Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Matthew T. Luongo"'
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 16, Iss 2, Pp n/a-n/a (2024)
Abstract Positive feedbacks in climate processes can make it difficult to identify the primary drivers of climate phenomena. Some recent global climate model (GCM) studies address this issue by controlling the wind stress felt by the surface ocean su
Externí odkaz:
https://doaj.org/article/7eb1813ffcb84ab6aab3ec083f312b51
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023)
Abstract Previous studies have found that Northern Hemisphere aerosol‐like cooling induces a La Niña‐like response in the tropical Indo‐Pacific. Here, we explore how a coupled ocean‐atmosphere feedback pathway communicates and sustains this
Externí odkaz:
https://doaj.org/article/6e838edfc6ed484a84a3f3e6a96754eb
Autor:
Hung-Yi Tseng, Yen-Ting Hwang, Shang-Ping Xie, Yu-Heng Tseng, Sarah M. Kang, Matthew T. Luongo, Ian Eisenman
Publikováno v:
Journal of Climate. :1-31
This study investigates the transient evolution of tropical Pacific sea surface temperature (SST) responses to a constant northern high latitude solar heating in fully coupled CESM 1.2. The study identifies two stages through multiple ensemble runs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9dfde5e5b8eb6d697771628477ad6192
https://doi.org/10.1175/jcli-d-22-0622.1
https://doi.org/10.1175/jcli-d-22-0622.1
Publikováno v:
Journal of Climate, vol 35, iss 20
Cross-equatorial ocean heat transport (OHT) changes have been found to damp meridional shifts of the intertropical convergence zone (ITCZ) induced by hemispheric asymmetries in radiative forcing. Zonal-mean energy transport theories and idealized mod
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8765cdd0cdd752587e18751c0b65b12f
https://doi.org/10.1175/jcli-d-21-0950.1
https://doi.org/10.1175/jcli-d-21-0950.1
Positive feedbacks in climate processes can obscure the initial drivers of climate phenomena. Some recent global climate model (GCM) studies partially circumvent this issue by controlling the wind stress felt by the surface ocean such that the atmosp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11a0386e65373aae183c3b95d6192211
https://doi.org/10.22541/essoar.167839714.45887321/v1
https://doi.org/10.22541/essoar.167839714.45887321/v1
