江源冻土区水循环研究进展
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摘要
在气候变化背景下,江源冻土区水循环和生态系统发生改变,引发的水文、环境、工程问题受到广泛关注。本文从国内外江源冻土区水循环特征、水文模拟的相关研究、气候变化对江源冻土区产生的影响三个方面展开论述。总结了江源冻土区水循环特点,模拟了关键之处以及气候变化带来的利害,最后提出了江源冻土区的研究趋势和对发展方向的展望。
Under the background of climate change, the hydrological, environmental and engineering problems caused by the changes of water cycle and ecological system in the river headwater permafrost region have attracted wide attention. In this paper, the characteristics of water cycle, the related research of hydrological simulation, and the impact of climate change on the river headwater frozen soil area are discussed. The characteristics of water cycle in river headwater permafrost region, the key points of simulation and the benefits and disadvantages brought by climate change are summarized. Finally, the research trend and development direction of river headwater permafrost region are put forward.
Under the background of climate change, the hydrological, environmental and engineering problems caused by the changes of water cycle and ecological system in the river headwater permafrost region have attracted wide attention. In this paper, the characteristics of water cycle, the related research of hydrological simulation, and the impact of climate change on the river headwater frozen soil area are discussed. The characteristics of water cycle in river headwater permafrost region, the key points of simulation and the benefits and disadvantages brought by climate change are summarized. Finally, the research trend and development direction of river headwater permafrost region are put forward.
引文
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[11] 张雪婷,李雪梅,高培,等.基于不同方法的中国天山山区降水形态分离研究[J].冰川冻土,2017,39(2):235-244.
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[16] 康尔泗,施雅风,杨大庆,等.乌鲁木齐河山区流域径流形成的实验研究[J].第四纪研究,1997,17(2):139-146.
[17] 叶柏生,杨大庆,丁永建,等.中国降水观误差分析及其修正[J].地理学报,2007,62(1):3-13.
[18] 何晓波,叶柏生,丁永建.青藏高原唐古拉山区降水观测误差修正分析[J].水科学进展,2009,20(3):403-408.
[19] 舒守娟,王元,李艳.西藏高原地形扰动对其降水分布影响的研究[J].水科学进展,2006,17(5):585-591.
[20] 宋璐璐,尹云鹤,吴绍洪.蒸散发测定方法研究进展[J].地理科学进展,2012, 31(9):1186-1195.
[21] McCabe M F,Wood E F. Scale influences on the remote estimation of evapotranspiration using multiple satellite sensors[J].Remote Sensing of Environment,2006,105(4):271-285.
[22] Ma X, Yasunari T, Ohata T, et al. Hydrological regime analysis of the Selenge River basin, Mongolia[J]. Hydrological Processes,2003,17(14):2929-2945.
[23] 张寅生,蒲健辰,太田岳史.青藏高原中部地面蒸发量观测计算与特征分析[J].冰川冻土,1994,16(2):166-172.
[24] Zhang Y, Ohata T, Kadota T. Land-surface hydrological processes in the permafrost region of the eastern Tibetan Plateau [J].Journal of Hydrology, 2003, 283: 41-56.
[25] 张海红.长江源及其周边地区蒸发量特征及变化趋势研究[J].水文,2004, 24(5):41-44.
[26] 裴超重,钱开铸,吕京京,等.长江源区蒸散量变化规律及其影响因素[J].现代地质,2010,24(2):362-368.
[27] 杨广云,阴法章,刘晓凤,等.寒冷地区冻土水文特性与产流机制研究[J].水利水电技术,2007,38(1):39-42.
[28] 陈仁升,康尔泗,吉喜斌,等.黑河源头高山草甸带冻土及水文过程初步研究[J].冰川冻土,2007,29(3):387-396.
[29] 王慧.天山北坡融雪期季节性冻土下渗机制研究以军塘湖流域为例[D].乌鲁木齐:新疆大学,2013.
[30] 王一博,高泽永.青藏高原多年冻土区热融湖塘对土壤物理特性及入渗过程的影响[J].中国科学地球科学,2014,44(10):2285-2293.
[31] 程艳涛.冻土高寒草甸草地土壤水分入渗过程及影响因素的试验研究[D].兰州:兰州大学,2008:39-44.
[32] 延耀兴,郑秀清.季节性冻融条件下草地入渗特性的试验研究[J].水土保持学报, 2007,21(5):34-37.
[33] Mamoru Ishikawa, Natsagdorj Sharkhuu, Yinsheng Zhang,et al. Ground thermal and moisture conditions at the Southern boundary of discontinuous permafrost, mongolia[J]. Permafrost and Periglac. Process, 2005, 16(2):209-216.
[34] 周石硚,中尾正义,桥本重将,等.水在雪中下渗的数学模拟[J].水利学报,2001,32(1):6-10.
[35] Litong Zhao, Gray D M. Estimating snowmelt infiltration into frozen soils. Hydrological Processes.1999, 15(12):1827-1842.
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