靳立亚, 任骊安, 冯瑞娟. 近16年白龙江流域植被NDVI对气候变化的响应[J]. 自然保护地,2023,3(2):44−52. DOI: 10.12335/2096-8981.2022072803
引用本文: 靳立亚, 任骊安, 冯瑞娟. 近16年白龙江流域植被NDVI对气候变化的响应[J]. 自然保护地,2023,3(2):44−52. DOI: 10.12335/2096-8981.2022072803
JIN Liya, REN Li’an, FENG Ruijuan. Response of Vegetation NDVI in Bailongjiang Basin to Climatic Changes During the Past Sixteen Years[J]. Natural Protected Areas, 2023, 3(2): 44−52. DOI: 10.12335/2096-8981.2022072803
Citation: JIN Liya, REN Li’an, FENG Ruijuan. Response of Vegetation NDVI in Bailongjiang Basin to Climatic Changes During the Past Sixteen Years[J]. Natural Protected Areas, 2023, 3(2): 44−52. DOI: 10.12335/2096-8981.2022072803

近16年白龙江流域植被NDVI对气候变化的响应

Response of Vegetation NDVI in Bailongjiang Basin to Climatic Changes During the Past Sixteen Years

  • 摘要: 白龙江流域的植被与近16年来气温、降水的变化存在着密切关系。其中在流域中下游区域(宕昌、舟曲、武都、文县)植被与降水呈显著正相关。不同季节气温和降水对植被的影响存在着明显差异,春季气温与植被的关系以正相关为主,其中显著正相关的像元占比为26.07%,主要位于流域中上游;夏季降水与生态植被的关系以正相关为主,其中显著正相关的像元占比为11.21%,主要位于流域中下游区域;秋季气温和降水与植被的关系类似,即在流域西部为负相关、流域东部为正相关,其中显著负相关的像元占比分别为7.13%(气温)和40.74%(降水)。生长季贯穿春季到初秋的时段,气温和降水与植被的关系呈显著正相关的像元占比分别为22.08%和28.65%。

     

    Abstract: There was a closely relationship between ecological vegetation and changes in temperature and precipitation during the past sixteen years in the Bailongjiang basin. There has been a significantly positive relationship between the vegetation index (NDVI) and the precipitation within the middle and down reaches of the Bailongjiang basin (Tanchang, Zhouqu, Wudu, Wenxian). The influence of temperature and precipitation in different seasons on vegetation showed significantly diverse. In spring, the relationship between temperature and vegetation was mainly positive, among which the significant positive correlation pixel proportion is 26.07%, mainly located in the middle and upper reaches of the watershed. In summer, there was a positive relationship between precipitation and NDVI, with significant pixels of more than 11.21%, located in the middle and lower reaches of the Bailongjiang basin. In autumn, the relationship between temperature and vegetation was similar to precipitation, which was negatively correlated in the west and positively correlated in the east, of which the significant negative correlation pixel proportion was 7.13% (temperature) and 40.74% (precipitation), respectively. During the growing season (from spring to early autumn), there has been a positive relationship between temperature and NDVI as well as precipitation and NDVI, with significant pixels more than 22.08% (temperature) and 28.65% (precipitation), respectively.

     

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