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机构地区:[1]中国科学院寒区旱区环境与工程研究所冻土工程国家重点实验室
出 处:《冰川冻土》2001年第1期1-6,共6页Journal of Glaciology and Geocryology
基 金:中国科学院冰冻圈特别支持项目;中国科学院旱区寒区环境与工程研究所创新项目 !(CACX2 10 0 47)
摘 要:利用英国Hadley气候预测与研究中心GCM模型HADCM2预测的气温变化背景 ,分别提取青藏公路沿线地区在 2 0 0 9年、2 0 49年和 2 0 99年的气温参数 ,考虑年平均气温和年平均地温的关系及年平均地温与海拔、纬度的关系模型、多年冻土下界分布模型和地温带分带 ,建立青藏公路沿线多年冻土下界分布的响应模型和多年冻土地温带的响应模型 .研究结果表明 ,2 0 0 9年青藏公路沿线的冻土变化较小 ,多年冻土极稳定带、稳定带和基本稳定带仅发生微弱的变化 ,基本稳定过渡带和不稳定带变化较大 ,多年冻土逐渐退化 ;2 0 49年青藏公路沿线多年冻土各地温带变化较大 ,但仍以基本稳定过渡带和不稳定带变化最大 ,多年冻土发生较大范围的退化 ;2 0 99年后青藏公路沿线冻土发生了很大的变化 ,多年冻土发生大面积的退化 ,融区面积逐渐增大 ,多年冻土地温带也发生了较大的变化 ,其中多年冻土上带仅保留了稳定带 ,极稳定带全部消失 。GCM model HADCM2, which was developed in the Hadley Center for Climate Prediction and Research in Britain, was adopted for climate scenarios. Only air temperature scenarios in permafrost response model are used. In order to preserve the original air temperature forecast results in the HADCM2; the nearest-neighbor method was used to resample the air temperature for the years 2009, 2049 and 2099 into 0.5°×0.5°grids compatible with the DEM. The predication shows that the mean raising of air temperature will be 0 46 ℃ in 2009, 0 78 ℃ in 2049 and 2 53 ℃ in 2099 from 36° to 33 5° N, and 0 72 ℃ in 2009, 0 78 ℃ in 2049 and 2 68 ℃ in 2099 from 33 5° to 31° N. Altitude model, which was proposed for the permafrost distribution limit in Northern Hemisphere, is used to determine the permafrost distribution limit (Equation 1). Permafrost zone model, which is proposed by the multiple linear regression relationships among MGATs, altitude and latitude, is used to determine the permafrost zone distribution (Equation 2). The altitude model does not contain climate variables, such as air temperature. Thus, the relationship between predicted air temperature change Δ T of HADCM2 and permafrost lower limit uplifting Δ H is established as Equation 3. The relationship between the MAGTs and MAATs can be established as Equation 4. And assuming that rising air temperature would result in immediate permafrost warming. The rising MAATs at lower limit will result in changing MAGTs of permafrost zones. The response model of permafrost zone is proposed on the Equations (3) and (5): Under the support of GIS, the response model of permafrost zone and the DTM along the Qinghai-Tibetan Highway, the permafrost change of the highway are obtained under GCM climate scenario in 2009, 2049, and 2099. The results show that permafrost zone will greatly change after climate warming. Their area is expected to decrease and permafrost zone will be moving upward and degrading. In order to easily discussing permafrost zone c
分 类 号:P642.12[天文地球—工程地质学]
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