Peak Runoff in the North Caucasus: Recent Trends in Magnitude, Variation and Timing


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

This paper presents the first thorough generalization of the recent change in annual peak runoff magnitude, variation, and timing in the North Caucasus. The patterns of the observed changes in the characteristics of peak runoff in the late XX–early XXI century are rather complicated, but show consistent structures over the territory. The main possible climatic drivers of the revealed changes in the tendencies are discussed, as well as the role of the observed change in the peak runoff in the context of flood danger in the region. The main peak runoff characteristics are re-evaluated for the first time for the whole region of the North Caucasus since the Volume of USSR Surface Water Resources series on this region issued in 1973.

作者简介

E. Rets

Water Problems Institute, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: retska@mail.ru
俄罗斯联邦, Moscow, 119333

I. Durmanov

Water Problems Institute, Russian Academy of Sciences; Faculty of Geography, Moscow State University

Email: retska@mail.ru
俄罗斯联邦, Moscow, 119333; Moscow, 119991

M. Kireeva

Faculty of Geography, Moscow State University

Email: retska@mail.ru
俄罗斯联邦, Moscow, 119991

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2019