In these coastal areas, a hurricane or other
large coastal storm can push water inland in a large and damaging storm surge.
Not exact matches
Prompt action is needed most in Asia and Africa where, today,
large parts of the
coastal population are already affected by
storm surge flooding.
This relatively sudden rise of normal sea level occurs when
storm winds and tides combine to transport
large volumes of water to
coastal areas.
And while countries like Myanmar will have the
largest number of displaced peoples from climate change, even countries like the US are likely to see a surge in internally displaced people as
coastal communities come face to face with sea level rise and more destructive
storms.
Coastal states with
large areas of low - lying land, including Louisiana, Florida, North Carolina, California, and South Carolina, are particularly vulnerable to rising seas and
coastal storm surges.
Mid-latitude islands, such as islands in the Gulf of St. Lawrence and off the coast of Newfoundland (St. Pierre et Miquelon), are exposed to impacts from tropical, post-tropical, and extra-tropical
storms that can produce
storm - surge flooding,
large waves,
coastal erosion, and (in some winter
storms) direct sea ice damage to infrastructure and property.
More - powerful
storms can combine with even a modest rise in sea level in a dangerous synergy, allowing for ever
larger storm surges that can flatten
coastal communities.
Coastal marshes absorb and store
large amounts of carbon dioxide from Earth's atmosphere; they help filter out pollution in
coastal waters; provide habitat for wildlife; help protect coastlines from erosion and
storm surge; and can store huge amounts of floodwater, reducing the threat of flooding in low - lying
coastal areas.
With the late - summer ice edge located farther north than it used to be,
storms produce
larger waves and more
coastal erosion.5 An additional contributing factor is that
coastal bluffs that were «cemented» by ice - rich permafrost are beginning to thaw in response to warmer air and ocean waters, and are therefore more vulnerable to erosion.22 Standard defensive adaptation strategies to protect
coastal communities from erosion, such as use of rock walls, sandbags, and riprap, have been largely unsuccessful.23 Several
coastal communities are seeking to relocate to escape erosion that threatens infrastructure and services but, because of high costs and policy constraints on use of federal funds for community relocation, only one Alaskan village has begun to relocate (see also Ch.
There is new information that lack of sea ice causes
storms to produce
larger waves and more
coastal erosion.5 An additional contributing factor is that
coastal bluffs that were «cemented» by permafrost are beginning to thaw in response to warmer air and ocean waters, and are therefore more vulnerable to erosion.22 Standard defensive adaptation strategies to protect
coastal communities from erosion such as use of rock walls, sandbags, and riprap have been largely unsuccessful.23 There remains considerable uncertainty, however, about the spatial patterns of future
coastal erosion.
«If we cause
large sea - level rise, that dominates future risks, but if we could prevent sea - level rise and just have the
storm surge to worry about, our projections show little change in
coastal risk from today during most years,» said Michael Mann, distinguished professor of meteorology and atmospheric science and director of Penn State's Earth System Science Centre, and one of the authors.
For example, rising sea level increases the likelihood that a
storm surge will overtop a levee or damage other
coastal infrastructure, such as
coastal roads, sewage treatment plants, or gas lines — all with potentially
large, expensive, and immediate consequences (Nordhaus, 2010).