Zobrazeno 1 - 10
of 220
pro vyhledávání: '"R Lonsdale"'
Autor:
C. R. Lonsdale, K. Sun
Publikováno v:
Atmospheric Chemistry and Physics, Vol 23, Pp 8727-8748 (2023)
Nitrogen oxides (NOx=NO+NO2) emissions are estimated in three regions in the Northern Hemisphere, generally located in North America, Europe, and East Asia, by calculating the directional derivatives of NO2 column amounts observed by the TROPOspheric
Externí odkaz:
https://doaj.org/article/81b18a6a72d84ffe98884e21d2359f3e
Autor:
A. L. Hodshire, E. Ramnarine, A. Akherati, M. L. Alvarado, D. K. Farmer, S. H. Jathar, S. M. Kreidenweis, C. R. Lonsdale, T. B. Onasch, S. R. Springston, J. Wang, Y. Wang, L. I. Kleinman, A. J. Sedlacek III, J. R. Pierce
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 6839-6855 (2021)
Biomass burning emits vapors and aerosols into the atmosphere that can rapidly evolve as smoke plumes travel downwind and dilute, affecting climate- and health-relevant properties of the smoke. To date, theory has been unable to explain observed vari
Externí odkaz:
https://doaj.org/article/a891b962e9494b0db5b70985485b0157
Publikováno v:
Geoscientific Model Development, Vol 13, Pp 4579-4593 (2020)
Biomass burning is a major source of trace gases and aerosols that can ultimately impact health, air quality, and climate. Global and regional-scale three-dimensional Eulerian chemical transport models (CTMs) use estimates of the primary emissions fr
Externí odkaz:
https://doaj.org/article/faeb0d7d2e2e43919e2b552e30910510
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 6561-6577 (2019)
Biomass burning is a significant global source of aerosol number and mass. In fresh biomass burning plumes, aerosol coagulation reduces aerosol number and increases the median size of aerosol size distributions, impacting aerosol radiative effects. N
Externí odkaz:
https://doaj.org/article/31397c9bf8da4942a5eb7487317ede4f
Autor:
C. R. Lonsdale, J. D. Hegarty, K. E. Cady-Pereira, M. J. Alvarado, D. K. Henze, M. D. Turner, S. L. Capps, J. B. Nowak, J. A. Neuman, A. M. Middlebrook, R. Bahreini, J. G. Murphy, M. Z. Markovic, T. C. VandenBoer, L. M. Russell, A. J. Scarino
Publikováno v:
Atmospheric Chemistry and Physics, Vol 17, Iss 4, Pp 2721-2739 (2017)
NH3 retrievals from the NASA Tropospheric Emission Spectrometer (TES), as well as surface and aircraft observations of NH3(g) and submicron NH4(p), are used to evaluate modeled concentrations of NH3(g) and NH4(p) from the Community Multiscale Air Qua
Externí odkaz:
https://doaj.org/article/21b44ca15f0f4e079aaef016be3372f3
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Autor:
M. J. Alvarado, C. R. Lonsdale, H. L. Macintyre, H. Bian, M. Chin, D. A. Ridley, C. L. Heald, K. L. Thornhill, B. E. Anderson, M. J. Cubison, J. L. Jimenez, Y. Kondo, L. K. Sahu, J. E. Dibb, C. Wang
Publikováno v:
Atmospheric Chemistry and Physics, Vol 16, Pp 9435-9455 (2016)
Accurate modeling of the scattering and absorption of ultraviolet and visible radiation by aerosols is essential for accurate simulations of atmospheric chemistry and climate. Closure studies using in situ measurements of aerosol scattering and ab
Externí odkaz:
https://doaj.org/article/32fbee8e1af64e31bfa4d4c4e573bbd5
Autor:
Chantelle R. Lonsdale, Kang Sun
Nitrogen oxides (NOx = NO + NO2) emissions are estimated in three regions in the Northern hemisphere, generally located in North America, Europe, and East Asia, by calculating the directional derivatives of NO2 column amounts observed by the TROPOMI
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ddfc4a4a72f88d33f4d49c36d8660a5
https://doi.org/10.5194/egusphere-2023-346
https://doi.org/10.5194/egusphere-2023-346
Autor:
M. J. Alvarado, C. R. Lonsdale, R. J. Yokelson, S. K. Akagi, H. Coe, J. S. Craven, E. V. Fischer, G. R. McMeeking, J. H. Seinfeld, T. Soni, J. W. Taylor, D. R. Weise, C. E. Wold
Publikováno v:
Atmospheric Chemistry and Physics, Vol 15, Iss 12, Pp 6667-6688 (2015)
Within minutes after emission, complex photochemistry in biomass burning smoke plumes can cause large changes in the concentrations of ozone (O3) and organic aerosol (OA). Being able to understand and simulate this rapid chemical evolution under a wi
Externí odkaz:
https://doaj.org/article/35b83a87fb7a4899b0202db3f071704d
Autor:
Anna L. Hodshire, C. R. Lonsdale, Yang Wang, Sonia M. Kreidenweis, Jian Wang, Delphine K. Farmer, Lawrence I. Kleinman, Shantanu H. Jathar, Matthew L. Alvarado, Timothy B. Onasch, Arthur J. Sedlacek, Stephen R. Springston, Ali Akherati, Emily Ramnarine, Jeffrey R. Pierce
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 6839-6855 (2021)
Biomass burning emits vapors and aerosols into the atmosphere that can rapidly evolve as smoke plumes travel downwind and dilute, affecting climate- and health-relevant properties of the smoke. To date, theory has been unable to explain observed vari