluga, S., additional, Tome, C. L., additional, Forde, H. E., additional, Netland, I. A., additional, Sleire, L., additional, Skeie, B., additional, Enger, P. O., additional, Goplen, D., additional, Giladi, M., additional, Tichon, A., additional, Schneiderman, R., additional, Porat, Y., additional, Munster, M., additional, Dishon, M., additional, Weinberg, U., additional, Kirson, E., additional, Wasserman, Y., additional, Palti, Y., additional, Gramatzki, D., additional, Staudinger, M., additional, Frei, K., additional, Peipp, M., additional, Weller, M., additional, Grasso, C., additional, Liu, L., additional, Berlow, N., additional, Davis, L., additional, Fouladi, M., additional, Gajjar, A., additional, Huang, E., additional, Hulleman, E., additional, Hutt, M., additional, Keller, C., additional, Li, X.-N., additional, Meltzer, P., additional, Quezado, M., additional, Quist, M., additional, Raabe, E., additional, Spellman, P., additional, Truffaux, N., additional, van Vurden, D., additional, Wang, N., additional, Warren, K., additional, Pal, R., additional, Grill, J., additional, Monje, M., additional, Green, A. L., additional, Ramkissoon, S., additional, McCauley, D., additional, Jones, K., additional, Perry, J. A., additional, Ramkissoon, L., additional, Maire, C., additional, Shacham, S., additional, Ligon, K. L., additional, Kung, A. L., additional, Zielinska-Chomej, K., additional, Grozman, V., additional, Tu, J., additional, Viktorsson, K., additional, Lewensohn, R., additional, Gupta, S., additional, Mladek, A., additional, Bakken, K., additional, Carlson, B., additional, Boakye-Agyeman, F., additional, Kizilbash, S., additional, Schroeder, M., additional, Reid, J., additional, Sarkaria, J., additional, Hadaczek, P., additional, Ozawa, T., additional, Soroceanu, L., additional, Yoshida, Y., additional, Matlaf, L., additional, Singer, E., additional, Fiallos, E., additional, Cobbs, C. S., additional, Hashizume, R., additional, Tom, M., additional, Ihara, Y., additional, Santos, R., additional, Torre, J. D. L., additional, Lepe, E., additional, Waldman, T., additional, James, D., additional, Huang, X., additional, Yu-Jen, L., additional, Gupta, N., additional, Solomon, D., additional, Zhang, Z., additional, Hayashi, T., additional, Adachi, K., additional, Nagahisa, S., additional, Hasegawa, M., additional, Hirose, Y., additional, Gephart, M. H., additional, Su, Y. S., additional, Hingtgen, S., additional, Kasmieh, R., additional, Nesterenko, I., additional, Figueiredo, J.-L., additional, Dash, R., additional, Sarkar, D., additional, Fisher, P., additional, Shah, K., additional, Horne, E., additional, Diaz, P., additional, Stella, N., additional, Huang, C., additional, Yang, H., additional, Wei, K., additional, Huang, T., additional, Hlavaty, J., additional, Ostertag, D., additional, Espinoza, F. 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E., additional, Liu, Q., additional, Turner, G., additional, Preul, M. C., additional, Scheck, A. C., additional, Shen, W., additional, Brown, D., additional, Pedersen, H., additional, Hariono, S., additional, Yao, T.-W., additional, Sidhu, A., additional, Weiss, W. A., additional, Nicolaides, T. P., additional, and Olusanya, T., additional

Published
2013
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46. Maritime aerosol network as a component of AERONET – first results and comparison with global aerosol models and satellite retrievals

Author

Smirnov, A., primary, Holben, B. N., additional, Giles, D. M., additional, Slutsker, I., additional, O'Neill, N. T., additional, Eck, T. F., additional, Macke, A., additional, Croot, P., additional, Courcoux, Y., additional, Sakerin, S. M., additional, Smyth, T. J., additional, Zielinski, T., additional, Zibordi, G., additional, Goes, J. I., additional, Harvey, M. J., additional, Quinn, P. K., additional, Nelson, N. B., additional, Radionov, V. F., additional, Duarte, C. M., additional, Losno, R., additional, Sciare, J., additional, Voss, K. J., additional, Kinne, S., additional, Nalli, N. R., additional, Joseph, E., additional, Krishna Moorthy, K., additional, Covert, D. S., additional, Gulev, S. K., additional, Milinevsky, G., additional, Larouche, P., additional, Belanger, S., additional, Horne, E., additional, Chin, M., additional, Remer, L. A., additional, Kahn, R. A., additional, Reid, J. S., additional, Schulz, M., additional, Heald, C. L., additional, Zhang, J., additional, Lapina, K., additional, Kleidman, R. G., additional, Griesfeller, J., additional, Gaitley, B. J., additional, Tan, Q., additional, and Diehl, T. L., additional

Published
2011
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