click to go home Education Module SECTORS DEMOGRAPHICS GIS Climate GCM
Wetlands

Download Full Report ( 2.1 MB )
The impact of future wetland loss from sea-level rise, storm surges and other forces over the next 100 years is examined with an emphasis on a case study in Jamaica Bay, Queens County, New York City. Change over the previous 100 years is documented through use of historic maps, aerial photography and field observations. Projections of future change are extrapolated from current trends and three global climate models (GCMs). Descriptions of intertidal wetland plant communities are discussed in relation to zonation that is strongly correlated with extent of tidal flooding which may become accelerated with global warming.

Coastal salt marshes of Northeastern United States (Maine to New Jersey) formed within the last 4000 to 7000 years, following deglaciation of the last Ice Age initiated about 15,000 years ago. As sea-level slowed, a string of highly productive, peat-forming coastal wetland marshes extending from the easternmost tip of Long Island to what is now New York City, and north along the Hudson River developed. More recently, alterations in marsh geomorphology consists of a reversal of the marsh-building process through land loss from marsh erosion and inundation.

The rate of local SLR is about 2.7mm per year as determined by tide gauge data (1961-1990) from Battery Park in Manhattan. This can be compared to the mean global sea-level rise (SLR) of 1.8 mm/yr since the 1900s, due in part to anthropogenic causes. The difference between the global and the New York average sea-level rise is due, in part, to local subsidence resulting from retreat of the last ice age. Using current trends and three GCMs, local SLR projections indicate that by the 2020s SLR is estimated to be between 2.7 and 7.3 mm/yr, by the 2050s it will likely range between 2.7 and 13.7 mm/yr, and by the 2080s SLR is estimated to be between 2.7 and 22.7 mm/yr. Erosion of Jamaica Bay marshes is likely to continue, caused by a combination of SLR, changes in inshore wave energy, dredging and channel modification, and lowered sediment levels available to nourish vertical marsh accretion. GCM scenarios, accounting for marsh accretion, indicate that future loss of New York City’s salt marshes may be greater than fifty percent due to erosion and inundation.

  • Local marsh accretion rates of 3-8mm yr-1, found in the scientific literature, can be compared to SLR rise projections. Comparisons suggest that marsh loss will be moderate during the 2020's, and potentially extreme by the 2080s when sea level rise projections outpace almost all known accretion rates.
  • Jamaica Bay is a renowned sanctuary for birds and threatened diamondback terrapins. It is provides productive habitat for fish and invertebrates that support a long food chain. Wetland loss will eliminate essential habitat for birds, terrapins, fish and invertebrates.
  • Wetlands serve as a protective barrier against coastal flooding. This valuable function may be lost in the MEC region as sea level rises- increasing the impacts of climate change.
  • Wetlands filter nutrients and inorganic materials, reducing the impacts of coastal pollution. This valuable service may be lost in the MEC region as sea level rises.
click to go home Related Links Comments Credits and Acknowledgements

site created and maintained by
Center for International Earth Science Information Network
CIESIN Columbia University
Copyright ©2000