Quaternary Internatio e o
sity sity ng 9 N; 65 a 1.75 km2 desiccated peat bog in the low hills of central Marine records of the last glacial from offshore Taiwan show that low-latitude sea-surface temperature is not as Farrera et al., 1999). On the other hand, a chronological timing of temperature changes from the Greenland...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.3037 http://ntur.lib.ntu.edu.tw/bitstream/246246/172507/1/16.pdf |
| Summary: | sity sity ng 9 N; 65 a 1.75 km2 desiccated peat bog in the low hills of central Marine records of the last glacial from offshore Taiwan show that low-latitude sea-surface temperature is not as Farrera et al., 1999). On the other hand, a chronological timing of temperature changes from the Greenland ice core GISP2 (Wang et al., 2001). This indicates that the East ARTICLE IN PRESSAsian monsoon is integral to millennial-scale changes in atmosphere/oceanic circulation patterns and is affected by orbitally induced insolation variations. Remarkable |
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