9129767 PWEZQ2Q2 1 apa 50 date desc year Roberts 18 https://gcroberts.scrippsprofiles.ucsd.edu/wp-content/plugins/zotpress/
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Lemonsu, A., Alessandrini, J. M., Capo, J., Claeys, M., Cordeau, E., De Munck, C., Dahech, S., Dupont, J. C., Dugay, F., Dupuis, V., Forceville, G., Garrigou, S., Garrouste, O., Goret, M., Goria, S., Haeffelin, M., Host, S., Joly, C., Keravec, P., … Wurtz, J. (2024). The heat and health in cities (H2C) project to support the prevention of extreme heat in cities. Climate Services, 34, 100472. https://doi.org/10.1016/j.cliser.2024.100472
D’Alessandro, J. J., McFarquhar, G. M., Stith, J. L., Diao, M., DeMott, P. J., McCluskey, C. S., Hill, T. C. J., Roberts, G. C., & Sanchez, K. J. (2023). An Evaluation of Phase, Aerosol‐Cloud Interactions and Microphysical Properties of Single‐ and Multi‐Layer Clouds Over the Southern Ocean Using in Situ Observations From SOCRATES. Journal of Geophysical Research: Atmospheres, 128(15), e2023JD038610. https://doi.org/10.1029/2023JD038610
Sanchez, K. J., Painemal, D., Brown, M. D., Crosbie, E. C., Gallo, F., Hair, J. W., Hostetler, C. A., Jordan, C. E., Robinson, C. E., Scarino, A. J., Shingler, T. J., Shook, M. A., Thornhill, K. L., Wiggins, E. B., Winstead, E. L., Ziemba, L. D., Chambers, S., Williams, A., Humphries, R. S., … Moore, R. H. (2023). Multi-campaign ship and aircraft observations of marine cloud condensation nuclei and droplet concentrations. Scientific Data, 10(1), 471. https://doi.org/10.1038/s41597-023-02372-z
Maury, N., Roberts, G. C., Couvreux, F., Verdu, T., Narvor, P., Lacroix, S., & Hattenberger, G. (2023). Quantifying the mixing of trade‐wind cumulus during the NEPHELAE‐EUREC4A field campaign with remotely piloted aircraft. Quarterly Journal of the Royal Meteorological Society, qj.4430. https://doi.org/10.1002/qj.4430
Zhao, X., Liu, X., Burrows, S., DeMott, P. J., Diao, M., McFarquhar, G. M., Patade, S., Phillips, V., Roberts, G. C., Sanchez, K. J., Shi, Y., & Zhang, M. (2023). Important Ice Processes Are Missed by the Community Earth System Model in Southern Ocean Mixed‐Phase Clouds: Bridging SOCRATES Observations to Model Developments. Journal of Geophysical Research: Atmospheres, 128(4). https://doi.org/10.1029/2022JD037513
Cheng, Z., Morgenstern, M., Henning, S., Zhang, B., Roberts, G. C., Fraund, M., Marcus, M. A., Lata, N. N., Fialho, P., Mazzoleni, L., Wehner, B., Mazzoleni, C., & China, S. (2023). Cloud condensation nuclei activity of internally mixed particle populations at a remote marine free troposphere site in the North Atlantic Ocean. Science of The Total Environment, 904, 166865. https://doi.org/10.1016/j.scitotenv.2023.166865
Maury, N., Roberts, G. C., Couvreux, F., Verdu, T., Narvor, P., Villefranque, N., Lacroix, S., & Hattenberger, G. (2022). Use of large-eddy simulations to design an adaptive sampling strategy to assess cumulus cloud heterogeneities by remotely piloted aircraft. Atmospheric Measurement Techniques, 15(2), 335–352. https://doi.org/10.5194/amt-15-335-2022
Pinto, J. O., O’Sullivan, D., Taylor, S., Elston, J., Baker, C. B., Hotz, D., Marshall, C., Jacob, J., Barfuss, K., Piguet, B., Roberts, G., Omanovic, N., Fengler, M., Jensen, A. A., Steiner, M., & Houston, A. L. (2021). The status and future of small uncrewed aircraft systems (UAS) in operational meteorology. Bulletin of the American Meteorological Society, 102(11), E2121–E2136. https://doi.org/10.1175/bams-d-20-0138.1
Stevens, B., Bony, S., Farrell, D., Ament, F., Blyth, A., Fairall, C., Karstensen, J., Quinn, P. K., Speich, S., Acquistapace, C., Aemisegger, F., Albright, A. L., Bellenger, H., Bodenschatz, E., Caesar, K. A., Chewitt-Lucas, R., de Boer, G., Delanoe, J., Denby, L., … Zoger, M. (2021). EUREC(4)A. Earth System Science Data, 13(8), 4067–4119. https://doi.org/10.5194/essd-13-4067-2021
Barthe, C., Bousquet, O., Bielli, S., Tulet, P., Pianezze, J., Claeys, M., Tsai, C. L., Thompson, C., Bonnardot, F., Chauvin, F., Cattiaux, J., Bouin, M. N., Amelie, V., Barruol, G., Calmer, R., Ciccione, S., Cordier, E., Duong, Q. P., Durand, J., … Zucule, J. (2021). Impact of tropical cyclones on inhabited areas of the SWIO basin at present and future horizons. Part 2: Modeling component of the research program RENOVRISK-CYCLONE. Atmosphere, 12(6). https://doi.org/10.3390/atmos12060689
Bousquet, O., Barruol, G., Cordier, E., Barthe, C., Bielli, S., Calmer, R., Rindraharisaona, E., Roberts, G., Tulet, P., Amelie, V., Fleischer-Dogley, F., Mavume, A., Zucule, J., Zakariasy, L., Razafindradina, B., Bonnardot, F., Singh, M., Lees, E., Durand, J., … Marquestaut, N. (2021). Impact of tropical cyclones on inhabited areas of the SWIO Basin at present and future horizons. Part 1: Overview and observing component of the research project RENOVRISK-CYCLONE. Atmosphere, 12(5), 41. https://doi.org/10.3390/atmos12050544
McFarquhar, G. M., Bretherton, C. S., Marchand, R., Protat, A., DeMott, P. J., Alexander, S. P., Roberts, G. C., Twohy, C. H., Toohey, D., Siems, S., Huang, Y., Wood, R., Rauber, R. M., Lasher-Trapp, S., Jensen, J., Stith, J. L., Mace, J., Um, J., Jarvinen, E., … McDonald, A. (2021). Observations of clouds, aerosols, precipitation, and surface radiation over the Southern Ocean: An overview of CAPRICORN, MARCUS, MICRE, and SOCRATES. Bulletin of the American Meteorological Society, 102(4), E894–E928. https://doi.org/10.1175/bams-d-20-0132.1
Sanchez, K. J., Roberts, G. C., Saliba, G., Russell, L. M., Twohy, C., Reeves, M. J., Humphries, R. S., Keywood, M. D., Ward, J. P., & McRobert, I. M. (2021). Measurement report: Cloud processes and the transport of biological emissions affect southern ocean particle and cloud condensation nuclei concentrations. Atmospheric Chemistry and Physics, 21(5), 3427–3446. https://doi.org/10.5194/acp-21-3427-2021
Twohy, C. H., DeMott, P. J., Russell, L. M., Toohey, D. W., Rainwater, B., Geiss, R., Sanchez, K. J., Lewis, S., Roberts, G. C., Humphries, R. S., McCluskey, C. S., Moore, K. A., Selleck, P. W., Keywood, M. D., Ward, J. P., & McRobert, I. M. (2021). Cloud-nucleating particles over the Southern Ocean in a changing climate. Earths Future, 9(3). https://doi.org/10.1029/2020ef001673
Siebert, H., Szodry, K. E., Egerer, U., Wehner, B., Henning, S., Chevalier, K., Luckerath, J., Welz, O., Weinhold, K., Lauermann, F., Gottschalk, M., Ehrlich, A., Wendisch, M., Fialho, P., Roberts, G., Allwayin, N., Schum, S., Shaw, R. A., Mazzoleni, C., … Mellado, J. P. (2021). Observations of aerosol, cloud, turbulence, and radiation properties at the top of the marine boundary layer over the eastern North Atlantic Ocean: The ACORES campaign. Bulletin of the American Meteorological Society, 102(1), E123–E147. https://doi.org/10.1175/bams-d-19-0191.1
Saliba, G., Sanchez, K. J., Russell, L. M., Twohy, C. H., Roberts, G. C., Lewis, S., Dedrick, J., McCluskey, C. S., Moore, K., DeMott, P. J., & Toohey, D. W. (2020). Organic composition of three different size ranges of aerosol particles over the Southern Ocean. Aerosol Science and Technology. https://doi.org/10.1080/02786826.2020.1845296
Sanchez, K. J., Roberts, G. C., Diao, M., & Russell, L. M. (2020). Measured constraints on cloud top entrainment to reduce uncertainty of nonprecipitating stratocumulus shortwave radiative forcing in the Southern Ocean. Geophysical Research Letters, 47(21). https://doi.org/10.1029/2020gl090513
Mansour, K., Decesari, S., Facchini, M. C., Belosi, F., Paglione, M., Sandrini, S., Bellacicco, M., Marullo, S., Santoleri, R., Ovadnevaite, J., Ceburnis, D., O’Dowd, C., Roberts, G., Sanchez, K., & Rinaldi, M. (2020). Linking marine biological activity to aerosol chemical composition and cloud-relevant properties over the North Atlantic Ocean. Journal of Geophysical Research-Atmospheres, 125(13). https://doi.org/10.1029/2019jd032246
Calmer, R., Roberts, G. C., Sanchez, K. J., Sciare, J., Sellegri, K., Picard, D., Vrekoussis, M., & Pikridas, M. (2019). Aerosol-cloud closure study on cloud optical properties using remotely piloted aircraft measurements during a BACCHUS field campaign in Cyprus. Atmospheric Chemistry and Physics, 19(22), 13989–14007. https://doi.org/10.5194/acp-19-13989-2019
Calmer, R., Roberts, G. C., Preissler, J., Sanchez, K. J., Derrien, S., & O’Dowd, C. (2018). Vertical wind velocity measurements using a five-hole probe with remotely piloted aircraft to study aerosol-cloud interactions. Atmospheric Measurement Techniques, 11(5), 2583–2599. https://doi.org/10.5194/amt-11-2583-2018
Crispel, P., & Roberts, G. (2018). All-sky photogrammetry techniques to georeference a cloud field. Atmospheric Measurement Techniques, 11(1), 593–609. https://doi.org/10.5194/amt-11-593-2018
Sanchez, K. J., Roberts, G. C., Calmer, R., Nicoll, K., Hashimshoni, E., Rosenfeld, D., Ovadnevaite, J., Preissler, J., Ceburnis, D., O’Dowd, C., & Russell, L. M. (2017). Top-down and bottom-up aerosol-cloud closure: towards understanding sources of uncertainty in deriving cloud shortwave radiative flux. Atmospheric Chemistry and Physics, 17(16), 9797–9814. https://doi.org/10.5194/acp-17-9797-2017
Claeys, M., Roberts, G., Mallet, M., Arndt, J., Sellegri, K., Sciare, J., Wenger, J., & Sauvage, B. (2017). Optical, physical and chemical properties of aerosols transported to a coastal site in the western Mediterranean: a focus on primary marine aerosols. Atmospheric Chemistry and Physics, 17(12), 7891–7915. https://doi.org/10.5194/acp-17-7891-2017
Arndt, J., Sciare, J., Mallet, M., Roberts, G. C., Marchand, N., Sartelet, K., Sellegri, K., Dulac, F., Healy, R. M., & Wenger, J. C. (2017). Sources and mixing state of summertime background aerosol in the north-western Mediterranean basin. Atmospheric Chemistry and Physics, 17(11), 6975–7001. https://doi.org/10.5194/acp-17-6975-2017
Ovadnevaite, J., Zuend, A., Laaksonen, A., Sanchez, K. J., Roberts, G., Ceburnis, D., Decesari, S., Rinaldi, M., Hodas, N., Facchini, M. C., Seinfeld, J. H., & Dowd, C. O. (2017). Surface tension prevails over solute effect in organic-influenced cloud droplet activation. Nature, 546(7660), 637–641. https://doi.org/10.1038/nature22806
Wex, H., Dieckmann, K., Roberts, G. C., Conrath, T., Izaguirre, M. A., Hartmann, S., Herenz, P., Schafer, M., Ditas, F., Schmeissner, T., Henning, S., Wehner, B., Siebert, H., & Stratmann, F. (2016). Aerosol arriving on the Caribbean island of Barbados: physical properties and origin. Atmospheric Chemistry and Physics, 16(22), 14107–14130. https://doi.org/10.5194/acp-16-14107-2016
Sanchez, K. J., Russell, L. M., Modini, R. L., Frossard, A. A., Ahlm, L., Corrigan, C. E., Roberts, G. C., Hawkins, L. N., Schroder, J. C., Bertram, A. K., Zhao, R., Lee, A. K. Y., Lin, J. J., Nenes, A., Wang, Z., Wonaschutz, A., Sorooshian, A., Noone, K. J., Jonsson, H., … Seinfeld, J. H. (2016). Meteorological and aerosol effects on marine cloud microphysical properties. Journal of Geophysical Research-Atmospheres, 121(8), 4142–4161. https://doi.org/10.1002/2015jd024595
Modini, R. L., Frossard, A. A., Ahlm, L., Russell, L. M., Corrigan, C. E., Roberts, G. C., Hawkins, L. N., Schroder, J. C., Bertram, A. K., Zhao, R., Lee, A. K. Y., Abbatt, J. P. D., Lin, J., Nenes, A., Wang, Z., Wonaschutz, A., Sorooshian, A., Noone, K. J., Jonsson, H., … Leaitch, W. R. (2015). Primary marine aerosol-cloud interactions off the coast of California. Journal of Geophysical Research-Atmospheres, 120(9), 4282–4303. https://doi.org/10.1002/2014jd022963
Hammer, E., Gysel, M., Roberts, G. C., Elias, T., Hofer, J., Hoyle, C. R., Bukowiecki, N., Dupont, J. C., Burnet, F., Baltensperger, U., & Weingartner, E. (2014). Size-dependent particle activation properties in fog during the ParisFog 2012/13 field campaign. Atmospheric Chemistry and Physics, 14(19), 10517–10533. https://doi.org/10.5194/acp-14-10517-2014
Werner, F., Ditas, F., Siebert, H., Simmel, M., Wehner, B., Pilewskie, P., Schmeissner, T., Shaw, R. A., Hartmann, S., Wex, H., Roberts, G. C., & Wendisch, M. (2014). Twomey effect observed from collocated microphysical and remote sensing measurements over shallow cumulus. Journal of Geophysical Research-Atmospheres, 119(3), 1534–1545. https://doi.org/10.1002/2013jd020131
Siebert, H., Beals, M., Bethke, J., Bierwirth, E., Conrath, T., Dieckmann, K., Ditas, F., Ehrlich, A., Farrell, D., Hartmann, S., Izaguirre, M. A., Katzwinkel, J., Nuijens, L., Roberts, G., Schafer, M., Shaw, R. A., Schmeissner, T., Serikov, I., Stevens, B., … Wex, H. (2013). The fine-scale structure of the trade wind cumuli over Barbados - an introduction to the CARRIBA project. Atmospheric Chemistry and Physics, 13(19), 10061–10077. https://doi.org/10.5194/acp-13-10061-2013
Wonaschutz, A., Coggon, M., Sorooshian, A., Modini, R., Frossard, A. A., Ahlm, L., Mulmenstadt, J., Roberts, G. C., Russell, L. M., Dey, S., Brechtel, F. J., & Seinfeld, J. H. (2013). Hygroscopic properties of smoke-generated organic aerosol particles emitted in the marine atmosphere. Atmospheric Chemistry and Physics, 13(19), 9819–9835. https://doi.org/10.5194/acp-13-9819-2013
Collins, D. B., Ault, A. P., Moffet, R. C., Ruppel, M. J., Cuadra-Rodriguez, L. A., Guasco, T. L., Corrigan, C. E., Pedler, B. E., Azam, F., Aluwihare, L. I., Bertram, T. H., Roberts, G. C., Grassian, V. H., & Prather, K. A. (2013). Impact of marine biogeochemistry on the chemical mixing state and cloud forming ability of nascent sea spray aerosol. Journal of Geophysical Research-Atmospheres, 118(15), 8553–8565. https://doi.org/10.1002/jgrd.50598
Juranyi, Z., Tritscher, T., Gysel, M., Laborde, M., Gomes, L., Roberts, G., Baltensperger, U., & Weingartner, E. (2013). Hygroscopic mixing state of urban aerosol derived from size-resolved cloud condensation nuclei measurements during the MEGAPOLI campaign in Paris. Atmospheric Chemistry and Physics, 13(13), 6431–6446. https://doi.org/10.5194/acp-13-6431-2013
Russell, L. M., Sorooshian, A., Seinfeld, J. H., Albrecht, B. A., Nenes, A., Ahlm, L., Chen, Y. C., Coggon, M., Craven, J. S., Flagan, R. C., Frossard, A. A., Jonsson, H., Jung, E., Lin, J. J., Metcalf, A. R., Modini, R., Mulmenstadt, J., Roberts, G. C., Shingler, T., … Wonaschutz, A. (2013). Eastern Pacific emitted aerosol cloud experiment. Bulletin of the American Meteorological Society, 94(5), 709-+. https://doi.org/10.1175/bams-d-12-00015.1
DeMott, P. J., Hudson, J. G., Roberts, G. C., & Bundke, U. (2013). Cloud condensation and ice nuclei. In M. Wendisch, J. L. Brenguier, & A. Kohkhanovsky (Eds.), Airborne Measurements for Environmental Research (pp. 157–223). John Wiley & Sons.
Begue, N., Tulet, P., Chaboureau, J. P., Roberts, G., Gomes, L., & Mallet, M. (2012). Long-range transport of Saharan dust over northwestern Europe during EUCAARI 2008 campaign: Evolution of dust optical properties by scavenging. Journal of Geophysical Research-Atmospheres, 117. https://doi.org/10.1029/2012jd017611
Baumgardner, D., Avallone, L., Bansemer, A., Borrmann, S., Brown, P., Bundke, U., Chuang, P. Y., Cziczo, D., Field, P., Gallagher, M., Gayet, J. F., Heymsfield, A., Korolev, A., Kramer, M., McFarquhar, G., Mertes, S., Mohler, O., Lance, S., Lawson, P., … Wendisch, M. (2012). In situ, airborne instrumentation: addressing and solving measurement problems in ice clouds. Bulletin of the American Meteorological Society, 93(2), E529–E534. https://doi.org/10.1175/bams-d-11-00123.1
Russell, L. M., Sorooshian, A., Seinfeld, J. H., Albrecht, B. A., Nenes, A., Ahlm, L., Chen, Y.-C., Coggon, M., Craven, J. S., Flagan, R. C., Frossard, A. A., Jonsson, H., Jung, E., Lin, J. J., Metcalf, A. R., Modini, R., Mülmenstädt, J., Roberts, G. C., Shingler, T., … Wonaschütz, A. (2012). Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE). Bulletin of the American Meteorological Society. https://doi.org/10.1175/BAMS-D-12-00015
Moore, M. J. K., Furutani, H., Roberts, G. C., Moffet, R. C., Gilles, M. K., Palenik, B., & Prather, K. A. (2011). Effect of organic compounds on cloud condensation nuclei (CCN) activity of sea spray aerosol produced by bubble bursting. Atmospheric Environment, 45(39), 7462–7469. https://doi.org/10.1016/j.atmosenv.2011.04.034
Creamean, J. M., Ault, A. P., Ten Hoeve, J. E., Jacobson, M. Z., Roberts, G. C., & Prather, K. A. (2011). Measurements of aerosol chemistry during new particle formation events at a remote rural mountain site. Environmental Science & Technology, 45(19), 8208–8216. https://doi.org/10.1021/es103692f
Kulmala, M., Asmi, A., Lappalainen, H. K., Baltensperger, U., Brenguier, J. L., Facchini, M. C., Hansson, H. C., Hov, O., O’Dowd, C. D., Poschl, U., Wiedensohler, A., Boers, R., Boucher, O., de Leeuw, G., van der Gon, H., Feichter, J., Krejci, R., Laj, P., Lihavainen, H., … Pandis, S. N. (2011). General overview: European Integrated project on Aerosol Cloud Climate and Air Quality interactions (EUCAARI) - integrating aerosol research from nano to global scales. Atmospheric Chemistry and Physics, 11(24), 13061–13143. https://doi.org/10.5194/acp-11-13061-2011
Martin, S. T., Andreae, M. O., Artaxo, P., Baumgardner, D., Chen, Q., Goldstein, A. H., Guenther, A., Heald, C. L., Mayol-Bracero, O. L., McMurry, P. H., Pauliquevis, T., Poschl, U., Prather, K. A., Roberts, G. C., Saleska, S. R., Dias, M. A. S., Spracklen, D. V., Swietlicki, E., & Trebs, I. (2010). Sources and properties of Amazonian aerosol particles. Reviews of Geophysics, 48. https://doi.org/10.1029/2008rg000280
Crumeyrolle, S., Manninen, H. E., Sellegri, K., Roberts, G., Gomes, L., Kulmala, M., Weigel, R., Laj, P., & Schwarzenboeck, A. (2010). New particle formation events measured on board the ATR-42 aircraft during the EUCAARI campaign. Atmospheric Chemistry and Physics, 10(14), 6721–6735. https://doi.org/10.5194/acp-10-6721-2010
Kuhn, U., Ganzeveld, L., Thielmann, A., Dindorf, T., Schebeske, G., Welling, M., Sciare, J., Roberts, G., Meixner, F. X., Kesselmeier, J., Lelieveld, J., Kolle, O., Ciccioli, P., Lloyd, J., Trentmann, J., Artaxo, P., & Andreae, M. O. (2010). Impact of Manaus City on the Amazon Green Ocean atmosphere: ozone production, precursor sensitivity and aerosol load. Atmospheric Chemistry and Physics, 10(19), 9251–9282. https://doi.org/10.5194/acp-10-9251-2010
Roberts, G. C., Day, D. A., Russell, L. M., Dunlea, E. J., Jimenez, J. L., Tomlinson, J. M., Collins, D. R., Shinozuka, Y., & Clarke, A. D. (2010). Characterization of particle cloud droplet activity and composition in the free troposphere and the boundary layer during INTEX-B. Atmospheric Chemistry and Physics, 10(14), 6627–6644. https://doi.org/10.5194/acp-10-6627-2010
Sullivan, R. C., Moore, M. J. K., Petters, M. D., Kreidenweis, S. M., Qafoku, O., Laskin, A., Roberts, G. C., & Prather, K. A. (2010). Impact of particle generation method on the apparent hygroscopicity of insoluble mineral particles. Aerosol Science and Technology, 44(10), 830–846. https://doi.org/10.1080/02786826.2010.497514
Stith, J. L., Ramanathan, V., Cooper, W. A., Roberts, G. C., DeMott, P. J., Carmichael, G., Hatch, C. D., Adhikary, B., Twohy, C. H., Rogers, D. C., Baumgardner, D., Prenni, A. J., Campos, T., Gao, R., Anderson, J., & Feng, Y. (2009). An overview of aircraft observations from the Pacific Dust Experiment campaign. Journal of Geophysical Research-Atmospheres, 114. https://doi.org/10.1029/2008jd010924
Shinozuka, Y., Clarke, A. D., DeCarlo, P. F., Jimenez, J. L., Dunlea, E. J., Roberts, G. C., Tomlinson, J. M., Collins, D. R., Howell, S. G., Kapustin, V. N., McNaughton, C. S., & Zhou, J. (2009). Aerosol optical properties relevant to regional remote sensing of CCN activity and links to their organic mass fraction: airborne observations over Central Mexico and the US West Coast during MILAGRO/INTEX-B. Atmospheric Chemistry and Physics, 9(18), 6727–6742. https://doi.org/10.5194/acp-9-6727-2009
Sullivan, R. C., Moore, M. J. K., Petters, M. D., Kreidenweis, S. M., Roberts, G. C., & Prather, K. A. (2009). Effect of chemical mixing state on the hygroscopicity and cloud nucleation properties of calcium mineral dust particles. Atmospheric Chemistry and Physics, 9(10), 3303–3316. https://doi.org/10.5194/acp-9-3303-2009