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Volumn 273, Issue 5276, 1996, Pages 771-773

Mongolian tree rings and 20th-century warming

Author keywords

[No Author keywords available]

Indexed keywords

ARCTIC; ARTICLE; CHRONOLOGY; CLIMATE; ENVIRONMENTAL TEMPERATURE; FOREST; GREENHOUSE EFFECT; MONGOLIA; PINE; PRIORITY JOURNAL; SOLAR RADIATION; TREE;

EID: 0029660054     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.273.5276.771     Document Type: Article
Times cited : (160)

References (37)
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    • note
    • Six tree-ring chronologies from Mongolia were placed in the International Tree-Ring Data Bank in February 1996 by K. V. Chistyakov of St. Petersburg Univ. in Russia. They are all larch and are from lower elevations than the Tarvagatay Pass series. The chronology from the highest elevation (2380 m) is somewhat similar to our series, with an increase in indices in the mid- to late 1700s, a decrease in the early 1800s, and an increase since the mid-1800s. Larch, a deciduous conifer, tends to have more of a warm-season-only response than evergreens [see, for example, (24)].
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    • note
    • All sampling of living trees was done by coring, leaving only a small wound. The trees will continue to grow and record environmental changes.
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    • note
    • We thank D, Baatar, R. Mijiddorj, S. Erdembileg, Dondov, D. Lawrence, D. Stahle, the American Museum of Natural History, and C. Goulden. Supported by NSF grant ATM94-06372. This is Lamont-Doherty Earth Observatory contribution number 5522.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.