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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Spatio-temporal variability of droughts in Bolivia: 1955-2012
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Spatio-temporal variability of droughts in Bolivia: 1955-2012

机译:玻利维亚干旱的时空变化:1955-2012年

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In this study, the spatio-temporal variability and trends of droughts across Bolivia between 1955 and 2012 were investigated using two climate drought indices: the Standardized Precipitation Index (SPI), which is based on precipitation data, and the Standardized Precipitation Evapotranspiration Index (SPEI), which is based on the difference between the precipitation and the reference evapotranspiration (ETo). We found that the average drought conditions across the country showed a temporal behaviour mainly characterized by decadal variations. The spatial pattern of drought evolution showed marked differences between the Amazonian region and the Bolivian Altiplano. Both regions showed different drought periods, a lower frequency of drought variability in the Amazon region and trends towards drier conditions in the Altiplano, mainly due to a higher atmospheric water demand as a consequence of increased ETo. We also showed that inclusion of ETo, obtained from maximum and minimum temperature records, increased the spatial heterogeneity of the drought evolution in relation to the evolution observed when only precipitation droughts were considered. The SPEI, the calculation of which includes precipitation and ETo, indicated intensification in drought severity in the last years analysed relative to the pattern found when precipitation droughts alone were considered, and also indicated an increase in the magnitude and duration of drought events. The potential for increasing drought conditions under various climate change scenarios is discussed.
机译:在这项研究中,使用两个气候干旱指数:基于降水数据的标准化降水指数(SPI)和标准化降水蒸散指数(SPEI),调查了1955年至2012年期间玻利维亚全国各地的干旱时空变化和趋势。 ),其基于降水量与参考蒸散量(ETo)之间的差异。我们发现,全国平均干旱条件表现出一种时间性行为,主要表现为年代际变化。干旱演变的空间格局显示亚马逊地区和玻利维亚高原之间存在明显差异。这两个地区都表现出不同的干旱时期,亚马逊地区干旱变化的频率较低,而高原地区干旱条件趋于发展,这主要是由于ETo增加导致大气水需求增加。我们还表明,从最高和最低温度记录中获得的ETo,与仅考虑降水干旱时观察到的演化有关,增加了干旱演化的空间异质性。 SPEI(包括降水和ETo在内)的计算表明,相对于仅考虑降水干旱时发现的模式,最近几年干旱严重性加剧,并且表明干旱事件的程度和持续时间有所增加。讨论了在各种气候变化情景下增加干旱条件的潜力。

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