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Evapotranspiration and humidity variations in response to land cover conversions in the Three Gorges Reservoir Region

机译:三峡库区的蒸散量和湿度变化对土地覆盖变化的响应

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摘要

A new land cover classification system was established for the Three Gorges Reservoir Region (TGRR) after considering the continuity of inundation and the natural characteristics of land cover.The potential evapotranspiration (PET) was predicted using a modified Penman-Monteith (P-M) model.The region's ratio of precipitation to evapotranspiration was calculated as the humidity index (HI).The data obtained was used to analyze climatic responses to land cover conversions from the perspectives of evapotranspiration and humidity variations.The results show that,from 1997 to 2009,the average annual PET increased in the early years and decreased later.In terns of overall spatial distribution,a significant reciprocal relationship appeared between annual PET and annual HI.In 1997,the annual PET was higher in the lower reaches than in the upper reaches of the TGRR,but the areas with high PET shifted substantially westward by 2003.The annum PET continued to increase in 2006,but the areas with high PET shrank by 2009.In contrast,the annum HI showed varying degrees of localized spatial variability.Over the three periods,the dominant forms of land cover conversions occurred from evergreen cover to seasonal green cover,from seasonal green cover to evergreen cover,and from seasonal green cover to seasonally inundated areas,respectively.These accounted for 48.0%,38.4%,and 23.8% of the total areas of converted land covers in the three periods,respectively.During the period between 1997 and 2003,the main forms of land cover conversions resulted in both positive and negative growths in the average annum PET,while all of them pushed down the average annual HI.From 2003 to 2006,the reservoir region experienced neither a decrease in the annum PET nor an increase in the annum HI.The period between 2006 and 2009 saw a consistent downward trend in the annum PET and a consistent upward trend in the annual HI.
机译:考虑到洪水泛滥的连续性和土地覆盖的自然特征,为三峡库区(TGRR)建立了新的土地覆盖分类系统,并使用改进的Penman-Monteith(PM)模型预测了潜在的蒸散量(PET)。计算该地区的降水量与蒸散量之比作为湿度指数(HI),所得数据用于从蒸散量和湿度变化的角度分析对土地覆盖转换的气候响应。结果表明,1997年至2009年,年平均PET在早年增加而后下降。在总体空间分布方面,年PET与年HI之间存在显着的相互关系。1997年,年PET在下游地区高于在上游地区。 TGRR,但高PET区域到2003年基本向西移动。2006年PET继续增长,但高PET区域gh PET在2009年之前萎缩。相反,年HI表现出不同程度的局部空间变异性。在这三个时期中,主要的土地覆被转化形式是从常绿覆盖到季节性绿盖,从季节性绿色覆盖到常绿覆盖,以及从季节性绿化覆盖到季节性淹没区域。这三个时期分别占转换后土地覆盖总面积的48.0%,38.4%和23.8%。在1997年至2003年期间,土地覆被的转换导致平均每年PET的正负增长,而所有这些均使平均每年HI下降。从2003年到2006年,水库地区年PET既不减少也不增加HI从2006年到2009年,PET年均呈下降趋势,而年度HI呈持续上升趋势。

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  • 来源
    《山地科学学报(英文版)》 |2018年第3期|590-605|共16页
  • 作者

    DENG Hua; SHAO Jing-an;

  • 作者单位

    Chongqing Youth Vocational & Technical College, Chongqing 400712, China;

    College of Geography and Tourism, Chongqing Normal University, Chongqing 401331, China;

    Key Laboratory of Surface Process and Environment Remote Sensing, in the Three Gorges Reservoir Area, Chongqing 401331, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
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