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Obser accep tertim Atlantic region during the last glaciation and into the Holocene. The primary evidence comes from mismatches between mean annual temperatures from Greenland ice cores in comparison with snowline changes in East Greenland, northern Europe, and oxygen-isotope ratios during the last...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.485.8982 http://www.bio.puc.cl/labs/clatorre/SemV/Denton_etal_2005_Role of seasonality.pdf |
Summary: | Obser accep tertim Atlantic region during the last glaciation and into the Holocene. The primary evidence comes from mismatches between mean annual temperatures from Greenland ice cores in comparison with snowline changes in East Greenland, northern Europe, and oxygen-isotope ratios during the last glaciation and into cores that reveal sea-surface temperatures (SSTs) (Bond show SST variations and shifts in the Atlantic Inter-et al., 2001), and the Hulu Cave in China (Wang et al., 2001), the Indian and East Asian monsoons featured abrupt shifts in summer intensity that seem to match |
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