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On the spatio-temporal analysis of hydrological droughts from global hydrological models

机译:基于全球水文模型的水文干旱时空分析

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摘要

The recent concerns for world-wide extreme events related to climate change have motivated the development of large scale models that simulate the global water cycle. In this context, analysis of hydrological extremes is important and requires the adaptation of identification methods used for river basin models. This paper presents two methodologies that extend the tools to analyze spatio-temporal drought development and characteristics using large scale gridded time series of hydrometeorological data. The methodologies are classified as non-contiguous and contiguous drought area analyses (i.e. NCDA and CDA). The NCDA presents time series of percentages of areas in drought at the global scale and for pre-defined regions of known hydroclimatology. The CDA is introduced as a complementary method that generates information on the spatial coherence of drought events at the global scale. Spatial drought events are found through CDA by clustering patterns (contiguous areas). In this study the global hydrological model WaterGAP was used to illustrate the methodology development. Global gridded time series of subsurface runoff (resolution 0.5°) simulated with the WaterGAP model from land points were used. The NCDA and CDA were developed to identify drought events in runoff. The percentages of area in drought calculated with both methods show complementary information on the spatial and temporal events for the last decades of the 20th century. The NCDA provides relevant information on the average number of droughts, duration and severity (deficit volume) for pre-defined regions (globe, 2 selected hydroclimatic regions). Additionally, the CDA provides information on the number of spatially linked areas in drought, maximum spatial event and their geographic location on the globe. Some results capture the overall spatio-temporal drought extremes over the last decades of the 20th century. Events like the El Ni?o Southern Oscillation (ENSO) in South America and the pan-European drought in 1976 appeared clearly in both analyses. The methodologies introduced provide an important basis for the global characterization of droughts, model inter-comparison of drought identified from global hydrological models and spatial event analyses.
机译:最近对与气候变化有关的世界范围极端事件的关注促使了模拟全球水循环的大规模模型的发展。在这种情况下,对水文极端事件进行分析很重要,需要对用于流域模型的识别方法进行调整。本文介绍了两种方法,这些方法扩展了使用大规模水文气象数据网格化时间序列分析时空干旱发展和特征的工具。这些方法分类为非连续和连续干旱地区分析(即NCDA和CDA)。 NCDA提供了全球范围内和已知水文气候学的预定义区域中干旱地区百分比的时间序列。引入CDA作为一种补充方法,可以在全球范围内生成有关干旱事件的空间一致性的信息。通过CDA通过聚类模式(连续区域)发现了空间干旱事件。在这项研究中,全球水文模型WaterGAP被用来说明方法的发展。使用了WaterGAP模型从陆地点模拟的地下径流的全球网格化时间序列(分辨率为0.5°)。开发了NCDA和CDA以识别径流中的干旱事件。两种方法计算出的干旱面积百分比显示出有关20世纪最后几十年的时空事件的补充信息。 NCDA提供了有关预定义区域(地球,2个选定的水文气候区域)的平均干旱次数,持续时间和严重程度(赤字量)的相关信息。此外,CDA还提供有关干旱中空间链接区域的数量,最大空间事件及其在全球地理位置的信息。一些结果记录了20世纪最后几十年的总体时空干旱极端情况。两项分析都清楚地表明了诸如南美的厄尔尼诺南方涛动(ENSO)和1976年泛欧干旱等事件。所介绍的方法为全球干旱特征,从全球水文模型和空间事件分析中确定的干旱模型间比较提供了重要基础。

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