Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Tracey A. Rissman"'
Autor:
Matthew M. Coggon, Richard C. Flagan, Natasha Hodas, Z. Wang, S. P. Hersey, Roy K. Woods, Hossein Dadashazar, Varuntida Varutbangkul, Lindsay C. Maudlin, Arnaldo Negron Marty, John H. Seinfeld, Patrick Y. Chuang, J. S. Craven, Taylor Shingler, Ewan Crosbie, Tracey A. Rissman, Alexander B. MacDonald, Kelvin H. Bates, Gouri Prabhakar, Haflidi Jonsson, Shane M. Murphy, Jack J. Lin, Athanasios Nenes, Andrew R. Metcalf, Luz T. Padró, Armin Sorooshian
Publikováno v:
Scientific Data
The article of record as published may be found at https://www.nature.com/articles/sdata201826 Airborne measurements of meteorological, aerosol, and stratocumulus cloud properties have been harmonized from six field campaigns during July-August month
Autor:
Timothy M. VanReken, Andrew J. Heymsfield, Haflidi Jonsson, Aaron Bansemer, Vaughan T. J. Phillips, John H. Seinfeld, Steven C. Sherwood, Constantin Andronache, Richard C. Flagan, James C. Wilson, Tracey A. Rissman, Paul J. DeMott, Micheal Poellot, Varuntida Varutbangkul, William C. Conant
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 131:2019-2046
SUMMARY Simulations of a cumulonimbus cloud observed in the Cirrus Regional Study of Tropical Anvils and Cirrus Layers–Florida Area Cirrus Experiment (CRYSTAL-FACE) with an advanced version of the Explicit Microphysics Model (EMM) are presented. Th
Publikováno v:
Aerosol Science and Technology. 39:485-491
A three-dimensional model has been developed within the framework of the commercial computational fluid dynamics program, FLUENT®, to investigate the collection efficiency of an airborne counterflow virtual impactor (CVI). The model assumes steady-s
Publikováno v:
Journal of the Atmospheric Sciences. 61:919-930
Cloud droplet number concentrations are controlled by both meteorological and microphysical factors. Microphysical factors include aerosol number concentration and composition. This paper examines the importance of microphysical phenomena compared to
Autor:
Sara Lance, Athanasios Nenes, Armin Sorooshian, Manvendra K. Dubey, Haflidi Jonsson, Richard C. Flagan, Graham Feingold, Claudio Mazzoleni, John H. Seinfeld, Varuntida Varutbangkul, Harmony Gates, Tracey A. Rissman, Shane M. Murphy
Publikováno v:
Journal of Geophysical Research. 114
The article of record as published may be located at http://dx.doi.org/10.1029/2008JD011699. In situ cloud condensation nuclei (CCN) measurements were obtained in the boundary layer over Houston, Texas, during the 2006 Gulf of Mexico Atmospheric Comp
Autor:
Richard C. Flagan, Gordon McFiggans, Jason D. Surratt, Varuntida Varutbangkul, John H. Seinfeld, Tracey A. Rissman, David Topping
Publikováno v:
Atmospheric Chemistry and Physics, Vol 7, Iss 11, Pp 2949-2971 (2007)
Scopus-Elsevier
Rissman, T A, Varutbangkul, V, Surratt, J D, Topping, D O, McFiggans, G, Flagan, R C & Seinfeld, J H 2007, ' Cloud condensation nucleus (CCN) behavior of organic aerosol particles generated by atomization of water and methanol solutions ', Atmospheric Chemistry and Physics, vol. 7, no. 11, pp. 2949-2971 . https://doi.org/10.5194/acp-7-2949-2007
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2007, 7 (11), pp.2949-2971
Scopus-Elsevier
Rissman, T A, Varutbangkul, V, Surratt, J D, Topping, D O, McFiggans, G, Flagan, R C & Seinfeld, J H 2007, ' Cloud condensation nucleus (CCN) behavior of organic aerosol particles generated by atomization of water and methanol solutions ', Atmospheric Chemistry and Physics, vol. 7, no. 11, pp. 2949-2971 . https://doi.org/10.5194/acp-7-2949-2007
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2007, 7 (11), pp.2949-2971
Cloud condensation nucleus (CCN) experiments were carried out for malonic acid, succinic acid, oxalacetic acid, DL-malic acid, glutaric acid, DL-glutamic acid monohydrate, and adipic acid, using both water and methanol as atomization solvents, at thr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b69c3dfcfe524f68af08efc3a9dcab67
https://resolver.caltech.edu/CaltechAUTHORS:RISacpd06
https://resolver.caltech.edu/CaltechAUTHORS:RISacpd06
Autor:
James G. Hudson, Richard Ferrare, Tracey A. Rissman, David D. Turner, Haflidi Jonsson, Timothy M. VanReken, Jian Wang, Connor Flynn, R. Elleman, Steven J. Ghan, John H. Seinfeld, Richard C. Flagan, John A. Ogren
The article of record as published may be located at http://dx.doi.org/10.1029/2004JD005752 If the aerosol composition and size distribution below cloud are uniform, the vertical profile of cloud condensation nuclei concentration can be retrieved ent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bcb3ab29c5fee7deb18c793c9b3e1d3c
https://resolver.caltech.edu/CaltechAUTHORS:20150818-165532823
https://resolver.caltech.edu/CaltechAUTHORS:20150818-165532823
Autor:
Jian Wang, Tracey A. Rissman, Richard C. Flagan, John H. Seinfeld, Fred J. Brechtel, Roberto Gasparini, Timothy M. VanReken, Don R. Collins, Haflidi Jonsson
Publikováno v:
Journal of Geophysical Research. 111
Measurements were made by a new cloud condensation nuclei (CCN) instrument (CCNC3) during the Atmospheric Radiation Measurement (ARM) Program's Aerosol Intensive Observational Period (IOP) in May 2003 in Lamont, Oklahoma. An inverse aerosol/CCN closu
Publikováno v:
Journal of Geophysical Research: Atmospheres. 109
[1] Most aerosol-cloud-climate assessment studies use empirical aerosol number/droplet number relationships, which are subject to large variability. Historically, this variability has been attributed to unresolved variations in updraft velocity. We r
Autor:
Gregory Roberts, Haflidi Jonsson, Richard C. Flagan, Varuntida Varutbangkul, Jose L. Jimenez, A. E. Delia, Roya Bahreini, Athanasios Nenes, William C. Conant, Timothy M. VanReken, John H. Seinfeld, Tracey A. Rissman
Publikováno v:
Journal of Geophysical Research: Atmospheres. 109
Our understanding of the activation of aerosol particles into cloud drops during the formation of warm cumulus clouds presently has a limited observational foundation. Detailed observations of aerosol size and composition, cloud microphysics and dyna