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Monitoring a recent delta formation in a tropical coastal wetland using remote sensing and GIS. Case study: Guapo River delta, Laguna de Tacarigua, Venezuela
Calzadillla Pérez, A.; Damen, M.C.J.; Geneletti, D.; Hobma, T.W. (2002). Monitoring a recent delta formation in a tropical coastal wetland using remote sensing and GIS. Case study: Guapo River delta, Laguna de Tacarigua, Venezuela. Environ. Dev. Sustain. 4(2): 201-219. https://dx.doi.org/10.1023/A:1020830809448
In: Environment, Development and Sustainability. Springer Science+Business Media: London; Dordrecht; Boston. ISSN 1387-585X; e-ISSN 1573-2975, more
Also appears in:
Dahdouh-Guebas, F. (Ed.) (2002). Remote sensing and GIS in the sustainable management of tropical coastal ecosystems. Environment, Development and Sustainability, 4(2). Kluwer Academic: Dordrecht. 144 pp., more
Peer reviewed article  

Available in  Authors 

Keyword
    Marine/Coastal

Authors  Top 
  • Calzadillla Pérez, A.
  • Damen, M.C.J.
  • Geneletti, D.
  • Hobma, T.W.

Abstract
    The integrated use of remotely sensed data and GIS to monitor a rapid recent delta formation was undertaken in the Tacarigua Lagoon, a mangrove coastal protected wetland in the north-central coast of Venezuela. Recently, the resource value of coastal wetlands such as coastal lagoons and deltas, has brought about a need to protect and conserve these ecosystems. To that end, valuable resources such as these should be continuously monitored so that temporal changes in their environment can be analysed. The importance of determining the cause, extent, and spatial distribution of these changes can then be used in different aspects of environmental studies, land suitability analyses and for wise resource management. Aerospace data interpretation and a field survey were utilised to study the formation of the Guapo River delta within the Tacarigua Lagoon and to map the expansion that this depositional environment has undergone. A historical set of aerial photographs and a radar image, together with a GIS, were used to assess the growth of the delta from the beginning of its formation up to the present time.

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