scholarly journals Postglacial sea-level rise and sedimentary response in the Guadiana Estuary, Portugal/Spain border

2002 ◽  
Vol 150 (1-2) ◽  
pp. 103-122 ◽  
Author(s):  
T. Boski ◽  
D. Moura ◽  
C. Veiga-Pires ◽  
S. Camacho ◽  
D. Duarte ◽  
...  
2020 ◽  
Vol 44 ◽  
pp. 101169 ◽  
Author(s):  
Lara Mills ◽  
João Janeiro ◽  
Antonio Augusto Sepp Neves ◽  
Flávio Martins

Author(s):  
Lara Mills ◽  
João Janeiro ◽  
Flávio Martins

Abstract Sea level rise is a worldwide concern as a high percentage of the population accommodates coastal areas. The focus of this study is the impact of sea level rise in the Guadiana Estuary, an estuary in the Iberian Peninsula formed at the interface of the Guadiana River and the Gulf of Cadiz. Estuaries will be impacted by sea level rise as these transitional environments host highly diverse and complex marine ecosystems. The major consequences of sea level rise are the intrusion of salt from the sea into fresh water and an increase in flooding area. As the physical, chemical, and biological components of estuaries are sensitive to changes in salinity, the purpose of this study is to further evaluate salt intrusion in the Guadiana Estuary caused by sea level rise. Hydrodynamics of the Guadiana Estuary were simulated in a two-dimensional numerical model with the MOHID water modeling system. A previously developed hydrodynamic model was implemented to further examine changes in salinity distribution in the estuary in response to sea level rise. Varying tidal amplitudes, freshwater discharge from the Guadiana River and bathymetries of the estuary were incorporated in the model to fully evaluate the impacts of sea level rise on salinity distribution and flooding areas of the estuary. Results show an overall increase in salinity and land inundation in the estuary in response to sea level rise.


2011 ◽  
Vol 26 (2) ◽  
pp. 156-170 ◽  
Author(s):  
Dissanayake M.R. Sampath ◽  
Tomasz Boski ◽  
Patricia L. Silva ◽  
Flavio A. Martins

Eos ◽  
2020 ◽  
Vol 101 ◽  
Author(s):  
Kate Wheeling

Researchers identify the main sources of uncertainty in projections of global glacier mass change, which is expected to add about 8–16 centimeters to sea level, through this century.


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