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Par Collection Par Auteur- PRELL, W. L. (2)
- Centre national d'Etudes spatiales. (CNES), France (1)
- GEITZENAUER, K. (1)
- HUTSON, W. H. (1)
- MOLFINO, B. (1)
- WILLIAMS, D. F. (1)
- Physical geography (2)
- Géographie physique ; Mer d'Oman ; Océan ; Océan Indien ; Paléo-océanographie ; Quaternaire marin ; Remontée d'eau ; Upwelling (1)
- Géographie physique ; Océan Indien ; Océanographie ; Paléo-océanographie ; Pléistocène supérieur ; Quaternaire marin (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)
- Surface circulation of the Indian Ocean during the last glacial maximum, approximately 18,000 yr B. P. (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.
- Géographie physique ; Mer d'Oman ; Océan ; Océan Indien ; Paléo-océanographie ; Quaternaire marin ; Remontée d'eau ; Upwelling
- ... 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
- and subtropical during the winter. In general, the low latitudes underwent little temperature change. The western Arabian Sea was warmer which implies less upwelling and a weaker Southwest Monsoon. On the average, the Indian Ocean was 1.9C cooler in February