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Sea-level rise driven soil salinization

Citation Link: https://doi.org/10.15480/882.3862
Publikationstyp
Conference Paper
Date Issued
2021-04
Sprache
English
Author(s)
Nevermann, Hannes  
Agha Kouchak, Amir  
Shokri, Nima  
Institut
Geohydroinformatik B-9  
TORE-DOI
10.15480/882.3862
TORE-URI
http://hdl.handle.net/11420/10722
Article Number
14453
Citation
EGU General Assembly: 14453 (2021)
Contribution to Conference
EGU General Assembly, 2021  
Publisher DOI
10.5194/egusphere-egu21-14453
Sea level rise (SLR) is a well-documented aspect of anthropogenic climate change which is primary due to the thermal expansion of seawater and melting of ice caps and glaciers (1). Climate change is expected to exacerbate sea-level rise within the next century, much larger than the observations since the beginning of the recordings. Next to various natural hazards and extreme environmental events such as flooding, the sea level rise poses serious long-standing and possibly irreversible consequences on human timescales in coastal regions. For example, soil salinity is expected to increase near shorelines due to sea level rise. Soil salinization, referring to excess accumulation of salt in soil, is a global problem (2) adversely affecting many environmental and hydrologic processes such as terrestrial ecosystem functioning, water cycle and biodiversity. SLRs shift the saltwater-freshwater boundary in coastal regions which will increase the risk of soil salinization further inland. Considering the growing population living in coastal regions, SLR-driven soil salinization has a severe socio-economic impact posing significant threat to farmlands, wetlands, coastal marshes, forests and other ecosystems. Motivated by the importance of the interaction between SLR, climate change and soil salinization, this study aims to determine how the saltwater- freshwater interface moves under different Representative Concentration Pathways (RCP) scenarios in coastal regions. Groundwater data of coastal wells, Digital Elevation Model’s and satellite images will be used to highlight areas under high risk of soil salinization. The results will enable us to quantify the possible extent of the soil salinization as a result of SLR under different climate scenarios with the associated socio-economic consequences. Such information could support decision making and sustainable resource management under different RCPs.
DDC Class
004: Informatik
550: Geowissenschaften
Publication version
publishedVersion
Lizenz
https://creativecommons.org/licenses/by/4.0/
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