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Effects of climate change on lake area and vegetation cover over the past 55 years in Northeast Inner Mongolia grassland, China

机译:中国蒙古草原东北地区湖区气候变化对湖区和植被覆盖的影响

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摘要

Previous studies indicate that vegetation and lakes in arid and semi-arid regions are closely related to climate change. However, the responses of vegetation and lakes to climate-related variables have rarely been contrastively studied. The Hulun Lake (HLL) and its surrounding grasslands in Northeast Inner Mongolia of China comprise a semi-arid region that has experienced intense climate change over the last several decades. This study aims to understand the key factors that control the variations in the lake area and vegetation cover over the last five decades in the HLL region, as well as contrastively investigate the different responses of the lake area and vegetation cover to climate-related variables. Analysis results indicate that the variations with increasing change rates in the HLL area were mainly controlled by precipitation fluctuation. Moreover, an increase or decrease in the air temperature and relative humidity could affect the response time of the HLL area to the change in precipitation. The Normalized Difference Vegetation Index (NDVI) variations from 1990 to 1999 around the HLL region were mainly controlled by the intense local grazing rather than climatic restrictions. The fluctuation in NDVI after 1999 reflects the response of the vegetation cover to climatic change. The correlation analysis shows that the variations in the HLL area were closely related to the multi-year tendency of precipitation amount and to the Standardized Precipitation Evapotranspiration Index (SPEI) with a long timescale. However, NDVI is sensitive to changes in short-term precipitation amount, such as seasonal precipitation, and in SPEI with a monthly timescale. The soil moisture at shallow depths ( 0.1 m) was the key root-zone soil moisture that could influence NDVI, whereas soil moisture at depths of 0.4 to 1.0 m and the HLL area were closely related and had similar responses to climatic change.
机译:以前的研究表明,干旱和半干旱地区的植被和湖泊与气候变化密切相关。然而,植被和湖泊与气候相关变量的反应很少研究。中国东北蒙古的Hulun湖(HLL)及其周围的草原包括一个半干旱地区,在过去几十年中经历了强烈的气候变化。本研究旨在了解在HLL地区的过去五十年中控制湖区和植被覆盖物的关键因素,以及对湖区和植被覆盖的不同响应与气候相关的变量。分析结果表明,随着沉淀波动的影响,HLL面积中变化率的变化主要是由降水波动控制的。此外,空气温度和相对湿度的增加或减少可能影响HLL区域对降水变化的响应时间。 1990年至1999年周围HLL区域的归一化差异植被指数(NDVI)变化主要由激烈的当地放牧而不是气候限制来控制。 1999年后NDVI的波动反映了植被覆盖对气候变化的响应。相关分析表明,HLL面积的变化与沉淀量的多年趋势密切相关,并具有长时间的标准化沉淀蒸发散热指数(SPEI)。然而,NDVI对短期降水量的变化敏感,例如季节性降水,以及每月时间尺度的Spei。浅层深度(<0.1米)的土壤水分是影响NDVI的关键根区土壤水分,而在0.4至1.0米的水分下,HLL区域的土壤水分密切相关,对气候变化具有相似的反应。

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  • 来源
    《Theoretical and applied climatology》 |2019年第2期|13-25|共13页
  • 作者单位

    Minist Water Resources People S Republ China Inst Water Resource Pastoral Area Hohhot 010020 Inner Mongolia Peoples R China;

    Minist Water Resources People S Republ China Inst Water Resource Pastoral Area Hohhot 010020 Inner Mongolia Peoples R China;

    Minist Water Resources People S Republ China Inst Water Resource Pastoral Area Hohhot 010020 Inner Mongolia Peoples R China;

    Minist Water Resources People S Republ China Inst Water Resource Pastoral Area Hohhot 010020 Inner Mongolia Peoples R China;

    Minist Water Resources People S Republ China Inst Water Resource Pastoral Area Hohhot 010020 Inner Mongolia Peoples R China;

    Minist Water Resources People S Republ China Inst Water Resource Pastoral Area Hohhot 010020 Inner Mongolia Peoples R China;

    Minist Water Resources People S Republ China Inst Water Resource Pastoral Area Hohhot 010020 Inner Mongolia Peoples R China;

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