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Rain-use efficiency and NDVI-based assessment of karst ecosystem degradation or recovery: a case study in Guangxi, China

机译:喀斯特生态系统退化或恢复的雨水利用效率和基于NDVI的评估:以中国广西为例

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摘要

Interannual variation in productivity may be caused by ecosystem structure degradation or recovery or by interannual precipitation fluctuation. A new method for ecosystem assessment was proposed based on the combination of rain-use efficiency (RUE) and normalized difference vegetation index (NDVI). This study aimed to alleviate the effect of precipitation fluctuation on ecosystem productivity. The trend of annual precipitation, annual maximum NDVI, and annual RUE of the study area was first analyzed. The relationship between RUE and precipitation at both temporal and spatial scales was then clarified. Finally, the relationship between the trends of RUE and NDVI was recognized. According to this trend, ecosystem degradation or recovery determined, and the mask of precipitation fluctuation were removed. Results showed that annual RUE varied significantly in space from 1999 to 2008. Annual precipitation displayed a decreasing trend, whereas the annual maximum NDVI presented an increasing trend in most karst ecosystems. RUE presented a remarkable declining trend with annual precipitation at both the temporal and spatial scales (P < 0.001). At a significant level of 0.2, most karst ecosystems at 16 weather stations were recovering from 1999 to 2008. Ecosystems of Baise, Hechi, and Mengshan stations were in pseudo recovery, whereas those of Laibin and Duan stations were in pseudo degradation because of precipitation fluctuation. At a significant level of 0.05, most karst ecosystems showed non-significant change except four stations were in pseudo recovery. The method of combining RUE and NDVI for ecosystem assessment may remove the mask of precipitation fluctuations and thus improve single NDVI-based method for vegetation analysis.
机译:生产力的年际变化可能是由生态系统结构退化或恢复或年际降水波动引起的。提出了一种综合利用雨水利用效率和归一化植被指数的生态系统评价方法。这项研究旨在减轻降水波动对生态系统生产力的影响。首先分析了研究区的年降水量,年最大NDVI和年RUE的趋势。然后阐明了时空尺度上RUE与降水之间的关系。最后,人们认识到RUE和NDVI趋势之间的关系。根据这一趋势,确定了生态系统退化或恢复,并消除了降水波动的掩盖。结果表明,从1999年到2008年,年RUE在空间上变化很大。在大多数喀斯特生态系统中,年降水量呈下降趋势,而年最大NDVI呈上升趋势。在时间和空间尺度上,RUE呈现出显着的下降趋势,年降水量(P <0.001)。在0.2的显着水平上,1999年至2008年,16个气象站的大多数喀斯特生态系统都在恢复。百色,河池和蒙山站的生态系统处于假恢复状态,而来宾和段段的生态系统由于降水波动而处于假退化状态。 。在0.05的显着水平上,除了四个站点处于假恢复状态外,大多数喀斯特生态系统都没有显着变化。结合RUE和NDVI进行生态系统评估的方法可以消除降水波动的掩盖,从而改进基于NDVI的单一植被分析方法。

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