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Can human-induced land degradation be distinguished from the effects of rainfall variability? A case study in South Africa

机译:是否可以将人为造成的土地退化与降雨多变性的影响区分开来?南非的案例研究

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Advanced Very High Resolution Radiometer (AVHRR), Normalized Difference Vegetation Index data (NDVI, 1 km~2, 1985-2003) and modeled net primary production (NPP, 8 km~2, 1981-2000) data were used to estimate vegetation production in South Africa (SA). The linear relationships of Log_eRainfall with NPP and ΣNDVI were calculated for every pixel. Vegetation production generally had a strong relationship with rainfall over most of SA. Therefore, human-induced land degradation can only be detected if its impacts on vegetation production can be distinguished from the effects of rainfall. Two methods were tested (ⅰ) Rain-Use Efficiency (RUE = NPP/Rainfall or ΣNDVI/ Rainfall) and (ⅱ) Residual Trends (RESTREND), i.e. negative trends in the differences between the observed ΣNDVI and the ΣNDVI predicted by the rainfall. Degraded areas mapped by the National Land Cover in north-eastern SA had reduced RUE; however, annual RUE had a very strong negative correlation with rainfall and varied greatly between years. Therefore, RUE was not a reliable indicator of degradation. The RESTREND method showed promising results at a national scale and in the Limpopo Province, where negative trends were often associated with degraded areas in communal lands. Both positive and negative residual trends can, however, result from natural ecological processes, e.g. the carryover effects of rainfall in previous years. Thus, the RESTREND method can only identify potential problem areas at a regional scale, while the cause of negative trends has to be determined by local investigations.
机译:先进的超高分辨率辐射计(AVHRR),归一化植被指数数据(NDVI,1 km〜2,1985-2003)和模型化的净初级生产(NPP,8 km〜2,1981-2000)数据用于估算植被产量在南非(SA)。计算每个像素的Log_eRainfall与NPP和ΣNDVI的线性关系。在南半球大部分地区,植被生产通常与降雨有很强的关系。因此,只有将人类对土地的退化对植被生产的影响与降雨的影响区分开来,才能发现。测试了两种方法(ⅰ)雨水利用效率(RUE = NPP /雨量或ΣNDVI/雨量)和(ⅱ)残留趋势(RESTREND),即观察到的ΣNDVI和由降雨预测的ΣNDVI之间差异的负趋势。南非东北部国家土地覆被划定的退化地区降低了RUE;但是,年RUE与降雨有很强的负相关关系,并且在几年之间变化很大。因此,RUE并不是降解的可靠指标。 RESTREND方法在全国范围内和林波波省(Limpopo Province)均显示出令人鼓舞的结果,在林波波省,消极趋势通常与公共土地退化地区有关。但是,正向和负向残余趋势都可能来自自然生态过程,例如自然过程。前几年降雨的结转效应。因此,RESTREND方法只能识别区域范围内的潜在问题区域,而负面趋势的原因则必须通过本地调查来确定。

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