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Transition Characteristics of the Dry-Wet Regime and Vegetation Dynamic Responses over the Yarlung Zangbo River Basin, Southeast Qinghai-Tibet Plateau

机译:青藏高原东南部雅鲁藏布江流域干湿状况过渡特征及植被动态响应

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The dry-wet transition is of great importance for vegetation dynamics, however the response mechanism of vegetation variations is still unclear due to the complicated effects of climate change. As a critical ecologically fragile area located in the southeast Qinghai-Tibet Plateau, the Yarlung Zangbo River (YZR) basin, which was selected as the typical area in this study, is significantly sensitive and vulnerable to climate change. The standardized precipitation evapotranspiration index (SPEI) and the normalized difference vegetation index (NDVI) based on the GLDAS-NOAH products and the GIMMS-NDVI remote sensing data from 1982 to 2015 were employed to investigate the spatio-temporal characteristics of the dry-wet regime and the vegetation dynamic responses. The results showed that: (1) The spatio-temporal patterns of the precipitation and temperature simulated by the GLDAS-NOAH fitted well with those of the in-situ data. (2) During the period of 1982–2015, the whole YZR basin exhibited an overall wetting tendency. However, the spatio-temporal characteristics of the dry-wet regime exhibited a reversal phenomenon before and after 2000, which was jointly identified by the SPEI and runoff. That is, the YZR basin showed a wetting trend before 2000 and a drying trend after 2000; the arid areas in the basin showed a tendency of wetting whereas the humid areas exhibited a trend of drying. (3) The region where NDVI was positively correlated with SPEI accounted for approximately 70% of the basin area, demonstrating a similar spatio-temporal reversal phenomenon of the vegetation around 2000, indicating that the dry-wet condition is of great importance for the evolution of vegetation. (4) The SPEI showed a much more significant positive correlation with the soil water content which accounted for more than 95% of the basin area, implying that the soil water content was an important indicator to identify the dry-wet transition in the YZR basin.
机译:干湿过渡对于植被动力学非常重要,但是由于气候变化的复杂影响,植被变化的响应机制仍不清楚。作为位于青藏高原东南部的一个关键的生态脆弱地区,雅鲁藏布江流域(YZR)被选为本研究的典型区域,对气候变化非常敏感并易受其影响。利用1982-2015年GLDAS-NOAH产物和GIMMS-NDVI遥感数据的标准化降水蒸散指数(SPEI)和归一化植被指数(NDVI)研究了干湿地的时空特征状况和植被动态响应。结果表明:(1)GLDAS-NOAH模拟的降水和温度的时空格局与原位数据吻合良好。 (2)在1982–2015年期间,整个YZR盆地呈现出总体的润湿趋势。然而,干湿政权的时空特征在2000年前后表现出逆转现象,这是由SPEI和径流共同确定的。也就是说,YZR盆地在2000年之前呈现出湿润趋势,而在2000年之后呈现出干燥趋势。流域的干旱地区表现出润湿的趋势,而潮湿地区表现出干燥的趋势。 (3)NDVI与SPEI呈正相关的区域约占流域面积的70%,这表明2000年前后植被存在类似的时空反转现象,这表明干湿条件对演化至关重要。植被。 (4)SPEI与土壤含水量呈显着正相关,占流域面积的95%以上,这表明土壤含水量是识别YZR盆地干湿过渡的重要指标。 。

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