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| Registros recuperados: 287 | |
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| Walker, C.D.; Brunel, Jean-Pierre; Dunin, F.X.; Edwards, W.R.N.; Hacker, J.M.; Hartmann, J.; Jupy, D.L.; Reyenga, W.; Schwerdtfeger, P; Shao, Y.; Williams, A.E.. |
| Tipo: Text |
Palavras-chave: EVAPOTRANSPIRATION; PRODUCTION VEGETALE; PLANTE; BESOIN EN EAU; FLUX ENERGETIQUE; TEMPERATURE DE SURFACE; DONNEES SATELLITE; METHODOLOGIE; ETUDE COMPARATIVE; METHODE DE BOWEN. |
| Ano: 1990 |
URL: http://www.documentation.ird.fr/hor/fdi:41632 |
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| Meyers, G.; Bailey, R.; Lindstrom, E.; Phillips, H.. |
| The Southern Oscillation Index (SOI), equatorial zonal wind, sea level anomalies at islands, sea surface temperature at Puerto Chicama Peru and mixed layer temperature and depth from the XBT ship of opportunity network are used to describe conditions during the past two ENSO episodes. Onset of sustained ENSO anomalies in the 1986/87 episode was in July 1986, one month later in the year onset of the 1982/83 episode in June 1982. Both episodes of the 1980's the usual surface temperature difference along the equator between 165°W and 160°E reversed and rapidly increased to 1°C in the order direction. ENSO warming of the central Pacific tends to be confined to the region 10°N-10°S whereas cooling of the western Pacific occurs in a broader region from... |
| Tipo: Text |
Palavras-chave: INTERACTION OCEAN ATMOSPHERE; TEMPERATURE DE SURFACE; ETUDE COMPARATIVE; ANOMALIE; FLUX THERMIQUE; ENSO. |
| Ano: 1989 |
URL: http://www.documentation.ird.fr/hor/fdi:30211 |
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| Goodrich, D.C; Chehbouni, Abdelghani; Goff, B.; MacNish, B.; Maddock, T.; Moran, S.; Shuttleworth, W.J.; Williams, D.G.; Toth, J.J.; Watts, C.; Hipps, L.H.; Cooper, D.I.; Schieldge, J.; Kerr, Y.H.; Arias, H.; Kirkland, M.; Carlos, R.; Kepner, W.; Jones, B.; Avissar, R.; Bégué, A.; Boulet, Gilles; Branan, B.; Braud, I.; Brunel, Jean-Pierre; Chen, L.C.; Clarke, T.; Davis, M.R.; Dauzat, J.; DeBruin, H.; Dedieu, G.; Eichinger, W.E.; Elguero, Eric; Everitt, J.; Garatuza-Payan, J.; Garibay, A.; Gempko, V.L.; Gupta, H.; Harlow, C.; Hartogensis, O.; Helfert, M.; Holifield, C.; Hymer, D.; Kahle, A.; Keefer, T.; Krishnamoorthy, S.; Lhomme, Jean-Paul; Lo Seen, D.; Luquet, D.; Marsett, R.; Monteny, Bruno; Ni, W.; Nouvellon, Y.; Pinker, R.; Peters, C.; Pool, D.; Qi, J.; Rambal, S.; Rey, H.; Rodriguez, J.; Sano, E.; Schaeffer, S.M.; Schulte, M.; Scott, R.; Shao, X.; Synder, K.A.; Sorooshian, S.; Unkrich, C.L.; Whitaker, M.; Yucel, I.. |
| Tipo: Text |
Palavras-chave: BILAN HYDRIQUE; ECOLOGIE; BIODIVERSITE; RELATION CLIMAT COUVERT VEGETAL; ATMOSPHERE; FLUX THERMIQUE; TEMPERATURE DE SURFACE; VEGETATION; CROISSANCE; EVAPOTRANSPIRATION; RESSOURCES EN EAU; EAU DE SURFACE; EAU SOUTERRAINE; TELEDETECTION; MESURE IN SITU; VARIATION TEMPORELLE; MODELISATION; ESTIMATION; PROGRAMME DE RECHERCHE; RECHERCHE PLURIDISCIPLINAIRE. |
| Ano: 1997 |
URL: http://www.documentation.ird.fr/hor/fdi:010023310 |
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| Hastenrath, S.; Merle, Jacques. |
| The subsurface thermal structure in the Tropical Atlantic ocean (30°N-20°S, East of 80°W) is studied on the basis of an extensive data bank of subsurface soundings. Calendar monthly maps are presented showing mixed layer depth, base of thermocline, thermocline thickness, and vertical temperature gradient across the thermocline. These maps are complemented by vertical cross sections depicting mixed layer depth, base of thermocline, and selected isotherms : a zonal profile along the equator (50°W-10°E), a meridional transect across the Eastern Atlantic (4°N-18°S), and a meridional section across the Central Atlantic (30°N-18°S). (D'après résumé d'auteur) |
| Tipo: Text |
Palavras-chave: FLUX THERMIQUE; THERMOCLINE; TEMPERATURE DE SURFACE. |
| Ano: 1987 |
URL: http://www.documentation.ird.fr/hor/fdi:43826 |
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| Merle, Jacques; Fieux, M.; Hisard, Philippe. |
| Analysis of historical data including coastal and open ocean data provides a quantitative description of the characteristics of the sea surface annual signal and of the interannual anomalies in the Eastern Equatorial Atlantic ocean. The annual signal has a larger amplitude than the interannual anomalies but has considerable spatial variations. In two regions, namely the Northern coast of the Gulf of Guinea and the equator, both annual and interannual variability are particularly large because of a seasonal surfacing of the thermocline. Eastward advection of warm water by the countercurrent system, local rain and runoff of great rivers could contribute significantly to the seasonal and interannual STT variability. Interannual anomalies have alarge spatial... |
| Tipo: Text |
Palavras-chave: TEMPERATURE DE SURFACE; ANOMALIE DE TEMPERATURE; VARIATION INTERANNUELLE; MODELISATION. |
| Ano: 1979 |
URL: http://www.documentation.ird.fr/hor/fdi:010004525 |
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| Registros recuperados: 287 | |
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