By Chad J. McGuire
Finished, yet now not overly technical, this ebook offers a legal-policy framework to the dialogue of ways coastal managers can most sensible method the matter of sea point upward thrust. It identifies felony boundaries and gives proposed recommendations to mitigate the impression of these limitations. The publication introduces the difficulty, delves into the technological know-how at the back of sea point upward push, discusses coverage complexities and recommendations, by means of an summary of similar legalities, then, bringing all of it jointly, the writer applies the rules provided within the publication, concluding with thoughts and recommendations and a standpoint at the destiny.
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Additional info for Adapting to Sea Level Rise in the Coastal Zone: Law and Policy Considerations
In addition, coastal wetlands provide important buffers from ocean-derived storms, mitigating the intensity and impact of storm surges on coastal areas (Bryant 1997). There are other valuable provisioning, regulating, and aesthetic services provided by coastal wetlands (Millennium Ecosystem Assessment 2003); the value of these services has been estimated to be in the billions to trillions of dollars (Costanza et al. 1997). The fact is that current impacts of sea level rise on the ecological values of near-coastal areas are substantial, and the impacts will likely increase with continued sea level rise.
Some of the air is distributed back toward the equator, while other portions are heated and rise to yet higher latitudes. Collectively, these patterns help to move currents in the ocean as warm air masses transfer heat to the oceans and that heat then drives currents through a process of cooling and heating that alters water densities and thereby creates movement as a by-product (Schlesinger 1997). This process is not unlike how our bodies regulate heat by using our system of blood vessels to move warmed liquid blood to the surface of our skin where it can be cooled by the air outside our bodies.
Changes in observed heat distribution patterns can impact components of the Earth system such as the hydrosphere. Lower-density hot air rises at the equator and then cools as it moves up into higher elevations of the atmosphere. Wind patterns push the denser cooler air to higher latitudes where it begins to sink. Some of the air is distributed back toward the equator, while other portions are heated and rise to yet higher latitudes. Collectively, these patterns help to move currents in the ocean as warm air masses transfer heat to the oceans and that heat then drives currents through a process of cooling and heating that alters water densities and thereby creates movement as a by-product (Schlesinger 1997).
Adapting to Sea Level Rise in the Coastal Zone: Law and Policy Considerations by Chad J. McGuire