Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Tra Dinh"'
Publikováno v:
Journal of Climate. 36:3289-3303
This study investigates the impact of the adjustment times of the atmospheric boundary layer (ABL) on the control of low-cloud coverage (LCC) climatology by large-scale atmospheric conditions in the subtropics. Using monthly data, we calculate back-t
Autor:
Pandit, Amit Kumar, Vernier, Jean-Paul, Fairlie, Thomas Duncan, Bedka, Kristopher M., Avery, Melody A., Gadhavi, Harish, Ratnam, Madineni Venkat, Dwivedi, Sanjeev, Jyothi, Kasimahanthi Amar, Wienhold, Frank G., Vömel, Holger, Hongyu Liu, Bo Zhang, Kumar, Buduru Suneel, Tra Dinh, Jayaraman, Achuthan
Publikováno v:
Atmospheric Chemistry & Physics Discussions; 11/24/2023, p1-45, 45p
Autor:
Mizuno, Seiya 1, 6, Tra, Dinh TH 1, 6, Mizobuchi, Atsushi 1, Iseki, Hiroyoshi 1, 2, Mizuno-Iijima, Saori 1, Kim, Jun-Dal 3, Ishida, Junji 3, Matsuda, Yoichi 4, Kunita, Satoshi 5, Fukamizu, Akiyoshi 3, Sugiyama, Fumihiro 1, Yagami, Ken-ichi 1
Publikováno v:
In Laboratory Investigation March 2014 94(3):321-330
Akademický článek
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Autor:
Huy, Le Duc, Tung, Pham Thanh, Nhu, Le Nguyen Quynh, Linh, Nguyen Tuan, Tra, Dinh Thanh, Thao, Nguyen Vu Phuong, Tien, Tran Xuan, Hai, Hoang Huu, Khoa, Vo Van, Anh Phuong, Nguyen Thi, Long, Hoang Bao, Linh, Bui Phuong
Publikováno v:
PLoS ONE; 7/27/2022, Vol. 17 Issue 7, p1-19, 19p
Autor:
Tra Dinh, Stephan Fueglistaler
Publikováno v:
Journal of Advances in Modeling Earth Systems. 9:2468-2482
In energetic equilibrium, the atmosphere's net radiative divergence (R) is balanced by sensible (S) and latent (L) heat fluxes, i.e. R+S+L=0. Radiative forcing from increasing CO2 reduces R, and the surface warming following an increase in CO2 is lar
Publikováno v:
Atmospheric Chemistry & Physics Discussions; 3/2/2022, p1-20, 20p
Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 22, Pp 12225-12236 (2014)
A high-resolution, two-dimensional numerical model is used to study the moisture redistribution following homogeneous ice nucleation induced by Kelvin waves in the tropical tropopause layer (TTL). We compare results for dry/moist initial conditions a