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DOI10.1016/j.palaeo.2019.03.038
High-elevation shrub-ring δ 18 O on the northern slope of the central Himalayas records summer (May–July) temperatures
Huang R.; Zhu H.; Liang E.; Grießinger J.; Dawadi B.; Bräuning A.
发表日期2019
ISSN0031-0182
起始页码230
结束页码239
卷号524
英文摘要The potential of shrub-ring oxygen isotopes (SRO) as a paleoclimatic proxy is not well demonstrated. In this study we explored the climate signals embedded in an SRO chronology from Saga, on the northern slope of the central Himalayas by correlation analysis with climate variables and comparison with tree-ring and/or ice-core δ 18 O records. The Saga SRO had significant and positive correlations with May–July temperatures in both local (r = 0.43) and moisture source areas (r = 0.49) during the period 1955–2015 (CE), while no significant correlations were found with hydroclimatic variables. It is also in good agreement with two tree-ring δ 18 O series from the southern slope of the central Himalayas, the source of moisture to the site. The temperature signals are further verified by an ice core δ 18 O record from the Tanggula Mountains on the central Tibetan Plateau. However, it shows little similarity with the nearest Himalayan ice core δ 18 O record from Dasuopu, demonstrating temperature signals of different seasons. This study suggests that SRO could be used as an acceptable climate proxy, like tree-ring and ice-core δ 18 O, to broaden the spatial extent of the paleoclimatic records network. However, we should be cautious when combining different proxies with climate signals of different seasons in paleoclimate studies. © 2019 Elsevier B.V.
英文关键词Central Himalayas; Climatic proxy; Paleoclimatology; Shrub-ring oxygen isotope; Southern Tibetan Plateau
语种英语
scopus关键词climate signal; ice core; oxygen isotope; paleoclimate; proxy climate record; shrub; slope; summer; temperature; tree ring; China; Dasuopu Glacier; Himalayas; Japan; Kyushu; Qinghai-Xizang Plateau; Saga; Tanggula Mountains; Xizang
来源期刊Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/150969
作者单位Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, China; University of Chinese Academy of Sciences, Beijing, 10049, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, China; Institute of Geography, Friedrich-Alexander-University of Erlangen-Nuremberg, Wetterkreuz 15, Erlangen, 91058, Germany; Central Department of Hydrology and Meteorology, Tribhuvan University Kirtipur, Kathmandu, Nepal
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Huang R.,Zhu H.,Liang E.,等. High-elevation shrub-ring δ 18 O on the northern slope of the central Himalayas records summer (May–July) temperatures[J],2019,524.
APA Huang R.,Zhu H.,Liang E.,Grießinger J.,Dawadi B.,&Bräuning A..(2019).High-elevation shrub-ring δ 18 O on the northern slope of the central Himalayas records summer (May–July) temperatures.Palaeogeography, Palaeoclimatology, Palaeoecology,524.
MLA Huang R.,et al."High-elevation shrub-ring δ 18 O on the northern slope of the central Himalayas records summer (May–July) temperatures".Palaeogeography, Palaeoclimatology, Palaeoecology 524(2019).
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