Sea level rise

Global warming and associated sea-level rise may have considerable implications the world over. The magnitude of the predicted global rise in sea-level is not known, but the Intergovernmental Panel on Climatic Changes (IPCC) estimates the rise to be 0.3-0.5 m by the year 2050 and about one meter by the year 2100. The implications would vary greatly from one coast to another, depending on local topography, climate, tectonics and use of the coastal zone.

Some of the most important effects of a rise in sea level would be inundation and displacement of coastal lowlands and wetlands, eroding shorelines, increased coastal storm flooding, increased salinity in estuaries and freshwater aquifers, altered tidal ranges, changes in sedimentation patterns and changed biological production.

According to a study conducted by the National Institute of Oceanography (NIO) Goa, the problem of flooding is more severe in east coast as a consequence of sea level rise due to low gradient of coastal topography. Global warming may cause considerable changes in the structure and distribution of marine habitats. Coastal wetlands and other coastal habitats may migrate inland or respond in other ways to sea level rise, but intensive human land-use will limit their distribution. Changes in ocean circulation, currents and upwelling areas may affect recruitment, distribution and catchability of commercial fish stocks.

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