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contributor authorHuang, Wen-Yu
contributor authorWang, Bin
contributor authorYu, Yong-Qiang
contributor authorLi, Li-Juan
date accessioned2017-06-09T17:25:12Z
date available2017-06-09T17:25:12Z
date copyright2014/02/01
date issued2013
identifier issn0739-0572
identifier otherams-84907.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228295
description abstractetter computational stability is achieved in an improved version of the National Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG)/Institute of Atmospheric Physics (IAP) Climate Ocean Model, version 2 (LICOM2, the standard version), after improvements to the implementations of the vertical mixing, mesoscale eddy parameterization, and bottom drag schemes. The large warm biases of LICOM2 in the western Pacific Ocean and eastern Indian Ocean warm pool and on the east coast of the Pacific Ocean are significantly improved. The salinity bias in the tropical Pacific Ocean related to the warm bias of the warm pool is also alleviated. The simulation of the Atlantic meridional overturning circulation is improved because of enhanced vertical mixing in the high latitudes of the North Atlantic Ocean. The new version also presents a stronger Deacon cell, and thus a more powerful Antarctic Circumpolar Current that is closer to the observation, due to weaker southward mesoscale eddy transport in the Southern Ocean.
publisherAmerican Meteorological Society
titleImprovements in LICOM2. Part I: Vertical Mixing
typeJournal Paper
journal volume31
journal issue2
journal titleJournal of Atmospheric and Oceanic Technology
identifier doi10.1175/JTECH-D-13-00065.1
journal fristpage531
journal lastpage544
treeJournal of Atmospheric and Oceanic Technology:;2013:;volume( 031 ):;issue: 002
contenttypeFulltext


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