Vegetation-based climate reconstruction for the Tibetan Plateau: integrating vegetation modelling and pollen data reanalyses
基于植被的青藏高原气候重建:整合植被建模和花粉数据再分析
基本信息
- 批准号:180325382
- 负责人:
- 金额:--
- 依托单位:
- 依托单位国家:德国
- 项目类别:Priority Programmes
- 财政年份:2010
- 资助国家:德国
- 起止时间:2009-12-31 至 2017-12-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
The Asian monsoonal system controls the vegetation over a large area of Eurasia. The environmental properties over the Tibetan Plateau in turn affect the monsoon system. Within the proposed projected we will study the millennial-scale climate changes and human-climatevegetation interactions on the Tibetan Plateau during the glacial times to Holocene. It is a key task of our project to set up a Tibetan Plateau regional vegetation model that will be used for inverse vegetation modelling of palaeoclimate based on pollen-inferred vegetation changes. Results will be compared to climate estimates that were quantified by the application of traditional pollen-climate transfer functions. Obtained climatic pattern in space and time will contribute to our understanding of causes and consequences of past climate change on the Tibetan Plateau. Furthermore, we will investigate how severe the linkage chain “climate-vegetationpollen” is disturbed by human impact and will considered that in the numerical climate inference approaches. Findings from this project will significantly contribute to the understanding of the “Late Cenozoic climate evolution and environmental response” and the “Phase of human impact and Global Change”, which are two major points of the priority program “TiP”.
亚洲季风系统控制着欧亚大陆大片地区的植被。青藏高原的环境特征反过来又会影响季风系统。在拟议的预测范围内,我们将研究青藏高原冰期至全新世期间千年尺度的气候变化和人类-气候变化的相互作用。建立青藏高原区域植被模型是本项目的一项关键任务,该模型将用于基于花粉推断植被变化的古气候的植被反演模拟。结果将与通过应用传统的花粉-气候转移函数进行量化的气候估计进行比较。所获得的气候时空格局将有助于我们理解青藏高原过去气候变化的原因和后果。此外,我们将调查“气候-植物-花粉”连锁链受到人类影响的严重程度,并将在数值气候推断方法中考虑这一点。该项目的研究结果将有助于理解“晚新生代气候演化和环境响应”和“人类影响和全球变化阶段”,这是优先计划“TIP”的两个要点。
项目成果
期刊论文数量(2)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Moisture-advection feedback supports strong early-to-mid Holocene monsoon climate on the eastern Tibetan Plateau as inferred from a pollen-based reconstruction
- DOI:10.1016/j.palaeo.2014.02.022
- 发表时间:2014-05
- 期刊:
- 影响因子:0
- 作者:U. Herzschuh;J. Borkowski;J. Schewe;S. Mischke;F. Tian
- 通讯作者:U. Herzschuh;J. Borkowski;J. Schewe;S. Mischke;F. Tian
Simulating Biome Distribution on the Tibetan Plateau Using a Modified Global Vegetation Model
使用修正的全球植被模型模拟青藏高原的生物群落分布
- DOI:10.1657/1938-4246-43.3.429
- 发表时间:2011
- 期刊:
- 影响因子:0
- 作者:Herzschuh
- 通讯作者:Herzschuh
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Professorin Dr. Ulrike Herzschuh其他文献
Professorin Dr. Ulrike Herzschuh的其他文献
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{{ truncateString('Professorin Dr. Ulrike Herzschuh', 18)}}的其他基金
Boreal forest bi-stability around Lake El’gygytgyn (NE Russia) during interglacial of the last 2.15 Million years
过去 215 万年间冰期期间 Elâgygytgyn 湖(俄罗斯东北部)周围的北方森林双稳定性
- 批准号:
398626025 - 财政年份:2018
- 资助金额:
-- - 项目类别:
Infrastructure Priority Programmes
Pliocene Arctic vegetation and its feedbacks with climate: combining Lake El´gygytgyn pollen data and vegetation modelling
上新世北极植被及其对气候的反馈:结合埃尔吉吉特金湖花粉数据和植被建模
- 批准号:
194256127 - 财政年份:2011
- 资助金额:
-- - 项目类别:
Infrastructure Priority Programmes
Polygons in tundra wetlands: state and dynamics under climate variability in Polar Regions (POLYGON)
苔原湿地中的多边形:极地地区气候变化下的状态和动态(POLYGON)
- 批准号:
164232461 - 财政年份:2010
- 资助金额:
-- - 项目类别:
Research Grants
Quaternary climate change in the most continental part of Central Asia
中亚大部分大陆地区的第四纪气候变化
- 批准号:
188649816 - 财政年份:2010
- 资助金额:
-- - 项目类别:
Research Grants
Vegetation changes during the last 400 years in norhern Yakutia, Arctic Russia: Evidence from pollen analysis and vegetation modeling
俄罗斯北极地区雅库特北部过去 400 年的植被变化:来自花粉分析和植被建模的证据
- 批准号:
71883563 - 财政年份:2008
- 资助金额:
-- - 项目类别:
Research Grants
Effective moisture changes and landscape development on the north-eastern Tibetan Plateau during the last 50 ka inferred from Lake Donggi Cona lake sediments
从东吉错那湖沉积物推断青藏高原东北部近50ka有效水分变化和景观发育
- 批准号:
46138072 - 财政年份:2007
- 资助金额:
-- - 项目类别:
Research Grants
Late Glacial-Early Holocene climate evolution on the Tibetan Plateau: a trigger or a response to Northern Hemisphere climate change?
青藏高原晚冰期-早全新世气候演化:北半球气候变化的触发因素还是响应?
- 批准号:
16318205 - 财政年份:2005
- 资助金额:
-- - 项目类别:
Research Grants
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MoLiCarb - 自末次冰期以来苔藓和地衣对永久冻土碳动态的影响
- 批准号:
514539694 - 财政年份:
- 资助金额:
-- - 项目类别:
Research Grants
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