Orange County NC Website
US. Globall Change e wear,::[° IPirogirarr <br />46 <br />Trends in Peak Streamflow Timing <br />Observed Tr nds <br />1948 to 202 <br />q <br />x&200 saw 0 1,0,46d Wboo <br />-100 ealft, - 20d alt <br />fid <br />00" 20" 240' 260, <br />Projected Trends <br />by 2080, to 2099 <br />200, 220` 240" 260" <br />Stewart et al 157 <br />Top map shows changes in runoff timing in snowmelt- driven streams <br />from 1948 to 2002 with red circles indicating earlier runoff, and blue <br />circles indicating later runoff. Bottom map shows projected changes <br />in snowmelt- driven streams by 2080 -2099, compared to 1951 -1980, <br />under a higher emissions scenario 91 <br />runoff, in some cases up to 60 days earlier. 157,159 For <br />the Northeast, projections indicate spring runoff <br />will advance by up to 14 days .151 Earlier runoff <br />produces lower late - summer streamflows, which <br />stress human and environmental systems through <br />less water availability and higher water tempera - <br />tures.145 Scientific analyses to determine the causes <br />of recent changes in snowpack, runoff timing, and <br />increased winter temperatures have attributed these <br />changes to human - caused climate change .14,160,161 <br />Global Climate Change Impacts in the United States <br />Srwurlauu: aut;rwur qua1ity auuriur°1111 giirwarwuuuiur °1111 aut;rwur <br />qtjiaiinutity wflli Ill rw afft�ct( :NJ111 by au <br />r: ulliauuriilgiiiuuriug r:n111iiiinaut;r . <br />Changes in water quality <br />Increased air temperatures lead to higher water <br />temperatures, which have already been detected in <br />many streams, especially during low -flow periods. <br />In lakes and reservoirs, higher water temperatures <br />lead to longer periods of summer stratification <br />(when surface and bottom waters do not mix). <br />Dissolved oxygen is reduced in lakes, reservoirs, <br />and rivers at higher temperatures. Oxygen is an <br />essential resource for many living things, and its <br />availability is reduced at higher temperatures both <br />because the amount that can be dissolved in water <br />is lower and because respiration rates of living <br />things are higher. Low oxygen stresses aquatic <br />animals such as coldwater fish and the insects and <br />crustaceans on which they feed .14' Lower oxygen <br />levels also decrease the self - purification capabili- <br />ties of rivers. <br />The negative effects of water pollution, includ- <br />ing sediments, nitrogen from agriculture, disease <br />pathogens, pesticides, herbicides, salt, and ther- <br />mal pollution, will be amplified by observed and <br />projected increases in precipitation intensity and <br />longer periods when streamflows are 10w.146 The <br />U.S. Environmental Protection Agency expects the <br />number of waterways considered "impaired" by <br />water pollution to increase .16' Heavy downpours <br />lead to increased sediment in runoff and outbreaks <br />of waterborne diseases .161,164 Increases in pollution <br />carried to lakes, estuaries, and the coastal ocean, <br />especially when coupled with increased tempera- <br />ture, can result in blooms of harmful algae and <br />bacteria. However, pollution has the potential <br />of being diluted in regions that experience <br />increased streamflow. <br />Water - quality changes during the last century were <br />probably due to causes other than climate change, <br />primarily changes in pollutants .149 <br />Changes in groundwater <br />Many parts of the United States are heavily de- <br />pendent on groundwater for drinking, residential, <br />and agricultural water supplies .164 How climate <br />change will affect groundwater is not well known, <br />-, <br />6N <br />r� <br />o rye, <br />36O eadial, <br />101 1 5d1 War <br />. <br />01 2,545d eaMw <br />16 $5,25d�iww <br />y <br />40 <br />tD 154FA0 oaft, <br />0 25,45dIWIN <br />h °D <br />G � <br />1, <br />200, 220` 240" 260" <br />Stewart et al 157 <br />Top map shows changes in runoff timing in snowmelt- driven streams <br />from 1948 to 2002 with red circles indicating earlier runoff, and blue <br />circles indicating later runoff. Bottom map shows projected changes <br />in snowmelt- driven streams by 2080 -2099, compared to 1951 -1980, <br />under a higher emissions scenario 91 <br />runoff, in some cases up to 60 days earlier. 157,159 For <br />the Northeast, projections indicate spring runoff <br />will advance by up to 14 days .151 Earlier runoff <br />produces lower late - summer streamflows, which <br />stress human and environmental systems through <br />less water availability and higher water tempera - <br />tures.145 Scientific analyses to determine the causes <br />of recent changes in snowpack, runoff timing, and <br />increased winter temperatures have attributed these <br />changes to human - caused climate change .14,160,161 <br />Global Climate Change Impacts in the United States <br />Srwurlauu: aut;rwur qua1ity auuriur°1111 giirwarwuuuiur °1111 aut;rwur <br />qtjiaiinutity wflli Ill rw afft�ct( :NJ111 by au <br />r: ulliauuriilgiiiuuriug r:n111iiiinaut;r . <br />Changes in water quality <br />Increased air temperatures lead to higher water <br />temperatures, which have already been detected in <br />many streams, especially during low -flow periods. <br />In lakes and reservoirs, higher water temperatures <br />lead to longer periods of summer stratification <br />(when surface and bottom waters do not mix). <br />Dissolved oxygen is reduced in lakes, reservoirs, <br />and rivers at higher temperatures. Oxygen is an <br />essential resource for many living things, and its <br />availability is reduced at higher temperatures both <br />because the amount that can be dissolved in water <br />is lower and because respiration rates of living <br />things are higher. Low oxygen stresses aquatic <br />animals such as coldwater fish and the insects and <br />crustaceans on which they feed .14' Lower oxygen <br />levels also decrease the self - purification capabili- <br />ties of rivers. <br />The negative effects of water pollution, includ- <br />ing sediments, nitrogen from agriculture, disease <br />pathogens, pesticides, herbicides, salt, and ther- <br />mal pollution, will be amplified by observed and <br />projected increases in precipitation intensity and <br />longer periods when streamflows are 10w.146 The <br />U.S. Environmental Protection Agency expects the <br />number of waterways considered "impaired" by <br />water pollution to increase .16' Heavy downpours <br />lead to increased sediment in runoff and outbreaks <br />of waterborne diseases .161,164 Increases in pollution <br />carried to lakes, estuaries, and the coastal ocean, <br />especially when coupled with increased tempera- <br />ture, can result in blooms of harmful algae and <br />bacteria. However, pollution has the potential <br />of being diluted in regions that experience <br />increased streamflow. <br />Water - quality changes during the last century were <br />probably due to causes other than climate change, <br />primarily changes in pollutants .149 <br />Changes in groundwater <br />Many parts of the United States are heavily de- <br />pendent on groundwater for drinking, residential, <br />and agricultural water supplies .164 How climate <br />change will affect groundwater is not well known, <br />