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A comparative study of historical droughts over Texas, USA and Murray-Darling Basin, Australia: Factors influencing initialization and cessation

机译:美国德克萨斯州和澳大利亚墨累达令盆地历史干旱的比较研究:影响初始化和停止的因素

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Water availability and food security are tightly coupled on a global scale. The occurrence of drought puts this balance at risk due to reductions in dryland farming production and water allocations to irrigated agriculture. Improved understanding of drought initiation and cessation would therefore be beneficial for drought planning and management. The study objective was to determine factors affecting drought initiation and cessation over the past century in two climatologically similar regions that represent net agricultural exporters; south central U.S. (Texas) and southeast Australia (Murray Darling Basin, MDB). Drought indices included the Standardized Precipitation Index (SPI, 1900-2014) for meteorological drought, the Normalized Difference Vegetation Index (NDVI, 1981-2014) for agricultural drought, and the Streamflow Drought Index (SDI, 1930-2014) for hydrological drought. Results show that meteorological drought tends to develop gradually over a period of up to six months, with agricultural drought developing shortly thereafter (within one month) in both regions. Evidence of hydrological drought was observed within one month (Texas) and within four months (MDB) on average after meteorological drought was established. Further, droughts appear to cease more quickly than they initiate over Texas, whereas rates of drought initiation and cessation are similar over the MDB. Drought breaking rainfall in Texas is generally a result of a southward shift in the Polar Jet Stream or a low-pressure trough over central North America, whereas drought cessation in the MDB is typically associated with a monsoon trough or low-pressure system in the Tasman Sea/Great Australian Bight. Improved knowledge of the climate mechanisms controlling the onset and termination of drought periods should enhance drought forecasts and improve drought management practices, particularly in regions where water security is a primary objective. (C) 2016 Published by Elsevier B.V.
机译:水资源供应和粮食安全在全球范围内紧密结合。干旱的发生使这一平衡处于危险之中,原因是旱地农业生产减少和灌溉农业用水分配减少。因此,更好地了解干旱的发生和停止将有助于干旱的规划和管理。该研究的目的是确定代表农业净出口国的两个气候相似地区在过去一个世纪中影响干旱启动和停止的因素。美国中南部(德克萨斯州)和澳大利亚东南部(Murray达令盆地,MDB)。干旱指数包括气象干旱的标准降水指数(SPI,1900-2014),农业干旱的标准差植被指数(NDVI,1981-2014)和水文干旱的径流干旱指数(SDI,1930-2014)。结果表明,气象干旱往往在长达六个月的时间内逐渐发展,此后不久(两个月以内)两个地区都出现了农业干旱。建立气象干旱后,平均在一个月内(德克萨斯州)和四个月内(MDB)观测到水文干旱的证据。此外,干旱似乎比在得克萨斯州引发的干旱停止得更快,而在多边开发银行,干旱的发生和停止的速率相似。得克萨斯州的干旱打破降雨通常是由于极地急流向南移动或北美中部出现低压槽造成的,而MDB中的干旱停止通常与塔斯曼地区的季风槽或低压系统有关。海洋/澳大利亚湾。尤其是在以水安全为主要目标的地区,对控制干旱时期的开始和结束的气候机制的了解应会增强干旱预报并改善干旱管理做法。 (C)2016由Elsevier B.V.发布

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