Researchers use satellite data to quantify wetland loss
June 28, 2016
University of Miami Rosenstiel School of Marine & Atmospheric Science
As Louisiana’s wetlands continue to disappear at an alarming rate, a new study has pinpointed the human-made structures that disrupt the natural water flow and threaten these important ecosystems. The findings have important implications for New Orleans and other coastal cities that rely on coastal wetlands to serve as buffer from destructive extreme weather events.
Scientists at the University of Miami (UM) Rosenstiel School of Marine and Atmospheric Science found that human-made canals limit the natural tidal inundation process in roughly 45 percent of the state’s coastline, and disruptions from levees accounted for 15 percent.
“This study demonstrates that human infrastructure development along coastal areas have long-term consequences on the ability of coastal wetlands to adapt to sea-level rise and other processes that reduce the size of coastal wetlands,” said Talib Oliver-Cabrera, the study’s first author and a UM Rosenstiel School Ph.D. student.
Coastal wetlands in Louisiana are economically and esthetically important by providing storm protection, flood control, and essential habitats for a myriad of wildlife. They support economically important commercial and recreational fishing industries, tourism, and oil and gas industries.
Human-made structures, such as levees and canals, have changed the regular patterns of tidal inundation in coastal wetlands and have become a main element in determining coastal wetland distribution.
Using a remote sensing technique, called Interferometric Synthetic Aperture Radar (InSAR),
the researchers analyzed water-level changes in Louisiana’s coastal wetlands that occurred due to tidal inundation. Based on the detected changes observed, they were able to determine the extent of tidal inundations along the Louisiana coast….
Talib Oliver-Cabrera, Shimon Wdowinski. InSAR-Based Mapping of Tidal Inundation Extent and Amplitude in Louisiana Coastal Wetlands. Remote Sensing, 2016; 8 (5): 393 DOI: 10.3390/rs8050393
The red frames show the location of enlarged interferograms presented in Figures A, B and C. A) Radarsat-1 interferogram of the western Chenier Plain spanning 24-day period (2004/01/03-2004/01/27). In the central part of the interferogram fringe patterns show changes in inland water bodies. The left side of the interferogram shows fringe patterns due to the morphology of the Chenier reflecting water level changes in the mudflats in between the ridges of the Chenier’s. B) ALOS interferogram, 92 days (2007/07/03-2007/10/03), of the central Chenier Plain showing phase changes due to elongated fringe patterns sub-parallel to the coastline coinciding with man-made canals. C) ALOS interferogram of the west of the Mississippi River delta, spanning 92-day period (2007/09/11-2007/12/12). The interferogram showing two fringe cycles across the tidal zone mapping the tide inundation extent.
Credit: Talib Oliver-Cabrera, UM Rosenstiel School of Marine and Atmospheric Science