Saltwater Intrusion in a Mediterranean Delta Under a Changing Climate

被引:42
|
作者
Bellafiore, Debora [1 ]
Ferrarin, Christian [1 ]
Maicu, Francesco [1 ,2 ]
Manfe, Giorgia [1 ]
Lorenzetti, Giuliano [1 ]
Umgiesser, Georg [1 ,3 ]
Zaggia, Luca [4 ]
Levinson, Arnoldo Valle [5 ]
机构
[1] Natl Res Council Italy, CNR, ISMAR Marine Sci Inst, Venice, Italy
[2] Univ Bologna, Dept Phys & Astron, Bologna, Italy
[3] Klaipeda Univ, Marine Res Inst, Klaipeda, Lithuania
[4] Natl Res Council Italy, CNR, IGG Inst Geosci & Earth Resources, Padua, Italy
[5] Univ Florida, Civil & Coastal Engn Dept, Gainesville, FL USA
关键词
climate change; coastal lagoons; Po Delta; river‐ sea systems; saltwater intrusion; SEA-LEVEL RISE; PEARL RIVER ESTUARY; SALINITY DISTRIBUTION; ADRIATIC SEA; LAGOONS; IMPACT; VARIABILITY; HYDRODYNAMICS; EVOLUTION; FLOWS;
D O I
10.1029/2020JC016437
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Saltwater intrusion (SWI) in deltas, estuaries, and other coastal areas represents a pressing problem affecting the sustainability of freshwater resources. Observations and numerical experiments are used to investigate SWI in the surface waters of the Italian's largest river delta (the Po Delta) under low discharge conditions. The model successfully reproduced the observed salinity variations along main river branches and in the delta lagoons and investigated fresh and saltwater dynamics during the entire summer 2017. The numerical model is used to explore the hydrological response of the delta system to climate change. The relative effect of controlling factors on saltwater penetration, such as sea-level rise (SLR), air-sea fluxes, and reduction of river discharge, was evaluated. Results suggest that changes driven by climate and SLR will exacerbate SWI in the surface waters of the Po Delta system. Extent of SWI in the major river branch is projected to increase up to 80% further into the river. Persistence of SWI at the same site is expected to increase 100% longer. Moreover, additional synthetic simulations were used to investigate the sensitivity of SWI to several river discharges and relative SLR values, highlighting the effects of the two factors in the delta. Such results show different combinations of river discharge and relative SLR values that represent possible scenarios, and are important for managing SWI in river-sea systems affected by both climatic and anthropogenic factors such as discharge changes from dam construction, land use, and irrigation.
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页数:23
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