Climate changes impacts in the upper Paiva River: today and in the future

被引:0
作者
Sousa, Vitor [1 ]
Meireles, Ines [2 ]
Goncalves, Alexandre B. [1 ]
Falcao, Ana Paula [1 ]
机构
[1] Univ Lisbon, Dept Civil Engn Architecture & Georesources, Inst Super Tecn, CERIS, Av Rovisco Pais 1, P-1049001 Lisbon, Portugal
[2] Univ Aveiro, Civil Engn Dept, RISCO, Campus Univ Santiago, P-3810193 Aveiro, Portugal
关键词
Climate change; Drying; Upper Paiva River; Rainfall; Runoff; HYDROLOGICAL IMPACTS; PRECIPITATION EVENTS; PROJECTIONS; EUROPE; MODELS; TRENDS; UNCERTAINTY; PORTUGAL; PATTERNS; FLOW;
D O I
10.5004/dwt.2020.25856
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The Paiva River is a tributary of the Douro River in northern Portugal with a length of 110 km and a catchment area of 790 km(2). Nowadays, its upper section dries completely by the end of the dry season every year. The individuals living in communities along the river are consistent in identifying the beginning of this phenomenon by the end of the 1990 s or early 2000 s. In the present research, the potential causes for this are identified, evaluated, and discussed. The direct human consumption was possible to exclude due to the decrease of both population and water-intensive activities in the period of interest. Considering the information available, climate changes are identified as the main driver for the complete dry out of the upper section. Specifically, the differences in the precipitation distribution along the year were found to be statistically significant and the increase of the number of consecutive days without rain could be related to the depletion of the underground water. Considering rainfall pattern forecasts for 2050 based on various climate change scenarios and global circulation models, it is possible to conclude that the already poor environmental condition of the upper Paiva River section will degrade even further in the future.
引用
收藏
页码:343 / 357
页数:15
相关论文
共 77 条
[1]  
APA, 2010, 5 NAT COMM UNFCCC CL
[2]  
APA/ARH Norte, 2012, PLAN GEST REG HIDR D
[3]   Climate change and global water resources [J].
Arnell, NW .
GLOBAL ENVIRONMENTAL CHANGE-HUMAN AND POLICY DIMENSIONS, 1999, 9 :S31-S49
[4]   The effect of climate change on hydrological regimes in Europe: a continental perspective [J].
Arnell, NW .
GLOBAL ENVIRONMENTAL CHANGE-HUMAN AND POLICY DIMENSIONS, 1999, 9 (01) :5-23
[5]   Climate risks and adaptation strategies in the Lower Mekong River basin [J].
Bastakoti, Ram C. ;
Gupta, Joyeeta ;
Babel, Mukand S. ;
van Dijk, Meine P. .
REGIONAL ENVIRONMENTAL CHANGE, 2014, 14 (01) :207-219
[6]  
Box G. E. P., 1970, Time series analysis, forecasting and control
[7]   SOME METHODS FOR TESTING THE HOMOGENEITY OF RAINFALL RECORDS [J].
BUISHAND, TA .
JOURNAL OF HYDROLOGY, 1982, 58 (1-2) :11-27
[8]   River networks dampen long-term hydrological signals of climate change [J].
Chezik, K. A. ;
Anderson, S. C. ;
Moore, J. W. .
GEOPHYSICAL RESEARCH LETTERS, 2017, 44 (14) :7256-7264
[9]   DETECTION OF TREND OR CHANGE IN ANNUAL FLOW OF AUSTRALIAN RIVERS [J].
CHIEW, FHS ;
MCMAHON, TA .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 1993, 13 (06) :643-653
[10]   Characterizing Uncertainty of the Hydrologic Impacts of Climate Change [J].
Clark, Martyn P. ;
Wilby, Robert L. ;
Gutmann, Ethan D. ;
Vano, Julie A. ;
Gangopadhyay, Subhrendu ;
Wood, Andrew W. ;
Fowler, Hayley J. ;
Prudhomme, Christel ;
Arnold, Jeffrey R. ;
Brekke, Levi D. .
CURRENT CLIMATE CHANGE REPORTS, 2016, 2 (02) :55-64