Orange County NC Website
Attachment 6 <br />Changes in the water cycle, which are consistent <br />with the warming observed over the past several <br />decades, include: <br />• changes in precipitation patterns and intensity <br />• changes in the incidence of drought <br />• widespread melting of snow and ice <br />• increasing atmospheric water vapor <br />• increasing evaporation <br />• increasing water temperatures <br />• reductions in lake and river ice <br />• changes in soil moisture and runoff <br />For the future, marked regional differences are <br />projected, with increases in annual precipitation, <br />runoff, and soil moisture in much of the Midwest <br />and Northeast, and declines in much of the West, <br />especially the Southwest. <br />Skagit River and surrounding mountains in the Northwest <br />The impacts of climate change include too little wa- <br />ter in some places, too much water in other places, <br />and degraded water quality. Some locations are ex- <br />pected to be subject to all of these conditions during <br />different times of the year. Water cycle changes are <br />expected to continue and to adversely affect energy <br />production and use, human health, transportation, <br />agriculture, and ecosystems (see table on page 50).14' <br />(:Iii �uruilp'c� IIii as aIir(M(Jy Illtc� urc� c]1 �uruicl9 <br />ii III III r:oirit;iiiuuriiuu( to aulllt( ur, t;llu at( it c r::lie, <br />fft :ut;iii ouruul„ wlu ir(:�, l u urii, au urii x°1 how ui'' uu r: li <br />autcflr is au auiiilllauJll Iii f6ir aullllll us( . <br />Substantial changes to the water cycle are expected <br />as the planet warms because the movement of water <br />in the atmosphere and oceans is one of the primary <br />mechanisms for the redistribution of heat around the <br />world. Evidence is mounting that human - induced <br />climate change is already altering many of the exist- <br />ing patterns of precipitation in the United States, <br />including when, where, how much, and what kind of <br />precipitation falls .61,14' A warmer climate increases <br />evaporation of water from land and sea, and allows <br />more moisture to be held in the atmosphere. For ev- <br />ery PF rise in temperature, the water holding capac- <br />ity of the atmosphere increases by about 4 percent .49 <br />41 <br />