Temporal changes in seasonal precipitation over the Sahara Desert from 1979 to 2016  

作　　者：Sindikubwabo Celestin Feng Qi RuoLin Li WenJu Cheng Jian Ma Habiyakare Telesphore Nzabarinda Vincent 

机构地区：[1]Key Laboratory of Eco-hydrology of Inland River Basin,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences(CAS),Lanzhou,Gansu 730000,China [2]University of Chinese Academy of Sciences,Beijing 100049,China [3]Qilian Mountains Eco environment Research Center,Lanzhou,Gansu 730000,China [4]Academy of Water Resources Conservation Forests in Qilian Mountains,Zhangye,Gansu 734000,China

出　　处：《Research in Cold and Arid Regions》2021年第3期220-233,共14页寒旱区科学（英文版）

基　　金：funded by the National Key R&D Program of China(No.2017YFC0404305);National Natural Science Foundation of China(No.41801015,No.41771252);the Foundation for Excellent Young Scholars of Northwest Institute of Eco-Environment and Resources NIEER Chinese Academy of Sciences,CAS(No.51Y851D61);the Major Program of the Natural Science Foundation of Gansu province,China(No.18JR4RA002);Science and Technology Program of Gansu Province,China(18JR2RA026);the Chinese Academy of Sciences-The World Academy of Sciences(CAS-TWAS)President's Fellowship programme。

摘　　要：Rainfall variability dominates livelihoods in all countries of Saharan Africa.To better understand the processes involved in Sahara precipitation changes,we used the Global Precipitation Climatology Center(GPCC)dataset to examine dry and wet seasonal trends in the Sahara region from 1979 to 2016.We also used the European Centre for Medium-Range Weather Forecasts(ECMWF)to evaluate the general atmospheric circulation associated with seasonal change of Sahara precipitation.The Mann-Kendall test and Theil sens'slope estimator methods were adopted to test and estimate the significance and weight of precipitation trend,respectively.The results revealed that Sahara precipitation has increased significantly.The seasonal evaluation shows a positive trend of 0.42 mm/decade and 1.43 mm/decade in JAS(June,August,and September)seasons for the northern and southern Saharan Desert,respectively.Moreover,the JFMA(January,February,March,and April)period shows a negative trend but not statistically significant.An examination of the general circulation and moisture transport changes suggested an increase of rainfall in southern Sahara.The wet period is also driven by northward penetration of moisture originating from the Sahel region,African Easterly Jet(AEJ),and weakening in the upper tropospheric zonal wind.Summer rainfall has also been likely associated with positive anomalies of sea surface temperature(SST)in the North Tropical Atlantic(NTA)and the Mediterranean Sea.

关 键 词：SAHARA PRECIPITATION variability ARID AFRICA climate 

分 类 号：P426.614[天文地球—大气科学及气象学]