contributor author | Panetta, R. Lee | |
contributor author | Held, Isaac M. | |
contributor author | Pierrehumbert, Raymond T. | |
date accessioned | 2017-06-09T14:27:41Z | |
date available | 2017-06-09T14:27:41Z | |
date copyright | 1987/10/01 | |
date issued | 1987 | |
identifier issn | 0022-4928 | |
identifier other | ams-19647.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4155786 | |
description abstract | In order to clarify the extent to which the two-layer model can successfully simulate the remote tropospheric response to localized stationary forcing, the structure of stationary Rossby waves in the two-layer model is compared with that in continuous models. One finds a close correspondence when the two-layer flow is supercritical in the sense of the Phillips' criterion, except for the possibility of upstream propagation in the two-layer model when the lower-layer wind is small. When the two-layer flow is subcritical, the stationary waves can be very seriously distorted. The manner in which neutral modes are spatially or temporally destabilized by damping in the two-layer model is contrasted with similar results for Charney's model. | |
publisher | American Meteorological Society | |
title | External Rossby Waves in the Two-Layer Model | |
type | Journal Paper | |
journal volume | 44 | |
journal issue | 20 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1987)044<2924:ERWITT>2.0.CO;2 | |
journal fristpage | 2924 | |
journal lastpage | 2933 | |
tree | Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020 | |
contenttype | Fulltext | |