Download Adapting to Sea Level Rise in the Coastal Zone: Law and by Chad J. McGuire PDF
By Chad J. McGuire
Accomplished, yet no longer overly technical, this booklet offers a legal-policy framework to the dialogue of ways coastal managers can top strategy the matter of sea point upward thrust. It identifies criminal boundaries and provides proposed suggestions to mitigate the impression of these limitations. The publication introduces the problem, delves into the technological know-how in the back of sea point upward push, discusses coverage complexities and ideas, via an summary of comparable legalities, then, bringing all of it jointly, the writer applies the foundations provided within the ebook, concluding with ideas and recommendations and a viewpoint at the destiny.
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Additional resources for Adapting to Sea Level Rise in the Coastal Zone: Law and Policy Considerations
The story of the carbon atom cycling throughout the Earth system helps identify an important contributor to sea level rise. To understand carbon’s contribution, a summary knowledge of system dynamics and equilibrium theory is necessary. With this summary knowledge, the following can be surmised: The Earth’s carbon cycle is shifting out of balance with its historical equilibrium state through actions that include the removal of carbon stored in one component of the system (lithosphere) and the addition of that carbon to another component of the system (atmosphere).
For example, the Keeling data on carbon dioxide concentrations now exists from 1958 up to the present time; well over 50 years of data are available for analysis. Not only can changes in the concentration of carbon dioxide be observed on a year-to-year and decade-to-decade basis, but any changes in the rates of increase can be observed as well. Also, the current information observed can be related to indirect observations through other methods of analysis. For example, cores of glacial ice dated to tens of thousands of years ago contain relative concentrations of what was in the atmosphere when the ice froze (Schlesinger 1997).
This rise in surface temperature is stimulating a phase change through the melting of water in areas where it has traditionally been stored as ice. The melting is causing more liquid water to enter our oceans, thus causing ocean levels to rise. This process is similar to how leaving the faucet on in a plugged bathtub will cause the water level in that bathtub to rise. So there we have it: The relationship between energy flows and the Earth system is responsible for some of the sea level rise we are currently observing, and most likely the vast majority of sea level rise currently observed (IPCC 2007).