Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Casey R. Patrizio"'
Autor:
Casey R. Patrizio, David A. Randall
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 7, Pp 1995-2019 (2019)
Abstract A 3‐D cloud‐resolving model has been used to investigate the domain size dependence of simulations of convective self‐aggregation (CSA) in radiative‐convective equilibrium. We investigate how large a domain is needed to allow multipl
Externí odkaz:
https://doaj.org/article/4c06e761558f436d838066bef575096b
Publikováno v:
Journal of Climate. 35:3313-3333
In a recent paper, we argued that ocean dynamics increase the variability of midlatitude sea surface temperatures (SSTs) on monthly to interannual time scales, but act to damp lower-frequency SST variability over broad midlatitude regions. Here, we u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb4636f1e73f90be4b2d16246accf712
https://doi.org/10.1175/jcli-d-21-0184.1
https://doi.org/10.1175/jcli-d-21-0184.1
Autor:
David A. Randall, Casey R. Patrizio
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 7, Pp 1995-2019 (2019)
A 3‐D cloud‐resolving model has been used to investigate the domain size dependence of simulations of convective self‐aggregation (CSA) in radiative‐convective equilibrium. We investigate how large a domain is needed to allow multiple convect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::96e8fca4bf8fb40096137638fce68eec
https://doi.org/10.1029/2019ms001672
https://doi.org/10.1029/2019ms001672
Understanding the role of the ocean in climate variability requires first understanding the role of ocean dynamics in the ocean mixed layer and thus sea surface temperature variability. However, key aspects of the spatially and temporally varying con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1f1382b95431ee7146dafc5d79cd5933
https://ueaeprints.uea.ac.uk/id/eprint/85510/
https://ueaeprints.uea.ac.uk/id/eprint/85510/
