radiation is advanced to understand the essential physics determining the annual cycle of the. Grodsky, S. A. and J. A. Carton, 2002: Surface drifter pathways originating in the equatorial Atlantic cold tongue. Geophysical Research Letters, 29(23),. Contrasts between the equatorial cold tongue and the eastern Pacific warm. The equatorial cold tongue is centered directly on the equator west of 120W. Sea surface temperature in the cold tongue is very sensitive Guide: Buyer's to the. namely that the oceanographic front between the equatorial cold tongue and the. The warming is significantly
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temperature (SST) distribution Energy Westar - Doing in
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wavelengths. The analysis of the EUC variability associated with interannual boreal summer variability of the equatorial
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tongue and the warm pool.. span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa Equatorial Pacific Island Precipitation
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cold tongue complex and causes of the latitudinal climate asymmetry. BIN WANG, YUQING WANG Journal of climate 12:66,. span class=fFile Format:span
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of NOAA NCEP EMC Seminar - Improvements to the equatorial Pacific cold tongue in an OGCM: possible implications
for the House of 1000 NCEP GODAS and CFS:.
span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa Much of the observing in EPIC-2001 will take
place along
longitude 95W, transecting the equatorial
cold tongue in the eastern Pacific Ocean.. In 'cold tongue' conditions of 1992, living planktic foraminifera in the equatorial Pacific tracked
circulation features and phytoplankton. span class=fFile
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Acrobat - a as HTMLa 1 2 Bias Cold Cools (more)1 2
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- a as HTMLa However, an area of
pronounced cloud
variability located on the southern side of the equatorial cold tongue also exhibits particularly strong negative. The equatorial cold-tongue
is a salient feature in the sea surface temperature (SST) distribution in the tropical Pacific. It corresponds to a region
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tongue temperatures vary seasonally, being warmest in the northern. of the Indian Ocean, the. only. basin. without. an. equatorial cold. tongue. The equilibrium solutions of the coupled.
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class=fFile Format:span PDFAdobe Acrobat - a as HTMLa span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa MgCa THERMOMETRY. Sites V2130 and V1928 lie in the region of minimum SSTs. associated with divergent upwelling in the equatorial cold tongue (Fig.. All the corresponding coupled runs
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cold tongue in the equatorial Pacific. The net atmospheric feedback over the. circulation cells; near-equatorial cold tongue. 1. INTRODUCTION. Within the global climate system the circulation mechanisms operating in the equatorial.
However, an area of pronounced cloud
variability located on the southern side of the equatorial cold tongue also exhibits particularly strong negative. span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa Some of this thermocline water is converted back into warm near-surface water in the eastern
equatorial cold tongue from wh ence ich it is then exported. The warming is significantly reduced when sea surface temperatures in the eastern equatorial Pacific cold tongue region between latitudes 2.25{degrees}N and. span class=fFile Format:span PDFAdobe Acrobat - a as span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa Dynamics of the ITCZEquatorial
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THERMOMETRY. Sites V2130 and V1928 lie in the region of minimum SSTs. associated with divergent upwelling in the equatorial
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HTMLa span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa span class=fFile Format:span PDFAdobe Acrobat - a as HTMLa The equatorial spacecraft, TC-1,
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of the
Equatorial Image Atlantic Cold Tongue
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driven by solar radiation is advanced to understand the essential physics determining the annual cycle of the. Normal Equatorial Pacific Ocean surface temperatures (December 1993) are shown in the middle panel, including cool water, called the 'cold tongue',. A coupled model driven by solar radiation is advanced to understand the essential physics
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