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Prediction of permafrost distribution on the Qinghai-Tibet Plateau in the next 50 and 100 years

查看全文 作  者:NAN Zhuotong LI Shuxun CHENG [1]Guodong 高影响力作者 机构地区:[1]State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China高影响力机构 出  处:《Science China Earth Sciences》索引2005年第48卷第6期,共8页高影响力期刊 基  金:the Knowledge Innovation Project of Chinese Academy of Sciences(CAS)(Grant No.KZCX1-SW-04);the Knowledge Innovation Project of CAREERI,CAS(Grant No.CACX200009); the Project of Ministry of Science and Technology of China(Grant No.G1998040812). 摘  要:Intergovernmental Panel on Climate Change (IPCC) in 2001 reported that the Earth air temperature would rise by 1.4-5.8℃ and 2.5℃ on average by the year 2100. China re-gional climate model results also showed that the air temperature on the Qinghai-Tibet Plateau (QTP) would increase by 2.2-2.6℃ in the next 50 years. A numerical permafrost model was developed to predict the changes of permafrost distribution on the QTP over the next 50 and 100 years under the two climatic warming scenarios, i.e. 0.02℃/a, the lower value of IPCC’s estima-tion, and 0.052℃/a, the higher value predicted by Qin et al. Simulation results show that ( i ) in the case of 0.02℃/a air-temperature rise, permafrost area on the QTP will shrink about 8.8% in the next 50 years, and high temperature permafrost with mean annual ground temperature (MAGT) higher than ?0.11℃ may turn into seasonal frozen soils. In the next 100 years, perma-frost with MAGT higher than ?0.5℃ will disappear and the permafrost area will shrink up to 13.4%. (ii) In the case of 0.052℃/a air-temperature rise, permafrost area on the QTP will reduce about 13.5% after 50 years. More remarkable degradation will take place after 100 years, and permafrost area will reduce about 46%. Permafrost with MAGT higher than ?2℃ will turn into seasonal frozen soils and even unfrozen soils. 关 键 词:PERMAFROST distribution, SCENARIO prediction, the Qinghai-Tibet Plateau (QTP), numerical methods, Geo-graphical Information System (GIS).
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