By Chad J. McGuire
Complete, yet no longer overly technical, this e-book presents a legal-policy framework to the dialogue of the way coastal managers can top strategy the matter of sea point upward thrust. It identifies criminal boundaries and gives proposed options to mitigate the impression of these boundaries. The ebook introduces the difficulty, delves into the technology in the back of sea point upward push, discusses coverage complexities and recommendations, via an outline of comparable legalities, then, bringing all of it jointly, the writer applies the rules provided within the publication, concluding with techniques and suggestions and a standpoint at the destiny.
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Additional resources for Adapting to Sea Level Rise in the Coastal Zone: Law and Policy Considerations
Examples of heat-trapping compounds include carbon dioxide (CO2) and methane (CH4). When these compounds are found in higher concentrations in the atmosphere, more heat tends to be trapped in the Earth system; the compounds allow new heat to enter the system but they prevent existing heat from leaving the system. This phenomenon is commonly referred to as the greenhouse effect (Schlesinger 1997). The greenhouse effect can cause the Earth system to carry more heat than is historically found within the Earth since human civilization began.
51–57). Science behind Sea Level Rise ◾ 23 into the atmosphere through a process of respiration. Once in the atmosphere, the carbon atom links up with oxygen to form carbon dioxide. The carbon ultimately gets taken up by a plant near the surface during photosynthesis and is transformed into a simple carbohydrate, becoming part of another plant body. The plant is eaten again and the carbon atom becomes part of the consumer’s muscular system. The animal (say, a dinosaur) dies in a low oxygen environment and its body slowly decays over millions of years, ultimately becoming oil trapped underground.
Moreover, in the well-mixed Earth system, carbon concentrations are at equilibrium, meaning the amount of carbon within any component of the system is relatively stable and at a certain concentration that will be the same even when measured at different times. This idea of well-mixed concentrations is readily observed in the atmosphere with oxygen; the concentration of oxygen in the atmosphere is around 21 percent and it remains relatively constant over time even though the oxygen itself is constantly being removed and added to the atmosphere (Schlesinger 1997).
Adapting to Sea Level Rise in the Coastal Zone: Law and Policy Considerations by Chad J. McGuire