Rain Impacts on the Surface Atmosphere and Upper Ocean in the Central Equatorial Pacific

dc.contributor.author	Daniel B. Whitt
dc.date.accessioned	2023-04-12T18:29:14Z
dc.date.available	2023-04-12T18:29:14Z
dc.date.copyright	2022/09/01
dc.date.issued	2022
dc.identifier.other	JPO-D-22-0033.1.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl1/handle/yetl/4289749
dc.description.abstract	The impacts of rainy days (>24 mm) on the physics of the surface atmosphere and upper ocean are characterized in the central Pacific Ocean (140°–170°W) on the equator, where deep-cycle turbulence substantially influences the sea surface temperature and air–sea heat flux on diurnal and longer time scales. Here, rainfall is relatively weak on average (1–3 mm day
dc.publisher	American Meteorological Society
dc.title	Rain Impacts on the Surface Atmosphere and Upper Ocean in the Central Equatorial Pacific
dc.type	Journal Paper
dc.journal.volume	52
dc.journal.issue	9
dc.journal.title	Journal of Physical Oceanography
dc.identifier.doi	10.1175/JPO-D-22-0033.1
dc.journal.fristpage	1969
dc.journal.lastpage	1991
dc.page	1969–1991
dc.tree	Journal of Physical Oceanography:;2022:;volume( 052 ):;issue: 009
dc.contenttype	Fulltext