Zobrazeno 1 - 10
of 115
pro vyhledávání: '"Frank O. Bryan"'
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 13, Pp n/a-n/a (2023)
Abstract Air‐sea flux variability has contributions from both ocean and atmosphere at different spatio‐temporal scales. Atmospheric synoptic scales and the air‐sea turbulent heat flux that they drive are well represented in climate models, but
Externí odkaz:
https://doaj.org/article/ad8f97598b7d4afaab909372128915bc
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 5, Pp 1189-1206 (2019)
Abstract Recent studies have explored the sensitivity of global ocean model simulations to the treatment of riverine freshwater and the representation of estuarine processes via an estuary box model applied within Community Earth System Model (CESM).
Externí odkaz:
https://doaj.org/article/6ce39e54049a45589798852350677e36
Autor:
Xiaoning Wu, Kevin A. Reed, Christopher L. P. Wolfe, Gustavo M. Marques, Scott D. Bachman, Frank O. Bryan
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 13, Iss 4, Pp n/a-n/a (2021)
Abstract Idealized models can reveal insights into Earth’s climate system by reducing its complexities. However, their potential is undermined by the scarcity of fully coupled idealized models with components comparable to contemporary, comprehensi
Externí odkaz:
https://doaj.org/article/909a136e976e4d20839374a04dea4f62
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 12, Iss 10, Pp n/a-n/a (2020)
Abstract The thermal component of oceanic eddy available potential energy (EPE) generation due to air‐sea interaction is proportional to the product of anomalous sea surface temperature (SST) and net air‐sea heat flux (SHF). In this study we asse
Externí odkaz:
https://doaj.org/article/4c3881cb5c4c42e19c97b1a7c6a99232
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 12, Iss 2, Pp n/a-n/a (2020)
Abstract Oceanic mesoscale eddies are known to diffuse and stir tracers, and the development of skillful eddy closures is aided considerably by the accurate diagnosis of these processes from eddy‐resolving model statistics. In this work a multiple
Externí odkaz:
https://doaj.org/article/5b00f1c011b7459c83990a157810f6af
Publikováno v:
Journal of Physical Oceanography. 52:2657-2668
The equatorial Pacific zonal circulation is composed of westward surface currents, the eastward equatorial undercurrent (EUC) along the thermocline, and upwelling in the eastern cold tongue. Part of this upwelling arises from water flowing along isot
The mixing of tracers by mesoscale eddies, parameterized in many ocean general circulation models (OGCMs) as a diffusive-advective process, contributes significantly to the distribution of tracers in the ocean. In the ocean interior, diffusive contri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::92bf1c83bfdffc8a3fc9e5736305fce3
https://doi.org/10.22541/essoar.168167292.27837727/v1
https://doi.org/10.22541/essoar.168167292.27837727/v1
Publikováno v:
Journal of Physical Oceanography. 52:789-804
The water mass transformation (WMT) framework describes how water of one class, such as a discrete interval of density, is converted into another class via air–sea fluxes or interior mixing processes. This paper investigates how this process is mod
Autor:
Lucas C. Laurindo, R. Justin Small, LuAnne Thompson, Leo Siqueira, Frank O. Bryan, Ping Chang, Gokhan Danabasoglu, Igor V. Kamenkovich, Ben P. Kirtman, Hong Wang, Shaoqing Zhang
Publikováno v:
Journal of Geophysical Research: Oceans. 127