dc.contributor.author | Niitsuma, N. | |
dc.contributor.author | Naidu, P.D. | |
dc.date.accessioned | 2009-01-07T11:01:37Z | |
dc.date.available | 2009-01-07T11:01:37Z | |
dc.date.issued | 2001 | |
dc.identifier.citation | Encyclopedia of ocean sciences, Ed. by: Steele, J.H. 1841-1849p. | |
dc.identifier.uri | http://drs.nio.org/drs/handle/2264/1607 | |
dc.description.abstract | The evolution of the Asian monsoon started at around 9.5 Ma, in response to the uplift of the Himalayas. The monsoonal intensity reached its maximum at around 5 Ma, and from that time the associated easterly trade winds caused intense upwelling in the equatorial Pacific. The chronological sequence of monsoonal events, and the strength of trade winds and equatorial upwelling suggests that the Asian monsoons were an important control on global climate and oceanic productivity | |
dc.language.iso | en | |
dc.publisher | Academic Press, San Diego, USA | |
dc.rights | Copyright [2001]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository. | |
dc.subject | palaeoceanography | |
dc.subject | palaeoclimate | |
dc.subject | monsoons | |
dc.subject | heat budget | |
dc.title | Monsoons, history of | |
dc.type | Book Chapter | |