The Relationship of the δ18 O in the Guliya Shallow Ice Core during the Prevailing Summer Monsoons with Global SST and Height at the 500 hPa over the Northern Hemisphere

doi:10.7522/j.issn.1000-0240.2000.0057

The Relationship of the δ¹⁸ O in the Guliya Shallow Ice Core during the Prevailing Summer Monsoons with Global SST and Height at the 500 hPa over the Northern Hemisphere

ZHANG Xin-ping, YAO Tan-dong, NAKAWO Masayoshi, JIAO Ke-qin

Journal of Glaciology and Geocryology ›› 2000, Vol. 22 ›› Issue (4) : 289-297.

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Journal of Glaciology and Geocryology ›› 2000, Vol. 22 ›› Issue (4) : 289-297. DOI: 10.7522/j.issn.1000-0240.2000.0057

The Relationship of the δ¹⁸ O in the Guliya Shallow Ice Core during the Prevailing Summer Monsoons with Global SST and Height at the 500 hPa over the Northern Hemisphere

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{{article.zuoZheEn_L}}. {{article.title_en}}[J]. {{journal.qiKanMingCheng_EN}}, 2000, 22(4): 289-297 https://doi.org/10.7522/j.issn.1000-0240.2000.0057

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Received	Revised	Published
2000-05-08	2000-07-31	2000-11-25
Online
2012-04-26

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