By Chad J. McGuire
Finished, yet now not overly technical, this publication presents a legal-policy framework to the dialogue of the way coastal managers can top technique the matter of sea point upward thrust. It identifies felony obstacles and gives proposed strategies to mitigate the effect of these obstacles. The ebook introduces the problem, delves into the technology in the back of sea point upward thrust, discusses coverage complexities and innovations, through an outline of comparable legalities, then, bringing all of it jointly, the writer applies the rules provided within the booklet, concluding with thoughts and strategies and a viewpoint at the destiny.
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Additional info for Adapting to Sea Level Rise in the Coastal Zone: Law and Policy Considerations
The cause of these changes is almost always a shift in energy distributions within the system (IPCC 2007). The causes of sea level rise can be discussed in the context of Earth system dynamics, particularly by looking for shifts in energy distributions throughout the system. The clearest way to explain energy shifts within the Earth system itself is to look for changes in the major components of the Earth system; by identifying shifts in energy distributions between system components—say shifts in the hydrosphere and atmosphere—the cause of sea level rise becomes apparent.
Some of the upland connected to the ocean can be more susceptible to erosion, depending on the makeup of the soil and the dynamics associated with the new land–sea boundary. A strong surging tide can also impact the shape of the nearshore landmass, creating shifting land that is relatively unstable. In addition, the rate of sea level rise in a given coastal area can impact existing wetlands and the development of new wetlands or intertidal areas, depending on local conditions (Brooks, Adger, and Kelly 2005).
Broadly speaking, low-lying island nations that are particularly vulnerable to sea level rise are experiencing a disproportionate impact on social and cultural identity. This is primarily due to the fact that “vulnerability” related to sea level rise is often determined by two factors: (1) exposure to a hazard and (2) the capacity to adapt to the hazard. Beyond island nations, low-lying coastal communities with available upland retreat areas can be just as vulnerable to sea level rise as island areas where retreat inland is not possible, and sometimes these regions can be more vulnerable than island nations.