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Characteristics of drought propagation in South Korea: relationship between meteorological, agricultural, and hydrological droughts

机译:韩国干旱繁殖特征:气象,农业和水文干旱关系

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摘要

To investigate the propagation of meteorological droughts to agricultural and hydrological droughts, the relationship between droughts was analyzed using observed precipitation and agricultural reservoir and dam storage levels with SPI from 1998 to 2015 in South Korea. For the relationship between different types of droughts, we find that the occurrence of meteorological droughts after concentrated precipitation in the wet season (from June to September) tends not to lead to agricultural or hydrological droughts. A lack of precipitation from April to September, when large volumes of irrigation water are consumed, triggers both meteorological and agricultural droughts. In the case of hydrological droughts propagated from meteorological droughts, precipitation deficits in the dry season (between October and March) caused decrease in dam storage levels only. The occurrence of all different types of droughts is associated with extreme meteorological droughts, which are mainly caused by precipitation deficits in the wet season or prolonged rainfall shortages; in these cases, meteorological droughts led to agricultural and hydrological droughts. An analysis of the seasonal characteristics of storage level changes that in the wet season, agricultural reservoir storage levels are more dependent on precipitation deficits than dam storage levels. On other hand, when precipitation deficits were recorded in the dry season, agricultural reservoir storage levels went up, but dam storage levels dropped. The propagation of meteorological droughts to agricultural and hydrological droughts depends not only on drought severity but also on the drought timing. These findings may contribute to establishing a comprehensive drought monitoring system.
机译:为了探讨气象干旱对农业和水文干旱的繁殖,使用1998年至2015年在韩国的观察到的降水和农业储层和水坝储存水平分析干旱之间的关系。对于不同类型的干旱之间的关系,我们发现湿季浓缩沉淀(从6月至9月开始)后气象干旱发生的发生往往不会导致农业或水文干旱。 4月至9月缺乏降水,当消耗大量的灌溉水,触发气象和农业干旱。在流动繁殖的水文干旱的情况下,干燥季节(10月和3月)中的降水缺陷仅导致坝储存水平降低。所有不同类型的干旱发生的发生与极端气象干旱有关,主要是潮湿季节的降水缺陷或长期降雨短缺引起;在这些情况下,气象干旱导致农业和水文干旱。对湿季的储存水平变化的季节性特征分析,农业储层储存水平更依赖于坝体储存水平的降水缺陷。另一方面,当旱季记录降水缺陷时,农业储层储存水平上升,但坝储存水平掉落。气象干旱对农业和水文干旱的繁殖不仅取决于干旱严重程度,而且取决于干旱时间。这些调查结果可能有助于建立综合干旱监测系统。

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