Zobrazeno 1 - 10
of 3 282
pro vyhledávání: '"C. Dang"'
Autor:
D. Hao, G. Bisht, K. Rittger, E. Bair, C. He, H. Huang, C. Dang, T. Stillinger, Y. Gu, H. Wang, Y. Qian, L. R. Leung
Publikováno v:
Geoscientific Model Development, Vol 16, Pp 75-94 (2023)
With the highest albedo of the land surface, snow plays a vital role in Earth's surface energy budget and water cycle. Snow albedo is primarily controlled by snow grain properties (e.g., size and shape) and light-absorbing particles (LAPs) such as bl
Externí odkaz:
https://doaj.org/article/b9a157cf52a747aea47c00cd1c6cbb9a
Autor:
C. Dang, M. Segal-Rozenhaimer, H. Che, L. Zhang, P. Formenti, J. Taylor, A. Dobracki, S. Purdue, P.-S. Wong, A. Nenes, A. Sedlacek III, H. Coe, J. Redemann, P. Zuidema, S. Howell, J. Haywood
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 9389-9412 (2022)
This study characterizes single-particle aerosol composition from filters collected during the ObseRvations of Aerosols above CLouds and their intEractionS (ORACLES) and CLoud–Aerosol–Radiation Interaction and Forcing: Year 2017 (CLARIFY-2017) ca
Externí odkaz:
https://doaj.org/article/3e90d56bfb1941c08234b76942a8e875
Autor:
H. Che, M. Segal-Rozenhaimer, L. Zhang, C. Dang, P. Zuidema, A. J. Sedlacek III, X. Zhang, C. Flynn
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 8767-8785 (2022)
From June to October, southern Africa produces one-third of the global biomass burning (BB) emissions by widespread fires. BB aerosols are transported westward over the south-eastern Atlantic with the mid-tropospheric winds, resulting in significant
Externí odkaz:
https://doaj.org/article/61e45123be44481c9b241e8281b71b25
Autor:
L. Zhang, M. Segal-Rozenhaimer, H. Che, C. Dang, A. J. Sedlacek III, E. R. Lewis, A. Dobracki, J. P. S. Wong, P. Formenti, S. G. Howell, A. Nenes
Publikováno v:
Atmospheric Chemistry and Physics, Vol 22, Pp 9199-9213 (2022)
Biomass burning emissions often contain brown carbon (BrC), which represents a large family of light-absorbing organics that are chemically complex, thus making it difficult to estimate their absorption of incoming solar radiation, resulting in large
Externí odkaz:
https://doaj.org/article/68255d04437a4eb9bcbce1c4541c19a2
Publikováno v:
The Cryosphere, Vol 16, Pp 1197-1220 (2022)
Accurate modeling of cryospheric surface albedo is essential for our understanding of climate change as snow and ice surfaces regulate the global radiative budget and sea-level through their albedo and mass balance. Although significant progress has
Externí odkaz:
https://doaj.org/article/a93a2207819c4e5297c7f71b9ab4a77f
Autor:
C.-H. Lu, Q. Liu, S.-W. Wei, B. T. Johnson, C. Dang, P. G. Stegmann, D. Grogan, G. Ge, M. Hu, M. Lueken
Publikováno v:
Geoscientific Model Development, Vol 15, Pp 1317-1329 (2022)
The Community Radiative Transfer Model (CRTM), a sensor-based radiative transfer model, has been used within the Gridpoint Statistical Interpolation (GSI) system for directly assimilating radiances from infrared and microwave sensors. We conducted nu
Externí odkaz:
https://doaj.org/article/d15ae18d57de4d86bff00be43f14dea0
Autor:
M. G. Flanner, J. B. Arnheim, J. M. Cook, C. Dang, C. He, X. Huang, D. Singh, S. M. Skiles, C. A. Whicker, C. S. Zender
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 7673-7704 (2021)
The Snow, Ice, and Aerosol Radiative (SNICAR) model has been used in various capacities over the last 15 years to model the spectral albedo of snow with light-absorbing constituents (LACs). Recent studies have extended the model to include an adding-
Externí odkaz:
https://doaj.org/article/d7fa227e4c16425e989e8c97a62b9658
Autor:
R. M. Miller, G. M. McFarquhar, R. M. Rauber, J. R. O'Brien, S. Gupta, M. Segal-Rozenhaimer, A. N. Dobracki, A. J. Sedlacek, S. P. Burton, S. G. Howell, S. Freitag, C. Dang
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 14815-14831 (2021)
During the 3 years of the ObseRvations of Aerosols above CLouds and their intEractionS (ORACLES) campaign, the NASA Orion P-3 was equipped with a 2D stereo (2D-S) probe that imaged particles with maximum dimension (D) ranging from 10 < D < 1280 µm.
Externí odkaz:
https://doaj.org/article/5f307640dc2648daa35f764c8b6269be
Publikováno v:
The Cryosphere, Vol 13, Pp 2325-2343 (2019)
Snow is an important climate regulator because it greatly increases the surface albedo of middle and high latitudes of the Earth. Earth system models (ESMs) often adopt two-stream approximations with different radiative transfer techniques, the same
Externí odkaz:
https://doaj.org/article/5c2770bb2cd04dc5836b0c62da159f86
Publikováno v:
Atmospheric Chemistry and Physics, Vol 15, Iss 22, Pp 12805-12822 (2015)
The Community Atmosphere Model (CAM5), equipped with a technique to tag black carbon (BC) emissions by source regions and types, has been employed to establish source–receptor relationships for atmospheric BC and its deposition to snow over western
Externí odkaz:
https://doaj.org/article/7b77a1dc32c343ceb0afe1856f586d8d