Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Pornampai Narenpitak"'
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-17 (2024)
Abstract Solar radiation modification (SRM) has been proposed to temporarily reduce anthropogenic warming. This study presents an assessment of the regional impacts of SRM via solar dimming and stratospheric aerosol injection (SAI) on temperature and
Externí odkaz:
https://doaj.org/article/6385ae316cac4347b566f5b2cd6d66fd
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 16, Iss 9, Pp n/a-n/a (2024)
Abstract We investigate the role of mesoscale organization for the response of trade cumulus (Tc) clouds to climate change. Among four recently identified states of Tc organization, the “Sugar” state has the lowest and the “Flower” state the
Externí odkaz:
https://doaj.org/article/c4eb78be02b34696a806f3bbb66994f1
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 15, Iss 1, Pp n/a-n/a (2023)
Abstract A shallow cumulus cloud transition from a sugar to flower type of organization occurred under a layer of mineral dust on 2 February 2020, during the multinational Atlantic Tradewind Ocean‐Atmosphere Mesoscale Interaction Campaign (ATOMIC)
Externí odkaz:
https://doaj.org/article/9e9d235bf7dc41a78271cfd748d85322
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 13, Iss 10, Pp n/a-n/a (2021)
Abstract The Atlantic Tradewind Ocean‐Atmosphere Mesoscale Interaction Campaign (ATOMIC) took place in January–February, 2020. It was designed to understand the relationship between shallow convection and the large‐scale environment in the trad
Externí odkaz:
https://doaj.org/article/fec6b78ec74f4cc899799074ae25ff58
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 6, Pp 1600-1626 (2019)
Abstract Limited area cloud‐resolving model (CRM) simulations called LASAM are used to reproduce and understand negative subtropical shallow cumulus cloud feedbacks in a near‐global aquaplanet CRM (NGAqua) with 4‐K sea surface temperature (SST)
Externí odkaz:
https://doaj.org/article/480a0c24d6f84c668a0d4409b86e3210
We present a first study showing that organization of trade cumulus (Tc) clouds can significantly enhance Tc response to climate change. Among four recently identified states of Tc organization, the “Flower” state has the highest and the “Sugar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40c76c10ef0b3d0cb6e1348748e4f20b
https://doi.org/10.22541/essoar.167690110.06867051/v1
https://doi.org/10.22541/essoar.167690110.06867051/v1
Publikováno v:
Journal of the Atmospheric Sciences. 77:2847-2863
Tropical cyclogenesis (TCG) is a multiscale process that involves interactions between large-scale circulation and small-scale convection. A near-global aquaplanet cloud-resolving model (NGAqua) with 4-km horizontal grid spacing that produces tropica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86d3efc046c8d9196979c17751404d86
https://doi.org/10.1175/jas-d-20-0021.1
https://doi.org/10.1175/jas-d-20-0021.1
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 13, Iss 10, Pp n/a-n/a (2021)
The Atlantic Tradewind Ocean‐Atmosphere Mesoscale Interaction Campaign (ATOMIC) took place in January–February, 2020. It was designed to understand the relationship between shallow convection and the large‐scale environment in the trade‐wind
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e92735674c1700f4e3cbd91045fb0c8f
https://doaj.org/article/fec6b78ec74f4cc899799074ae25ff58
https://doaj.org/article/fec6b78ec74f4cc899799074ae25ff58
Publikováno v:
Journal of Advances in Modeling Earth Systems. 9:1069-1090
A near-global aquaplanet cloud-resolving model (NGAqua) with fixed meridionally-varying sea-surface temperature (SST) is used to investigate cloud feedbacks due to three climate perturbations: a uniform 4 K SST increase, a quadrupled CO2 concentratio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4b596c1fcfc5920781585ff9ff19d4f
https://doi.org/10.1002/2016ms000872
https://doi.org/10.1002/2016ms000872