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首页> 外文期刊>Geography, Environment, Sustainability >Estimation Of The Impact Of Climatic And Anthropogenic Factors On The Formation Of The Extreme Low-Flow Period In The Don River Basin During 2007-2016
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Estimation Of The Impact Of Climatic And Anthropogenic Factors On The Formation Of The Extreme Low-Flow Period In The Don River Basin During 2007-2016

机译:估计气候和人为因素对2007 - 2016年唐河流域极端低流量期的影响

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The Don River is the largest river in the southwestern part of European Russia and the second largest river system in European Russia. The Don River basin is one of the most water deficient regions in Russia and the long term average water usage in the basin amounts to 45%.The period 2007-2016 was the longest long-term low-flow period observed, with an estimated total water resources deficit of 40.4 km3 over 8 years. The main reason for this deficit were anomalously warm winters (2-4 degrees over average) with a low degree of soil frost penetration. This resulted in low spring flood volume (37% of the average) due to heavy seepage losses combined with thin snow cover.A similar low-flow situation was observed in 2014, when the drought caused great damage to ecosystem of Tsimlianskoye water reservoir and the River Don. Most of the fish breeding grounds had dried up by May 2014. This caused the number of round fish whitebait to drop 5-10 times below the 2002-2014 average. Inland shipping and hydropower industry also sustained losses of 42 million euro (according to interview from State Shipping company) due to low water level.This study shows that the main reasons for the 2007-2016 extreme hydrological drought are exceptional hydro-climatic conditions and anthropogenic transformations in the watershed, such as urbanisation growth and afforestation. The analysis shows that the main cause in water deficit is associated with the left tributaries of Don – Khoper and Medveditsa, while the flow in Upper Don remained more or less normal. The results can be interpreted as a “warning sign” to reduce water consumption in these sub-basins to avoid similar drought situations in future.
机译:唐河是欧洲俄罗斯西南部最大的河流,也是欧洲俄罗斯第二大河流系统。唐河流域是俄罗斯最多的水缺乏地区之一,盆地的长期平均水资料量为45%。2007 - 2016年期间是观察到的最长的长期低流量,估计总数8岁以上的水资源赤字40.4平方公里。这种赤字的主要原因是具有低于土壤霜冻渗透程度的低常温暖的冬季(2-4度)。这导致春季洪水量低(平均值的37%)由于薄雪覆盖。2014年在2014年观察到类似的低流量情况,当时干旱导致了尖莲科尤水库生态系统造成了巨大损害河唐。大多数鱼类养殖场在2014年5月已经干涸。这导致圆形鱼类白宝数量下降5-10倍以下的平均水平。由于水平低,内陆航运和水电产业也持续了4200万欧元(根据国家航运公司的访谈)。本研究表明,2007 - 2016年极端水文干旱的主要原因是卓越的水力 - 气候条件和人为流域的转型,如城市化的增长和造林。分析表明,水赤字的主要原因与Don - Khoper和Medveditsa的左支流相关,而上部的流量仍然或多或少正常。结果可以解释为“警告标志”,以减少这些子盆地中的用水量,以避免将来类似的干旱情况。

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