Show simple item record

contributor authorAnna-Lena Deppenmeier
contributor authorFrank O. Bryan
contributor authorWilliam S. Kessler
contributor authorLuAnne Thompson
date accessioned2023-04-12T18:34:06Z
date available2023-04-12T18:34:06Z
date copyright2022/10/21
date issued2022
identifier otherJPO-D-21-0316.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289892
description abstractThe 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 isotherms sloping up to the east, but it also includes water mass transformation and consequent diabatic (cross-isothermal) flow (
publisherAmerican Meteorological Society
titleDiabatic Upwelling in the Tropical Pacific: Seasonal and Subseasonal Variability
typeJournal Paper
journal volume52
journal issue11
journal titleJournal of Physical Oceanography
identifier doi10.1175/JPO-D-21-0316.1
journal fristpage2657
journal lastpage2668
page2657–2668
treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 011
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record