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Presentation transcript:

Begin with introductory video

Climate Change & Sea-Level Rise Along the Gulf of Mexico A COSEE Online Institute Presentation Dr. E.D. Estevez Mote Marine Laboratory

Today’s Topics Sea level background Signs of sea-level rise Projections of future sea-level rise Visualizing sea level now and in the future

Sea-Level Variations Waves Tides Storm Surges Seiches Intra-Annual Cycles Multi-Annual/Decadal Cycles (El Niño, AMO) Planetary Cycles (Milankovitch Cycles) Anthropogenic Forcing

In the Context of Climate Change… The main contributors to sea level and sea- level rise are: 1.Steric effects- the expansion of the world ocean as it warms 2.“New water”- addition of water from ice sheets and glaciers Other factors are also involved.

Subsidence Subsidence, or the sinking of land, has multiple causes. Without sea-level rise, a subsiding coast experiences a relative rise in sea level. Subsidence added to sea-level rise enhances the rate of relative sea-level rise. Subsidence contributes to the loss of coastal wetlands, but Coastal wetlands and forests are also affected by the present rate of sea-level rise, even in the absence of subsidence.

Effects: Sea Level Rise WHAT WE KNOW Many tidal wetlands are keeping pace with sea level changes. Some are accreting vertically, migrating up-slope, or both. Open estuarine waters, brackish marsh, and mangroves in south Florida estuaries are expanding. Wetlands elsewhere are perishing as estuarine and coastal forests and swamps are retreating, replaced by marsh vegetation. Even at constant rates of sea level rise, some tidal wetlands will eventually “pinch out” where their upslope migration is prevented by upland defenses such as seawalls.

Effects: Sea Level Rise WHAT IS PROBABLE Major spatial shifts in wetland communities, including exotic species invasions, will occur. More lowland coastal forests will be lost during the next one to three centuries as tidal wetlands expand across low-lying coastal areas. High diversity wetlands in tidal freshwater reaches of coastal rivers will be replaced by low diversity wetlands. Most tidal wetlands in areas with low freshwater and sediment supplies will “drown” if sea level rise outpaces their ability to accrete vertically.

Effects: Sea Level Rise WHAT IS POSSIBLE More than half of the saltmarsh, shoals, and mudflats critical to birds and fishes foraging in Florida estuaries, could be lost during the 21 st century. Recreational and commercial fish species that depend on shallow water, or intertidal and subtidal plant communities, are vulnerable. The loss of tidal wetlands will result in dangerous losses of the coastal systems that buffer storm impacts.

Lido Key, Sarasota County, Florida Wednesday 09/16/09 11:05 am (2.4 ft. astronomical)

Gulf Waters Flooding Storm-water Drains at Normal High Tide

We Already Adapt Seawalls, Docks and Piers Bridges and Causeways Stormwater Systems Beach Policies and Practices Wetland Creation Building Heights Disaster Preparedness

Sea-Level Rise Visualization for Alabama and Mississippi. This pilot project is a collaborative effort of the National Oceanic and Atmospheric Administration (NOAA) Coastal Services Center, Mississippi-Alabama Sea Grant Consortium, and U.S. Geological Survey.

Insert second video with pan of beach

Mobile State Docks, Mobile River Mobile State Docks

Used with permission by Sarasota Magazine

For Local Help Louisiana Universities Marine Consortium Gulf Coast Research Laboratory Dauphin Island Sea Lab NOAA CO-OPS Water Level Program

Thank You, and Thanks to… Brian M. McCann, Ph.D. Center for Educational and Training Technology Multimedia Development Group Mississippi State University Rusty Holmes and Joe Nickelson Mote Marine Laboratory Barbara Lausche Mote Marine Policy Institute Sarasota Magazine Anonymous reviewers …and the many public agencies from whom slides were borrowed.