Environmental change modelling for Central and High Asia: Pleistocene, present and future scenarios

Bohner, J. & Lehmkuhl, F. 2005 (May): Environmental change modelling for Central and High Asia: Pleistocene, present and future scenarios. Boreas, Vol. 34, pp. 220–231. Oslo. ISSN 0300–9483. A regional modelling concept was developed for late Quaternary climate reconstructions and future climate impact assessments. Based on estimates of different climate parameters covering the entire Central and High Asia in a grid-cell spacing of 1 km2, climatic determinants of the recent spatial distribution of climate-sensitive environments (glacial and periglacial environments, forest) were explored. Simple climatic threshold functions were established, defining critical climate values for modelling the spatial extension of environments considered. Using palaeogeomorphological indicators as a basis, late Quaternary climatic conditions were modelled in a Last Glacial Maximum (LGM) scenario consistent with palaeogeomorphological and palaeoclimatological data. The results enabled a validation of LGM palaeoclimate simulations performed by the ECHAM GCM. To assess the magnitude of possible future climatic impacts on the spatial distribution of glaciers, permafrost and potential forest stands, two GCM-based IPCC-SRES climate change scenarios (IPCC special report on emission scenarios) for the time period 2070–2099 were considered. Assuming future climates to be perturbed for long enough to affect the environments, a distinct loss of glaciated areas and permafrost must be expected.

[1]  L. Owen,et al.  The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion , 1998, Journal of the Geological Society.

[2]  Jürgen Böhner,et al.  Geomorphologische Formungs- und Prozessregionen in Zentralasien , 2003 .

[3]  F. Lehmkuhl,et al.  Timings and causes of glacial advances across the PEP-II transect (East-Asia to Antarctica) during the last glaciation cycle , 2004 .

[4]  S. Malyshev,et al.  Climate change in the 21st Century - Interim Characterizations based on the new IPCC Emissions Scenarios , 2000 .

[5]  Hugh M. French,et al.  Climate controls and high‐altitude permafrost, qinghai‐xizang (tibet) Plateau, China , 1994 .

[6]  M. Domrös,et al.  The climate of China , 1987 .

[7]  Jin-qi Fang Lake evolution during the past 30,000 years in China, and its implications for environmental change , 1991, Quaternary Research.

[8]  F. Lehmkuhl,et al.  Geomorphologische Untersuchungen zum Klima des Holozäns und Jungpleistozäns Osttibets , 1995 .

[9]  M. Kuhle Reconstruction of the 2.4 million km2 late Pleistocene ice sheet on the Tibetan Plateau and its impact on the global climate , 1998 .

[10]  Karl Tilman Rost Paleoclimatic field studies in and along the Qinling Shan (Central China) , 1994 .

[11]  M. Caffee,et al.  A note on the extent of glaciation throughout the Himalaya during the global Last Glacial Maximum , 2002 .

[12]  Hucai Zhang,et al.  Lake Evolution in the Tengger Desert, Northwestern China, during the Last 40,000 Years , 1995, Quaternary Research.

[13]  A. Zhisheng,et al.  Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the Northeastern Tibetan Plateau , 2001 .

[14]  Douglas I. Benn,et al.  Mass balance and equilibrium-line altitudes of glaciers in high-mountain environments , 2000 .

[15]  Zheng Benxing,et al.  On the problem of Quaternary glaciations, and the extent and patterns of Pleistocene ice cover in the Qinghai-Xizang (Tibet) Plateau , 1998 .

[16]  F. Lehmkuhl,et al.  Geomorphological investigations and luminescence dating in the southern part of the Khangay and the Valley of the Gobi Lakes (Central Mongolia) , 2001 .

[17]  F. Lehmkuhl,et al.  Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia) , 2000 .

[18]  M. Sharma,et al.  Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, northern India: defining the timing of Late Quaternary glaciation , 2001 .

[19]  Jürgen Böhner,et al.  Climate pattern, snow- and timberlines in the Altai Mountains, Central Asia , 2003 .

[20]  Karl Tilman Rost Pleistocene paleoenvironmental changes in the high mountain ranges of central China and adjacent regions , 2000 .

[21]  M. Caffee,et al.  Timing of multiple late Quaternary glaciations in the Hunza Valley, Karakoram Mountains, northern Pakistan: Defined by cosmogenic radionuclide dating of moraines , 2002 .

[22]  Shi Yafeng,et al.  Quaternary glaciation of tibet: The geological evidence , 1991 .

[23]  F. Lehmkuhl,et al.  Late Quaternary aeolian sedimentation in central and south-eastern Tibet , 2000 .

[24]  A. Lang,et al.  Late Quaternary glacier advances, lake level fluctuations and aeolian sedimentation in Southern Tibet , 2002 .

[25]  F. Lehmkuhl Extent and spatial distribution of Pleistocene glaciations in eastern Tibet , 1998 .