Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Adam B. Sokol"'
Autor:
Adam B. Sokol, Dennis L. Hartmann
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 14, Iss 7, Pp n/a-n/a (2022)
Abstract This study examines how the congestus mode of tropical convection is expressed in numerical simulations of radiative‐convective equilibrium (RCE). We draw insights from the ensemble of cloud‐resolving models participating in the RCE Mode
Externí odkaz:
https://doaj.org/article/b160b6d9fae844239e346bd45a2e3a10
Autor:
Fayçal Lamraoui, Martina Krämer, Armin Afchine, Adam B. Sokol, Sergey Khaykin, Apoorva Pandey, Zhiming Kuang
Publikováno v:
Atmospheric Chemistry and Physics. 23:2393-2419
Cirrus clouds that form in the tropical tropopause layer (TTL) can play a key role in vertical transport through the upper troposphere and lower stratosphere, which can significantly impact the radiative energy budget and stratospheric chemistry. How
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af17c34cd4ebf007ee0deb16dc39409f
https://doi.org/10.5194/acp-23-2393-2023
https://doi.org/10.5194/acp-23-2393-2023
Publikováno v:
Journal of Climate. 35:6253-6265
The vertical profile of clear-sky radiative cooling places important constraints on the vertical structure of convection and associated clouds. Simple theory using the cooling-to-space approximation is presented to indicate that the cooling rate in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::445486dd76c48cdafe3ea0022d617c38
https://doi.org/10.1175/jcli-d-21-0861.1
https://doi.org/10.1175/jcli-d-21-0861.1
Autor:
Fayçal Lamraoui, Martina Krämer, Armin Afchine, Adam B. Sokol, Sergey Khaykin, Apoorva Pandey, Zhiming Kuang
Publikováno v:
Atmospheric chemistry and physics / Discussions (2022). doi:10.5194/acp-2022-670
Cirrus clouds that form in the tropical tropopause layer (TTL) can play a key role in vertical transport through the upper troposphere and lower stratosphere, which can significantly impact the radiative energy budget and stratospheric chemistry. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c6be150c61f4fcca6fa5d4a2681cd325
https://hdl.handle.net/2128/33149
https://hdl.handle.net/2128/33149
Satellite observations of tropical maritime convection indicate an afternoon maximum in anvil cloud fraction that cannot be explained by the diurnal cycle of deep convection peaking at night. We use idealized cloud-resolving model simulations of sing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2257a1c390eb11946d072e957746d1f4
https://doi.org/10.1002/essoar.10506580.2
https://doi.org/10.1002/essoar.10506580.2
Autor:
Adam B. Sokol, Dennis L. Hartmann
The radiative cooling rate in the tropical upper troposphere is expected to increase as climate warms. Since the tropics are approximately in radiative–convective equilibrium (RCE), this implies an increase in the convective heating rate, which is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b00f4025093a4ab89ce699792ccb1d7
https://doi.org/10.1002/essoar.10508040.1
https://doi.org/10.1002/essoar.10508040.1
Geostationary satellite observations of tropical maritime convection indicate an afternoon maximum in anvil cloud fraction that cannot be explained by the diurnal cycle of deep convection peaking in the night. This implies that the daytime anvils mus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1576fb71900f576de5e5b548075dc368
https://doi.org/10.5194/egusphere-egu21-785
https://doi.org/10.5194/egusphere-egu21-785
Autor:
Dennis L. Hartmann, Adam B. Sokol
Publikováno v:
Journal of Geophysical Research: Atmospheres. 125
The evolution of anvil clouds detrained from deep convective systems has important implications for the tropical energy balance and is thought to be shaped by radiative heating. We use combined rad...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e7d88907b81c6c8d8cc0c6bf602c83bf
https://doi.org/10.1029/2020jd033107
https://doi.org/10.1029/2020jd033107