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ClimateChange Assessment Guide.pdf - University of Waterloo

ClimateChange Assessment Guide.pdf - University of Waterloo

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Background9Table 2.3 Projected changes in global climate as they relate to water (Bates et al., 2008; Meehl et al., 2007)Projected Changes• Hot extremes and heat waves will very likely be more intense, frequent and longer in duration.• Number <strong>of</strong> frost days in middle and high latitudes decrease and growing season lengthens.• Increased likelihood <strong>of</strong> summer drying in mid-latitudes and associated risk <strong>of</strong> drought (increasing from 1% <strong>of</strong>present-day land area to 30% by 2100).• Increase in number <strong>of</strong> consecutive dry days.• Very likely that heavy precipitation events will become more frequent.• Increase in the amount and intensity <strong>of</strong> precipitation at high latitudes and in tropics; decreases in some subtropicaland lower mid-latitude regions.• Area <strong>of</strong> snow cover projected to contract, glaciers/ice caps lose mass; in many areas summer melting is greaterthan winter snowfall accumulation.• By 2050, permafrost area in Northern Hemisphere likely to decrease 20-35%; increases in thaw depth.• Potential evaporation projected to increase (atmosphere’s water-holding capacity increases with highertemperatures but relative humidity stays same); increase in water vapour deficit.• Run<strong>of</strong>f increases in high latitudes and wet tropics, decreases in mid-latitudes and some parts <strong>of</strong> dry tropics.Impacts <strong>of</strong> climate change occur due to changes inmean conditions and changes in variability includingthe sequence, frequency, duration and intensity <strong>of</strong>extreme events. Extreme events, rather than changes inmean conditions, are <strong>of</strong>ten more relevant to assessingthe impacts <strong>of</strong> a changing climate. This is becausebiophysical and human systems are more likely tosuffer harm from these extreme events which are <strong>of</strong>tenoutside coping capacity, than from changes in themean conditions. Some projected changes in extremeevents, and their likelihood <strong>of</strong> occurring, are summarizedin Table 2.4. Note that the IPCC has developedterminology to clarify uncertainty by relating confidencein being correct to the likelihood <strong>of</strong> an occurrence oroutcome; these findings use that language.A changing climate is likely to affect global wateravailability; many regions that are already hydrologicallychallengedwill experience further stress with climatechange. But how will Ontario fare in the future?

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