咨询与建议

看过本文的还看了

相关文献

该作者的其他文献

文献详情 >Influence of atmospheric circu... 收藏

Influence of atmospheric circulation on precipitation in Altai Mountains

Influence of atmospheric circulation on precipitation in Altai Mountains

作     者:MALYGINA Natalia PAPINA Tatiana KONONOVA Nina BARLYAEVA Tatiana 

作者机构:Institute for Water and Environmental ProblemsSiberian Branch of the Russian Academy of SciencesBarnaul 656038Russia Institute of GeographyRussian Academy of SciencesMoscow 117312Russia Laboratoire d'Astrophysique de Marseille UMR 7326CNRS-INSUMarseille13388France 

出 版 物:《Journal of Mountain Science》 (山地科学学报(英文))

年 卷 期:2017年第14卷第1期

页      面:46-59页

核心收录:

学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学] 

基  金:supported by RFBR according to the research project No.16-35-00188 mol_a project“Climatic and ecological changes in Siberia by the data on glacio-chemical,diatomic and sporepollen analysis of ice-cores”(No.0383-2014-0005) 

主  题:Altai Mountains Precipitation Atmospheric circulation 

摘      要:We analyzed the changes in precipitation regime in the Altai Mountains for 1959-2014 and estimate the influence of atmospheric circulations on these changes. Our study showed that during last 56 years the changes in the precipitation regime had a positive trend for the warm seasons(April-October),but weakly positive or negative trends for the cold seasons(November-March). It was found that these changes correspond to the decreasing contribution of Northern meridional and Stationary anticyclone(Nm-Sa) and Northern meridional and East zonal(Nm-Ez) circulation groups and to the increasing contribution of West zonal and Southern meridional(Wz-Sm) circulation groups,accordingly to the Dzerdzeevskii classification. In addition,it was found that the variation of precipitation has a step change point in 1980. For the warm seasons,the precipitation change at this point is associated with the reduced influence of West zonal(Wz),Northern meridional and Stationary anticyclone(Nm-Sa) and Northern meridional and Southern meridional(Nm-Sm) circulation groups. For the cold seasons,a substantialincrease of Wz-Sm and a decrease of Nm-Sa,Nm-Ez circulation groups are responsible for the precipitation change in the two time periods(1959-1980 and 1981-2014).

读者评论 与其他读者分享你的观点

用户名:未登录
我的评分