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024 8    |a FI14082515
024 7    |a 10.5670/oceanog.2013.46 |2 doi
245 00 |a Remote-sensing monitoring of tide propagation through coastal wetlands |h [electronic resource].
260        |a [S.l.] : |b The Oceanography Society, |c 2013.
490        |a Oceanography.
506        |a This article has been published in Oceanography, Volume 26, Number 3, a quarterly journal of The Oceanography Society. Copyright 2013 by The Oceanography Society. All rights reserved. Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: info@tos.org or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA.
510        |a Wdowinski, S., S.-H. Hong, A. Mulcan, and B. Brisco. 2013. Remote-sensing monitoring of tide propagation through coastal wetlands. Oceanography 26(3):64–69, http://dx.doi.org/10.5670/ oceanog.2013.46.
520 3    |a Tide propagation through coastal wetlands is a complex phenomenon affected by vegetation, channels, and tidal conditions. Generally, tidal flow is studied using stage (water level) observations, which provide good temporal resolution, but they are acquired in limited locations. Here, a remotesensing technique, wetland InSAR (interferometric synthetic aperture radar), is used to detect tidal flow in vegetated coastal environments over broad spatial scales. The technique is applied to data sets acquired by three radar satellites over the western Everglades in south Florida. Interferometric analysis of the data shows that the greatest water-level changes occur along tidal channels, reflecting a high velocity gradient between fast horizontal flow in the channel and the slow flow propagation through the vegetation. The high-resolution observations indicate that the tidal flushing zone extends 2–3 km on both sides of tidal channels and can extend 3–4 km inland from the end of the channel. The InSAR observations can also serve as quantitative constraints for detailed coastal wetland flow models.
533        |a Electronic reproduction. |c Florida International University, |d 2014. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650        |a Coastal ecology |z Florida |z Everglades.
655    4 |a article.
655    7 |a serial |2 sobekcm
700 1    |a Wdowinski, Shimon.
700 1    |a Hong, Sang-Hoon.
700 1    |a Mulcan, Amanda.
700 1    |a Brisco, Brian.
830    0 |a dpSobek.
830    0 |a Everglades Digital Library: Reclaiming the Everglades.
852        |a dpSobek |c Everglades Digital Library: Reclaiming the Everglades
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI14082515/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/14/08/25/15/00001/FI14082515thm.jpg
997        |a Everglades Digital Library: Reclaiming the Everglades


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