Show simple item record

dc.contributor.authorGloersen, Per
dc.date.accessioned2017-06-09T14:00:02Z
dc.date.available2017-06-09T14:00:02Z
dc.date.copyright1984/02/01
dc.date.issued1984
dc.identifier.issn0733-3021
dc.identifier.otherams-10669.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145811
dc.description.abstractGlobal displays of sea surface temperatures (SST's) from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR) are obtained with spatial sampling intervals as small as 50 km rather than the 150 km spacing normally used for such retrievals. An example is illustrated using a composite global SMMR data set for January 1979, a preliminary version of the SST retrieval algorithm, and a sampling interval of 100 km. The results were found to be in qualitative agreement with in situ and climatic data, insofar as such comparisons were attempted. In addition to the expected climatic patterns, the global oceanic isotherms contain oscillations that are clearly not instrumental but geophysical in nature.
dc.publisherAmerican Meteorological Society
dc.titleSea Surface Temperatures from Nimbus-7 SMMR Radiances
dc.typeJournal Paper
dc.journal.volume23
dc.journal.issue2
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1984)023<0336:SSTFNS>2.0.CO;2
dc.journal.fristpage336
dc.journal.lastpage340
dc.treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 002
dc.contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record