中国不同植被区对极端气候的响应差异
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国家自然科学基金项目(42077436)


Differential analysis of vegetation response to extreme climate in different vegetation regions of China
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The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan)

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    摘要:

    分析不同区域植被对极端气候的响应对于加深对植被与气候之间关系的理解以及制定应对极端气候条件的措施尤为重要。基于2001-2020年气候数据和归一化植被指数(NDVI)数据,以植被区划为分析单元,分析中国8个植被区的NDVI和27个极端气候指数的时空变化趋势,探究各植被区植被NDVI对极端气候的响应特征与差异性。结果表明:(1)整个研究区及各植被区的平均NDVI年最大值呈显著增加趋势,其中,温带针叶、落叶阔叶混交林区增加趋势最明显,青藏高原高寒植被区增加趋势最弱。(2)极端高温指数多呈升高趋势。极端降水指数在研究区东部呈升高趋势,在西南部呈减少趋势。(3)在不同植被区对NDVI影响最大的极端气候指数不同,其中在寒温带针叶林区影响最大的指数为温暖时间持续指数(WSDI);在温带针叶、落叶阔叶混交林区和热带季风雨林、雨林区影响最大的指数为最高低温(TNx);在暖温带落叶阔叶林区和亚热带常绿阔叶林区为简单降水强度指数(SDII);在温带草原区为最高高温(TXx);在温带荒漠区为年总降水量(PRCPTOT);在青藏高原高寒植被区为结冰天数(ID)。

    Abstract:

    Under the background of climate warming, extreme climate poses a serious threat to vegetation. The response of vegetation to extreme climate is spatially heterogeneous, which is influenced by factors such as vegetation type and soil composition. China has complex topographic and climatic conditions, which make the vegetation types vary in its different regions. Analyzing the response patterns of vegetation to extreme climate in different regions is of particular importance to advance our understanding of the relationship between vegetation and climate and to develop measures to address extreme climate conditions. The main purpose of this study is to explore the spatiotemporal changes in normalized difference vegetation index (NDVI) and extreme climate, and analyze the effects of extreme climate on vegetation NDVI within various vegetation regions. Based on climatic data and NDVI data, the study firstly explored the spatiotemporal changes of NDVI and 27 extreme climate indicators across different vegetation regions in China from 2001 to 2020 by the Theil Sen Median slope estimation and Mann Kendall trend test methods. Then, the correlation analysis and random forest importance ranking method were used to analyze the relationship between different extreme climate indicators and the NDVI and further discuss the variations in vegetation response to extreme climate across different vegetation regions. The results indicated that:(1) the annual maximum value of NDVI (NDVImax) of the whole study area and various vegetation regions showed a significant increasing trend. Among them, the temperate coniferous and deciduous broad-leaved mixed forest area exhibited the strongest increasing trend, while the alpine vegetation area of Qinghai-Tibet Plateau showed the weakest increasing trend. (2) The extreme heat indicators increased significantly. Except for consecutive dry days (CDD), the extreme precipitation indicators showed an increasing trend in the eastern study area and a decreasing trend in the southwest. (3) The extreme climate indicators that had the greatest influence on NDVImax in different vegetation regions were different. In the cold temperate coniferous forest area, warm spell duration indicator (WSDI) had the greatest effect. In the temperate coniferous and deciduous broad-leaved mixed forest area and tropical monsoon rainforest and rainforest area, the maximum daily minimum temperature (TNx) had the greatest effect. In warm temperate deciduous broad-leaved forest area and subtropical evergreen broad-leaved forest area, simple daily intensity indicator (SDII) had the greatest effect. In temperate grassland area, maximum daily maximum temperature (TXx) had the greatest effect. In temperate desert area, annual precipitation total (PRCPTOT) had the greatest effect. In the alpine vegetation area of the Qinghai-Tibet Plateau, ice days (ID) had the greatest effect.

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吴欣宇,朱秀芳.中国不同植被区对极端气候的响应差异.生态学报,2023,43(24):10202~10215

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