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Evaluation of NASA's high-resolution global composition simulations: Understanding a pollution event in the Chesapeake Bay during the summer 2017 OWLETS campaign [期刊论文]
Atmospheric Environment, 2020-01-01, 222
Dacic N.;  Sullivan J.T.;  Knowland K.E.;  Wolfe G.M.;  Oman L.D.;  Berkoff T.A.;  Gronoff G.P.
View/Download:21/0
 
Evaluation of NASA's high-resolution global composition simulations: Understanding a pollution event in the Chesapeake Bay during the summer 2017 OWLETS campaign [期刊论文]
Atmospheric Environment, 2020-01-01, 222
Dacic N.;  Sullivan J.T.;  Knowland K.E.;  Wolfe G.M.;  Oman L.D.;  Berkoff T.A.;  Gronoff G.P.
View/Download:35/0
 
The Role of Roughness and Stability on the Momentum Flux in the Marine Atmospheric Surface Layer: A Study on the Southwestern Atlantic Ocean [期刊论文]
Journal of Geophysical Research: Atmospheres, 2018-01-01, 123 (8
Hackerott J.A.;  Pezzi L.P.;  BakhodayPaskyabi M.;  Oliveira A.P.;  Reuder J.;  de Souza R.B.;  deCamargo R.
View/Download:14/0
 
Large-eddy simulation of subtropical cloud-topped boundary layers: 2. Cloud response to climate change [期刊论文]
Journal of Advances in Modeling Earth Systems, 2017-01-01, 9 (1
Tan Z;  , Schneider T;  , Teixeira J;  , Pressel K;  G
View/Download:19/0
 
Large-eddy simulation of subtropical cloud-topped boundary layers: 1. A forcing framework with closed surface energy balance [期刊论文]
Journal of Advances in Modeling Earth Systems, 2016-01-01, 8 (4
Tan Z;  , Schneider T;  , Teixeira J;  , Pressel K;  G
View/Download:23/0
 
The role of precipitation and spatial organization in the response of trade-wind clouds to warming [期刊论文]
Journal of Advances in Modeling Earth Systems, 2016-01-01, 8 (2
Vogel R;  , Nuijens L;  , Stevens B
View/Download:9/0
 
An les model study of the influence of the free tropospheric thermodynamic conditions on the stratocumulus response to a climate perturbation [期刊论文]
Journal of Advances in Modeling Earth Systems, 2015-01-01, 7 (2
Van Der Dussen J;  J;  , De Roode S;  R;  , Gesso S;  D;  , Siebesma A;  P
View/Download:38/0
 

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