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Comparison of suitable drought indices for climate change impacts assessment over Australia towards resource management

机译:适用于澳大利亚气候变化影响评估的干旱指数与资源管理的比较

摘要

Droughts have significant environmental and socio-economic impacts in Australia. This emphasizes Australia’s vulnerability to climate variability and limitations of adaptive capacity. Two drought indices are compared forudtheir potential utility in resource management. The Rainfall Deciles-based Drought Index is a measure of rainfall deficiency while the Soil-Moisture Deciles-based Drought Index is a measure of soil-moisture deficiency attributed to rainfall and potential evaporation. Both indices were used to assess future drought events over Australia under global warming attributed to low and high greenhouse gas emission scenarios (SRES B1 and A1F1 respectively) for 30-year periods centred on 2030 and 2070. Projected consequential changes in rainfall and potential evaporation were based on results from the CCCma1 and Mk2 climate models, developed by the Canadian Climate Center and the Australian Commonwealth Scientific and Industrial Research Organisation (CSIRO) respectively. A general increase in drought frequency associated with global warming was demonstrated by both indices for both climate models, except for the western part of Australia. Increasesudin the frequency of soil-moisture-based droughts are greater than increases in meteorological drought frequency. By 2030, soil-moisture-based drought frequency increases 20–40% over most of Australia with respect to 1975–2004 and up to 80% over the Indian Ocean and southeast coast catchments by 2070. Such increases in drought frequency would haveudmajor implications for natural resource management, water security planning, water demand management strategies, anduddrought relief payments.
机译:干旱对澳大利亚的环境和社会经济产生重大影响。这强调了澳大利亚在气候变化方面的脆弱性和适应能力的局限性。比较了两个干旱指数在资源管理中的潜在用途。基于降雨十分位数的干旱指数是对降雨量不足的一种度量,而基于土壤水分十分位数的干旱指数是归因于降雨和潜在蒸发的土壤水分不足的度量。这两个指数均用于评估在全球变暖的情况下澳大利亚未来的干旱事件,这归因于温室气体排放情景的高低变化(分别为SRES B1和A1F1),持续了30年(以2030年和2070年为中心)。预计降雨和潜在蒸发的相应变化为基于分别由加拿大气候中心和澳大利亚联邦科学与工业研究组织(CSIRO)开发的CCCma1和Mk2气候模型的结果。除澳大利亚西部以外,这两个气候模型的两个指数均表明与全球变暖有关的干旱频率总体增加。基于土壤水分的干旱频率的增加大于气象干旱频率的增加。到1975年至2004年,到2030年,澳大利亚大部分地区基于土壤水分的干旱频率将增加20-40%,到2070年,印度洋和东南沿海流域的干旱频率将增加80%。这种干旱频率的增加将对自然资源管理,水安全计划,水需求管理策略和干旱补偿的影响。

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