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		<issn>0148-0227</issn>
		<issn>2156-2202</issn>
		<citationkey>GrodskyCaPrSeLoMc:2005:CaStUs</citationkey>
		<title>Tropical instability waves at 0 degrees N, 23 degrees W in the Atlantic: A case study using Pilot Research Moored Array in the Tropical Atlantic (PIRATA) mooring data</title>
		<project>PIRATA</project>
		<year>2005</year>
		<month>Aug.</month>
		<secondarytype>PRE PI</secondarytype>
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		<size>800 KiB</size>
		<author>Grodsky,  S. A.,</author>
		<author>Carton,  J. A.,</author>
		<author>Provost,  C.,</author>
		<author>Servain,  J.,</author>
		<author>Lorenzzetti,  João Antonio,</author>
		<author>McPhaden,  M. J.,</author>
		<group>DSR-INPE-MCT-BR</group>
		<affiliation>Univ Maryland, Dept Atmospher & Ocean Sci</affiliation>
		<affiliation>Univ Maryland, Dept Atmospher & Ocean Sci</affiliation>
		<affiliation>Univ Paris 06, Lab Oceanog Dynam & Climatol, Paris</affiliation>
		<affiliation>Inst Rech Dev, UR 065, Brest, France</affiliation>
		<affiliation>INPE, Remote Sensing Div, Sao Jose dos Campos, Brasil</affiliation>
		<affiliation>NOAA, Pacific Marine Environm Lab, Seattle, WA, USA</affiliation>
		<journal>Journal of Geophysical Research</journal>
		<volume>110</volume>
		<number>C8</number>
		<pages>Art. No. C08010</pages>
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		<keywords>OCEANOGRAFIA, oceano Atlântico,salinidade,ondas, temperatura da superfície do mar, oceanography, sea-surface temperature, equatorial pacific-ocean, long waves, mixed-layer, cold-tongue, currents, energetics, model, heat, circulation.</keywords>
		<abstract>Temperature, salinity, velocity, and wind from a mooring at 0N, 23 Ware used along with satellite data for sea surface temperature and sea level to examine the contribution of tropical instability waves (TIWs) to the energy and heat balance of the equatorial Atlantic mixed layer. The TIWs appear as periodic 2030 day fluctuations of currents, temperature, and salinity, which intensify beginning in June and peak in late boreal summer. The intensification occurs in phase with strengthening of the southeasterly trade winds and the seasonal appearance of the equatorial tongue of cold mixed layer temperatures. In 2002 these waves, which warm the mixed layer by 0.35 C during summer months, are maintained by both barotropic and baroclinic conversions that are of comparable size. Salinity fluctuations, previously neglected, increase the magnitude of baroclinic energy conversion.</abstract>
		<area>SRE</area>
		<language>en</language>
		<targetfile>tropical instability.pdf</targetfile>
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