scholarly journals WATER RESERVE FOR THE ALVARADO COASTAL LAGOON WETLAND AS A MEASURE TO INCREASE RESILIENCE TO CLIMATE CHANGE

Author(s):  
HÉCTOR SANVICENTE-SÁNCHEZ ◽  
CERVANDO CASTILLO-ROMANO ◽  
YOLANDA SOLÍS-ALVARADO

2018 ◽  
Vol 85 ◽  
pp. 521-525 ◽  
Author(s):  
Sandra Costa ◽  
Ana Picado ◽  
Nuno Vaz ◽  
Carlos Coelho ◽  
Luís Portela ◽  
...  


2018 ◽  
Vol 9 ◽  
Author(s):  
Márcio S. de Souza ◽  
José H. Muelbert ◽  
Luiza D. F. Costa ◽  
Eliana V. Klering ◽  
João S. Yunes


2008 ◽  
Vol 78 (2) ◽  
pp. 403-412 ◽  
Author(s):  
Javier Lloret ◽  
Arnaldo Marín ◽  
Lázaro Marín-Guirao




2012 ◽  
Vol 114 ◽  
pp. 118-129 ◽  
Author(s):  
Francesca De Pascalis ◽  
Angel Pérez-Ruzafa ◽  
Javier Gilabert ◽  
Concepción Marcos ◽  
Georg Umgiesser


Author(s):  
Marta Rodrigues ◽  
Alexandra Rosa ◽  
Alexandra Cravo ◽  
José Jacob ◽  
André B. Fortunato


2020 ◽  
Author(s):  
Madeline LeBlanc ◽  
Theocharis Plomaritis ◽  
Alejandro Lopez-Ruiz

<p>Climate change has resulted in increased storminess and sea-level change that affects the morphodynamics of bays worldwide, impacting both the ecosystem and local infrastructure. This study explores the impact of differing storm winds on the sediment budget of the Bay of Cadiz. The Bay of Cadiz is a highly altered coastal lagoon located in Southwest Spain surrounded by ports, navigation channels, and urban developments and is of high socioeconomic and environmental importance. The human interactions with the bay have already caused morphological impacts, which could be exacerbated by increased storminess. Potential impacts on the sediment budget of the Bay of Cadiz will be modeled using a Delft3D model previously calibrated and tested using field data from December 2011 to January 2012. The model will consider a variety of storm wind scenarios and observe their impacts on sediment transport within the bay, identifying sources and sinks. This will help to estimate the potential impacts of climate change and increased storminess on the bay and the surrounding areas.</p>



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