Setting an environmental flow regime under climate change in a data-limited Mediterranean basin with temporary river

被引:0
|
作者
Leone, M. [1 ,2 ,4 ]
Gentile, F. [2 ]
Lo Porto, A. [1 ]
Ricci, G. F. [2 ]
Schuerz, C.
Strauch, M. [3 ]
Volk, M. [3 ]
De Girolamo, A. M. [1 ]
机构
[1] Natl Res Council Italy, CNR, Water Res Inst, IRSA, Viale F Blasio 5, I-70132 Bari, Italy
[2] Univ Bari Aldo Moro, Dept Soil Plant & Food Sci, Via Giovanni Amendola 165-A, Bari, Italy
[3] UFZ Helmholtz Ctr Environm Res, Dept Computat Landscape Ecol, Permoserstr 15, D-04318 Leipzig, Germany
[4] Univ Bari Aldo Moro, Dept Soil Plant & Food Sci, Via Giovanni Amendola 165-A, I-70126 Bari, Italy
关键词
Environmental Flows; SWAT+; Temporary rivers; Modeling low flows; Indicators of Hydrological Alterations (IHAs); Climate Change; BIAS CORRECTION; HYDROLOGIC ALTERATION; PERFORMANCE EVALUATION; ASSESSMENT-TOOL; APULIA REGION; COSMO-CLM; WATER; MODEL; PRECIPITATION; SIMULATIONS;
D O I
10.1016/j.ejrh.2024.101698
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Study region: Catchment in Southern Italy. Study focus: Mediterranean waterways are commonly non-perennial; they are vulnerable to climate change (CC). Their management is particularly complex due to limited data availability. This work aims to develop a methodology for setting an Environmental Flow regime (E-Flows) for a temporary river (Locone, Italy) under limited data availability and under CC. As observed longterm time series of streamflow under natural conditions were not available, the Soil and Water Assessment Tool model (SWAT+) was applied to simulate the daily streamflow for the baseline period (1980-2010) and future (2020-2050) based on observed and model climate projections, respectively. A specific workflow was developed for model calibration focusing on the low flows. The hydrological regime was characterized by means of Indicators of Hydrological Alteration (IHAs), whereas the Range of Variability Approach (RVA) was applied to define the E-Flows. New hydrological insights for the region: The basin is experiencing a statistically significant increase in the air temperatures observed from 1971 to 2020, which is also predicted to continue in the future. Consequently, the average annual streamflow and monthly streamflow in winter and spring is expected to decrease. The calibration, based on a multi -objective model evaluation, improved the low-flow simulation. The detected differences in IHAs for the predicted periods should be considered in future water management when setting E-Flows for temporary rivers.
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页数:19
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