The role of snow in the formation of water flow in Suceava hydrographic basin

A. Porcuţan
{"title":"The role of snow in the formation of water flow in Suceava hydrographic basin","authors":"A. Porcuţan","doi":"10.24193/RCJ2018_21","DOIUrl":null,"url":null,"abstract":"The role of snow in the formation of water flow in Suceava hydrographic basin. The hydrographic basin of the Suceava River is situated in the North-East sector of the Northern Carpathian Group from the Romanian Carpathians, more precisely, and much of the Suceava Plateau, a subunit of the Moldavian Plateau. The floods produced on the rivers in this basin were directly influenced by fallen liquid precipitations. The study is based on the processing and interpretation of climatic data about the snow layer recorded throughout the period. Also, data on the floods in the Suceava River Basin were recorded at eight hydrometer stations, three of which are located on the main course and five are on the main tributaries. The analysed period for the snow layer and its influence on the water flow formation in the study basin during the period 1961-2015, focusing on the variation in snow thickness and length over the analysed period. Finally, the influence of the snow layer on the drainage of the water and the drainage of the Suceava river basin during the analysed period with effect on large waters, floods and small waters was presented.","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"49 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Risks and Catastrophes Journal","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.24193/RCJ2018_21","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

The role of snow in the formation of water flow in Suceava hydrographic basin. The hydrographic basin of the Suceava River is situated in the North-East sector of the Northern Carpathian Group from the Romanian Carpathians, more precisely, and much of the Suceava Plateau, a subunit of the Moldavian Plateau. The floods produced on the rivers in this basin were directly influenced by fallen liquid precipitations. The study is based on the processing and interpretation of climatic data about the snow layer recorded throughout the period. Also, data on the floods in the Suceava River Basin were recorded at eight hydrometer stations, three of which are located on the main course and five are on the main tributaries. The analysed period for the snow layer and its influence on the water flow formation in the study basin during the period 1961-2015, focusing on the variation in snow thickness and length over the analysed period. Finally, the influence of the snow layer on the drainage of the water and the drainage of the Suceava river basin during the analysed period with effect on large waters, floods and small waters was presented.
雪在Suceava水文盆地水流形成中的作用
雪在Suceava水文盆地水流形成中的作用。苏切瓦河的水文盆地位于罗马尼亚喀尔巴阡山脉的北喀尔巴阡山脉的东北部分,更准确地说,位于摩尔多瓦高原的一个亚单元苏切瓦高原的大部分地区。该流域河流上产生的洪水直接受到降水的影响。这项研究是基于对整个时期记录的雪层气候数据的处理和解释。此外,8个比重计站记录了Suceava河流域洪水的数据,其中3个位于主要河道,5个位于主要支流。分析了1961-2015年研究流域雪层的形成周期及其对水流形成的影响,重点分析了分析期间积雪厚度和长度的变化。最后,分析了雪层在分析期间对水的影响以及对Suceava河流域的排水,对大水、洪水和小水的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信