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Recent Reductions of Subsidence Rates in the Mississippi River Delta Plain. Julie C. Bernier 1 and Robert A. Morton 2 1 U.S. Geological Survey, Florida Integrated Science Center, St. Petersburg, FL 2 U.S. Geological Survey, Florida Integrated Science Center, Austin, TX.
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Recent Reductions of Subsidence Rates in the Mississippi River Delta Plain Julie C. Bernier1 and Robert A. Morton2 1U.S. Geological Survey, Florida Integrated Science Center, St. Petersburg, FL 2U.S. Geological Survey, Florida Integrated Science Center, Austin, TX
Introduction – Historic Wetland Loss • Delta plain: ~ 4000 km2 land loss since 1930s
Objective • Identify historic trends and most recent subsidence rates through integration of: • tide-gauge records (NOS) → relative sea-level rise (RSLR) • repeat leveling surveys (NGS) → decadal elevation change • continuous GPS (CORS) → short-term elevation change
Grand Isle Tide Gauge • Mid-1960s to early 1990s: accelerated RSLR
Bayou Lafourche Leveling Line • 1982-1993: accelerated subsidence
Integrated Datasets: Temporal Trends 2003-2007: -4.4 mm/yr 1961-1984: -13.6 to -18.7 mm/yr 1965-1993: -9.6 mm/yr 2002-2007: -3.5 mm/yr 1966-1993: -11 mm/yr 1947-1965: -3.3 mm/yr 1965-1993: -10.7 mm/yr 1993-2006: -4.1 mm/yr 2003-2007: -6.3 mm/yr
Bayou Lafourche Leveling Line • Highest rates occur over nearby producing fields
Conclusions and Implications • Decadal-scale acceleration and subsequent deceleration of historic subsidence rates was likely induced by deep subsurface hydrocarbon production • Most recent subsidence rates are comparable to rates averaged over geological time scales • A better understanding of most recent trends and processes causing subsidence needs to be incorporated into coastal restoration efforts and efforts to model expected impacts of increased RSLR