Résultats de la recherche (4 résultats)
- > Centre national d'Etudes spatiales. (CNES), France (supprimer)
Affinez votre recherche
Par Collection Par Auteur- Centre national d'Etudes spatiales. (CNES), France (4)
- SHISHKOV, Y. A. (1)
- BRIMBLECOMBE, P. (1)
- MONIN, A. S. (1)
- PRELL, W. L. (1)
- REITER, E. R. (1)
- 1979 (4)
- Physical geography (4)
- Action anthropique ; Atmosphère ; Composition chimique ; Composition de l'air ; Géographie physique ; Variation climatique ; Variation historique (1)
- Bilan thermique ; Géographie physique ; Hydrologie marine ; Interaction ; Rétroaction ; Système océan-atmosphère ; Variabilité ; Variation climatique (1)
- Glaciation ; Géographie physique ; Paléogéographie ; Précambrien ; Période glaciaire (1)
- Géographie physique ; Mer d'Oman ; Océan ; Océan Indien ; Paléo-océanographie ; Quaternaire marin ; Remontée d'eau ; Upwelling (1)
- Glacial/Interglacial variability of monsoonal upwelling: western Arabian sea in Evolution des atmosphères planétaires et climatologie de la terre=Evolution of planetary atmospheres and climatology of the earth. (1)
- Historical changes in atmospheric trace components in Evolution des atmosphères planétaires et climatologie de la terre=Evolution of planetary atmospheres and climatology of the earth. (1)
- Ice ages in the Earth history in Evolution des atmosphères planétaires et climatologie de la terre=Evolution of planetary atmospheres and climatology of the earth. (1)
- The interannual variability of the ocean-atmosphere system as a consequence of feedback mechanisms in Evolution des atmosphères planétaires et climatologie de la terre=Evolution of planetary atmospheres and climatology of the earth. (1)
- ... Compared to modern conditions, the western Arabian Sea had more intense upwelling characterized by maximum frequency of G. bulloides and lowest SST (22C) during mid-Termination I and more tropical conditions and higher SST (26C) near the base
- current, but perhaps even more so by local air-sea interaction. Zonal atmospheric wind stress variations strongly affect the meridional SST anomaly gradients in the Central North Pacific-even more so than the meridional SST anomaly gradients in the Central
- North Pacific-, even more so than the SST anomalies.
- Early analyses have not been used frequently in attempts to find changes in the trace composition of the atmosphere. In the case of rainfall analyses records stretch back more than 100 years at some sites, and a long record at Rothamsted in England
- (as their patterns are). To verify the thesis paleogeographic reconstructions of the eras more ancient than the Phanerozoic needed.