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Monsoonal variations and climate change during the late Holocene derived from tree rings and glacier fluctuations
项目编号http://gepris.dfg.de/gepris/projekt/180323682
Professor Dr. FrankLehmkuhl (Applicant); Professor Dr. AchimBräuning (Applicant)
项目主持机构Rheinisch-Westfälische Technische Hochschule Aachen;Friedrich-Alexander-Universität Erlangen-Nürnberg
开始日期2010
结束日期2015
英文摘要We will apply a multiproxy analysis approach including geomorphological and dendrochronological data to reconstruct glacier and climate history in southeastern Tibet during the late Holocene (last 1500 years). Monsoonal temperate glaciers in southeastern Tibet react fast and sensitive on climate changes. Geomorphological and sedimentological data from glacier sediments shall be combined to reconstruct glacier fluctuations and equilibrium-line altitude variations. Newly collected tree-ring material from glacier-near sites will help to date Little Ice Age glacier advances and to reconstruct different seasonal climatic elements by using different wood parameters like ring width, maximum latewood density and the content of stable δ13C and δ18O isotopes. Glacier and tree-ring data will be used to reconstruct former moisture and temperature conditions during important late Holocene-climate episodes like the Little Ice Age and the Medieval Warm Period. The combination of temperature-sensitive and moisture-sensitive palaeoclimate proxies will enable us to disentangle the role of temperature and humidity changes for the behaviour of monsoonal temperate glaciers on the southeastern Tibetan plateau.
学科分类0802 - 地质学;08 - 地球科学
资助机构DE-DFG
项目类型Priority Programmes
URLhttp://gepris.dfg.de/gepris/projekt/180323682
国家DE
语种英语
文献类型项目
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/71923
推荐引用方式
GB/T 7714
Professor Dr. FrankLehmkuhl ,Professor Dr. AchimBräuning .Monsoonal variations and climate change during the late Holocene derived from tree rings and glacier fluctuations.2010.
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