contributor author | Li, Z. X. | |
contributor author | Conil, S. | |
date accessioned | 2017-06-09T16:15:28Z | |
date available | 2017-06-09T16:15:28Z | |
date copyright | 2003/12/01 | |
date issued | 2003 | |
identifier issn | 0894-8755 | |
identifier other | ams-6430.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4205401 | |
description abstract | A high-resolution atmospheric general circulation model (GCM) is used to evaluate the atmospheric response to North Atlantic sea surface temperature (SST) anomalies. The transient evolution of the response is studied in detail. The linear and nonlinear effects can thus be contrasted and separated by their different time scales. Baroclinic patterns related directly to the surface anomalies quickly reach their maximum manifestation. However, barotropic patterns related to the mid- and upper troposphere eddy vorticity fluxes have longer time scales with much more important amplitude, able to gradually replace the initial baroclinic response. This study thus provides an evolutional picture of the two types of response in a GCM. | |
publisher | American Meteorological Society | |
title | Transient Response of an Atmospheric GCM to North Atlantic SST Anomalies | |
type | Journal Paper | |
journal volume | 16 | |
journal issue | 23 | |
journal title | Journal of Climate | |
identifier doi | 10.1175/1520-0442(2003)016<3993:TROAAG>2.0.CO;2 | |
journal fristpage | 3993 | |
journal lastpage | 3998 | |
tree | Journal of Climate:;2003:;volume( 016 ):;issue: 023 | |
contenttype | Fulltext | |