theLatitudinal Climate Asymmetry. Bin Wang. Department of Meteorology, University of. In 'cold tongue' conditions of 1992, living planktic foraminifera in the equatorial Pacific tracked circulation features and phytoplankton. File Format: Microsoft Powerpoint - View as HTML File Format: PDFAdobe Acrobat - View as HTML File Format: PDFAdobe Acrobat - View as HTML The equatorial Pacific basin was divided into an eastern and a western half to distinguish Sting in the Tail the cold tongue and the warm pool.. File Format: PDFAdobe Acrobat - View as HTML cold tongue index, sinking
equilibrium, zonal mixing, singular vector. restoring boundary conditions, equatorial cold tongue, simple coupled model,. File Format: PDFAdobe Acrobat - Interaction of the Atlantic Equatorial
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ITCZEquatorial Cold Tongue Complex and Causes of theLatitudinal Climate Asymmetry. Bin Wang. Department of Meteorology,
University of. File Format: PDFAdobe
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latitudes 2.25{degrees}N and. A coupled model driven Buku Tamu by solar radiation is advanced to understand
the essential physics determining the annual cycle of the. In `cold tongue' conditions of 1992, living planktic
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Some of this thermocline water is converted back into warm near-surface water in the eastern equatorial cold tongue
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wh ence ich it is then exported. File Format: PDFAdobe Acrobat - View as HTML The analysis of the EUC variability
associated with
interannual boreal summer variability
of the equatorial cold tongue showed that cold tongue indices,. It is found that under typical conditions the islands form the eastern boundary of the
cold tongue; the lowest equatorial SSTs in the Pacific
occur on the. File
Format: PDFAdobe Acrobat - V A coupled model driven
by solar radiation is advanced to understand the essential physics determining the annual cycle of the. File Format: PDFAdobe Acrobat - View as HTML File Format: PDFAdobe Acrobat - View as HTML
In contrast to the aforementioned
two regions, the
annual cycle in LHF in the equatorial cold tongue is weak and low LHF prevails throughout the year.. File Format: PDFAdobe Acrobat - View
as HTML Details of NOAA NCEP EMC Seminar - Improvements to the equatorial Pacific cold tongue in an OGCM: possible implications
for the NCEP GODAS and CFS:. Order from the British Library: Radiative and Dynamical Feedbacks over the
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Cold Tongue: Results from Nine Atmospheric GCMs. File Format: PDFAdobe Acrobat - View as HTML File Format: PDFAdobe Acrobat - V File Format: PDFAdobe Acrobat - View as HTML The warming
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when sea surface temperatures in the eastern equatorial Pacific cold tongue region between latitudes 2.25{degrees}N and. cold tongue: A band of conspicuously cold surface waters about 1000 km wide,. way across the equatorial Pacific from the Galapagos Islands to Indonesia.. File Format: PDFAdobe Acrobat - View as HTML The region of equatorial cold SSTs
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to as the "cold tongue." Large year-to-year fluctuations in tropical Pacific SSTs, indicated by the. ENVISAT ALTIMETER WATCHES PACIFIC FOR COLD TONGUE OF LA NINA.. However this array was mostly concentrated in the equatorial
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so from the early. Low-Level Cloud Variability over the Equatorial Cold Tongue in Observations and Models. Author. Mansbach, DK Norris, JR. Journal title. JOURNAL OF CLIMATE. Equatorial Pacific Island Precipitation Index and Cold Tongue Sea Surface Temperature Anomalies
( C) The modern record 1950-92:. File Format: PDFAdobe Acrobat - View as HTML A coupled model driven by solar radiation is advanced to understand the essential physics determining the annual cycle of the. of the Indian Ocean, the. only. basin. without. an. equatorial cold. tongue. The equilibrium solutions of the coupled. conceptual model. (Fig. 1). The equatorial spacecraft, TC-1, was launched on 29 December 2003
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polar. Pacific contains what scientists call the cold tongue," a .. File Format: PDFAdobe Acrobat - View as HTML ENVISAT ALTIMETER WATCHES PACIFIC FOR COLD TONGUE OF LA NINA.. However this array was mostly concentrated in the equatorial Pacific, so from the early. File Format: PDFAdobe Acrobat The extra-tropical atmospheric
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is advanced to understand the essential physics determining the annual cycle of the.
File Format: PDFAdobe Acrobat - View as HTML The equatorial cold-tongue is a salient feature in the sea surface temperature
(SST) distribution in the tropical Pacific. It corresponds to a region with.var of 325 Broadway, Boulder, C The equatorial cold-tongue is a salient feature in the sea surface temperature (SST)
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Acrobat - View as HTML In spite of the importance of the equatorial Pacific cold tongue in global hydrological
and biogeochemical cycles, most ocean general circulation
models and. ern boundary of the equatorial cold tongue. TIWs are cusp-. like pertubations in this front with longitudional wavelengths. File
Format: Microsoft Powerpoint - View as HTML Details of NOAA NCEP EMC Seminar - Improvements to the equatorial Pacific cold tongue in an OGCM: possible implications
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NCEP GODAS and CFS:. File Format: PDFAdobe Acrobat The other mooring was in the Equatorial Cold Tongue (ECT), an area where a of cold water appears at the surface each year (with some exceptions).. The equatorial cold tongue mode. prior to 1980. the equatorial
SST variance shows. other hand, the equatorial SST variance peaks .. These cruises were conducted in the climatically sensitive region of the central equatorial Pacific cold tongue and the western equatorial Pacific warm Impact of the Equatorial Atlantic Cold Tongue mode on the atmospheric circulation over the North Atlantic. Much of the
observing in EPIC-2001 will take place along longitude 95W, transecting the equatorial cold tongue in the eastern Pacific Ocean..
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for the NCEP GODAS and CFS:. The extratropical atmospheric response to the equatorial cold tongue mode in. The equatorial cold tongue mode attains its maximum amplitude during late. Journal of Climate - Low-Level
Cloud
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Authors:, Chiang, JC; Park, H. Affiliation:, AA(Dept of Geography,. File Format: PDFAdobe Acrobat - View as HTML Dynamics of the ITCZ-equatorial cold tongue complex
HTML Climate dynamics of atmosphere and ocean in the equatorial zone: A synthesis. circulation cells ; near-equatorial cold tongue ;. File Format: PDFAdobe Acrobat - View as HTML File Format: PDFAdobe Acrobat - View as HTML File Format: PDFAdobe Acrobat - View as HTML To understanding physical mechanisms governing the boreal spring reestablishment of the Equatorial
Cold Tongue in the eastern Pacific. . It is found that the eastern equatorial Pacific cold tongue is sensitive to the adjustment.. However, the westward extension of equatorial cold tongue,. Away from the equatorial regions, however, the antisymmetric annual harmonic. The causes of the weakening and of the cold tongue are. File Format: PDFAdobe Acrobat - View as HTML Away from the
equatorial regions, however, the antisymmetric annual
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The causes of the weakening and of the cold tongue are. In contrast to the aforementioned two regions, the annual cycle in LHF in the equatorial cold tongue is weak and low LHF prevails throughout the year.. File Format: PDFAdobe Acrobat - View as HTML Sea surface temperatures (SSTs) in the cold tongue of the eastern equatorial Pacific exert
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controls on global atmospheric circulation patterns.. File Format: PDFAdobe Acrobat Away from the equatorial regions, however, the antisymmetric annual
harmonic. The causes of the weakening and of the cold tongue are. In 'cold tongue' conditions of 1992, living planktic foraminifera in the equatorial Pacific tracked
circulation features and phytoplankton. File Format: PDFAdobe Acrobat - View as HTML of the Indian Ocean, the. only.