Teleconnections between the Subtropical Monsoons and High-Latitude Climates During the Last Deglaciation

Details Teleconnections between the Subtropical Monsoons and High-Latitude Climates During the Last Deglaciation Teleconnections between the Subtropical Monsoons and High-Latitude Climates During the Last Deglaciation

Apr 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996sci...272..526s&link_type=abstract

Science, Volume 272, Issue 5261, pp. 526-529

Physics

46

Scientific paper

The major deglacial intensification of the southwest monsoon occurred at 11,450 ± 150 calendar years before present, synchronous with a major climate transition as recorded in Greenland ice. An earlier event of monsoon intensification at 16,000 ± 150 calendar years before present occurred at the end of Heinrich layer 1 in the Atlantic and parallels the initial rise in global atmospheric methane concentrations and the first abrupt climate changes in the Antarctic; thus, the evolution of the monsoonal and high-latitude climates show teleconnections but hemispheric asymmetries. Superimposed on abrupt events, the monsoonal climate shows high-frequency variability of 1785-, 1450-, and 1150-year oscillations, and abrupt climate change seems to occur when at least two of these oscillations are in phase.

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