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Anomaly Variation of Vegetation and Its Influencing Factors in Mainland China During ENSO Period

机译:enso期间中国大陆植被的异常变化及其影响因素

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摘要

Considering the noncore region influenced by El Ni00F1;o-Southern Oscillation (ENSO) events, China is hardly investigated in terms of the vegetation variation during the ENSO period.Therefore, this study focused on increasing knowledge of vegetation growth and variation during the ENSO period.The novelty of this paper is introduced the moving window correlation analysis method to determine the thresholds of vegetation response to sea surface temperature anomaly (SSTa) and southern oscillation index (SOI) and analyze the main reasons for such variations.China was divided into seven areas based on different weather conditions, and the variations in vegetation growth in various areas during the ENSO period were analyzed. The response of vegetation to ENSO events in China was analyzed from the perspectives of precipitable water vapor (PWV), temperature, and precipitation, thereby revealing the interplay of multi-factors on vegetation growth.The main conclusions include (1) a positive vegetation response to El Ni00F1;o exists all over China with thresholds of SSTa >= 1.8700B0;C and SOI <= -3.27hPa, whereas a negative response of vegetation variation to La Ni00F1;a exists with thresholds of SSTa <= -1.0500B0;C and SOI >= 1.7hPa; (2) the correlations (p 003C; 0.05) of PWV to normalized difference vegetation index (NDVI) (PWV-NDVI), temperature-NDVI, and precipitation-NDVI reached 0.84, 0.86, and 0.68, respectively, and PWV, temperature, and precipitation were negatively/positively abnormal during El Ni00F1;o/La Ni00F1;a periods; (3) in coastal areas of Southeast China, correlations between NDVI and PWV/temperature/ precipitation are poor and the opposite anomalies of PWV/temperature/ precipitation existed when compared to other areas of China.
机译:考虑到受EL NI00F1影响的非奇偶地区; O-Southern振荡(ENSO)事件,在ENSO期间的植被变化方面几乎没有调查。因此,这项研究旨在越来越多地了解enso期间的植被生长和变化的知识。本文的新颖性引入了移动窗口相关分析方法,以确定海面温度异常(SSTA)和南方振荡指数(SOI)的植被响应阈值,并分析了这种变化的主要原因。中国分为七个分析了基于不同天气条件的地区,并分析了ENSO期间各个区域植被生长的变化。从可降水水蒸气(PWV),温度和降水的角度分析了中国植物对ENSO事件的影响,从而揭示了多因素对植被生长的影响。主要结论包括(1)阳性植被反应对于El Ni00f1; o存在于中国的阈值> = 1.8700b0; c和soi <= -3.27hpa,而植被变化对La Ni00f1的负响应; A存在于SSTA <= -1.0500b0的阈值; C和SOI> = 1.7HPa; (2)PWV对归一化差异植被指数(NDVI)(PWV-NDVI),温度-NDVI和沉淀-NDVI的相关性(P 003c; 0.05)分别达到0.84,0.86和0.68,PWV,温度,在EL Ni00f1期间,沉淀在eL; o / la ni00f1期间产生负面/肯定异常;一段时间; (3)在中国东南沿海地区,与中国其他地区相比,NDVI和PWV /温度/降水量之间的相关性差,PWV /温度/降水的相反异常存在。

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