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greater changes. The figure below shows projected percentage change in precipitation between the current climate (represented by the average) and the end of the century ( ) in the average of all of the climate models featured in in the latest Intergovernmental Panel on Climate Change report , using the high-end warming scenario (RCP8.5). However, as the air warms its water-holding capacity increases, particularly over the oceans. According to the Clausius-Amazing metal dragon fire all over print stainless steel tumblerClapeyron equation, the air can generally hold around 7% more moisture for every 1C of temperature rise. As such, a world that is around 4C warmer than the pre-industrial era would have around 28% more water vapour in the atmosphere. Sea Breeze – An daytime coastal breeze that blows onshore, from the sea to the land. It is caused by the temperature difference when the surface of the land is warmer than the adjacent body of water. Predominate during the day, it reaches its maximum early to mid afternoon. It blows in the opposite direction of a land breeze. Erosion – The wearing away of the Earth’s surface by the action of the sea, running water, moving ice, precipitation or
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