Hydrology under climate change in a temporary river system: Potential impact on water balance and flow regime

被引:48
|
作者
De Girolamo, A. M. [1 ]
Bouraoui, F. [2 ]
Buffagni, A. [3 ,4 ]
Pappagallo, G. [1 ]
Lo Porto, A. [1 ]
机构
[1] CNR, Water Res Inst, 5 Viale F De Blasio, I-70132 Bari, Italy
[2] European Commiss, Joint Res Ctr, Ispra, VA, Italy
[3] CNR, Water Res Inst, Brugherio, MB, Italy
[4] Univ Tuscia, Dipartimento Sci Ecol & Biol, Viterbo, Italy
关键词
climate change; hydrological indicators; hydrological modelling; impact on blue waters; impact on hydrological regime; streamflow regime; MANAGEMENT; BASIN; STREAMS; PROJECTIONS; INDICATORS; DIVERSITY; QUALITY; EUROPE; TRENDS; TOOL;
D O I
10.1002/rra.3165
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The potential impacts of future climate scenarios on water balance and flow regime are presented and discussed for a temporary river system in southern Italy. Different climate projections for the future (2030-2059) and the recent conditions (1980-2009) were investigated. A hydrological model (Soil and Water Assessment Tool) was used to simulate water balance at the basin scale and streamflow in a number of river sections under various climate change scenarios, based on different combinations of global and regional models (global circulation models and regional climate models). The impact on water balance components was quantified at the basin and subbasin levels as deviation from the baseline (1980-2009), and the flow regime alteration under changing climate was estimated using a number of hydrological indicators. An increase in mean temperature for all months between 0.5-2.4 degrees C and a reduction in precipitation (by 4-7%) was predicted for the future. As a consequence, a decline of blue water (7-18%) and total water yield (11-28%) was estimated. Although the river type classification remains unvaried, the flow regime distinctly moves towards drier conditions and the divergence from the current status increases in future scenarios, especially for those reaches classified as I-D (ie, intermittent-dry) and E (ephemeral). Hydrological indicators showed a decrease in both high flow and low flow magnitudes for various time durations, an extension of the dry season and an exacerbation of extreme low flow conditions. A reduction of snowfall in the mountainous part of the basin and an increase in potential evapotranspiration was also estimated (4-4.4%). Finally, the paper analyses the implications of the climate change for river ecosystems and for River Basin Management Planning. The defined quantitative estimates of water balance alteration could support the identification of priorities that should be addressed in upcoming years to set water-saving actions.
引用
收藏
页码:1219 / 1232
页数:14
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