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CFE agenda 091117
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CFE agenda 091117
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9/11/2017
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CFE minutes 091117
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US. GIoball CI °Harm^ eseairm::[° IPirogirarn <br />44 <br />along the downwind coasts of the Great Lakes <br />have increased. Factors contributing to this <br />increase include reduced ice cover due to <br />warming, which lengthens the period of open <br />water. In addition, cold air moving over rela- <br />tively warm, open lake water induces strong <br />evaporation, often causing heavy lake - effect <br />snow. Heavy snowfall and snowstorm fre- <br />quency have increased in many northern parts <br />of the United States. In the South however, <br />where temperatures are already marginal for <br />heavy snowfall, climate warming has led to <br />a reduction in heavy snowfall and snowstorm <br />frequency. These trends suggest a northward <br />shift in snowstorm occurrence .61 <br />Global Climate Change Impacts in the United States <br />Increases in the Number of Days with <br />Very Heavy Precipitation (1958 to 2007) <br />iinurea,ses in Annual Number of Day <br />III °�IIIoo(1111 II�II�1111 ( "111111ro��111�'llhit� �u�llr(n Illlillllr���nlll to <br />�I <br />coIllmrm Illmrmo11 coII "mrmlllmrmollrll airld1 Illmrmo11 0 10% 11-20% 21-30% 31 .40,x, 41 - %)'% 51-60% <br />firlt(:NIIIS(r 'as rf ^Ir)('IIIoIIII "III�1 airld crasoirlai U..)lsclatecl furorrr Guroir.•,rrrari e�t crl,. <br />1''' <br />rll�'fIkrf���llll '� Ilit�� �t��lll�� IIII "III att(l�Ilrlllrlll (�:111allll"III)((� , �Illrllld" The map shows the percentage increases in the average number <br />r�lllllll "III'��� fP��rf���l��IIP " "rifP��r IIP " "ri��IlrfP��r f���l��IIII "Illf���lf�P��rllll "III ���IIr����f�P��rr "a of days with very heavy precipitation (defined as the heaviest <br />I percent of all events) from 1958 to 2007 for each region. There <br />IIIII"IIIto I'7iitlr tlr tlNrlllt IIItlii loIllrlll)('t'rlr, are clear trends toward more days with very heavy precipitation <br />l'fott(PNlr fair p(PNlrlllor "ally IIIIIII "Ill (PA (PNPNlll"Ill ). for the nation as a whole, and particularly in the Northeast <br />and Midwest. <br />While it sounds counterintuitive, a warmer <br />world produces both wetter and drier conditions. <br />Even though total global precipitation increases, the <br />regional and seasonal distribution of precipitation <br />changes, and more precipitation comes in heavier <br />rains (which can cause flooding) rather than light <br />events. In the past century, averaged over the <br />United States, total precipitation has increased by <br />about 7 percent, while the heaviest 1 percent of rain <br />events increased by nearly 20 percent.68 This has <br />been especially noteworthy in the Northeast, where <br />the annual number of days with very heavy precipi- <br />tation has increased most in the past 50 years, as <br />shown in the adjacent figure. Flooding often occurs <br />when heavy precipitation persists for weeks to <br />months in large river basins. Such extended periods <br />of heavy precipitation have also been increasing <br />over the past century, most notably in the past two <br />to three decades in the United States .112 <br />Observations also show that over the past several <br />decades, extended dry periods have become more <br />frequent in parts of the United States, especially <br />the Southwest and the eastern United States .146,147 <br />Longer periods between rainfalls, combined with <br />higher air temperatures, dry out soils and vegeta- <br />tion, causing drought. <br />For the future, precipitation intensity is projected <br />to increase everywhere, with the largest increases <br />occurring in areas in which average precipitation <br />increases the most. For example, the Midwest and <br />Northeast, where total precipitation is expected <br />to increase the most, would also experience the <br />largest increases in heavy precipitation events. The <br />number of dry days between precipitation events <br />is also projected to increase, especially in the more <br />and areas. Mid - continental areas and the Southwest <br />are particularly threatened by future drought. The <br />magnitude of the projected changes in extremes is <br />expected to be greater than changes in averages, <br />and hence detectable sooner .49,61,90,142,148 <br />
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