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�n=30 <br /> During wetter rainfall periods, high nutrient <br /> loading from the watershed associated with <br /> high precipitation and stream flows can <br /> transport higher sediment and nutrient loads to <br /> Falls Lake. These events may increase <br /> flushing and reduce residence times. Figure 4 <br /> shows the Flat River nearly rising to the bridge <br /> deck following a high rainfall event. <br /> Periods of low loading from the watershed <br /> and to small inflows and longer Figure 4.Flat River rising near the bridge deck following a UNRBA <br /> correspond g High Flow Sampling Storm Event <br /> residence times when algae are provided <br /> longer periods for growth. Sporadic storm events that occur during periods of long detention can <br /> provide pulses of nutrients to Falls Lake that may remain stagnant in the lake for an extended time. <br /> The complex relationship between hydrologic condition, nutrient loading, and lake residence time <br /> means there is not a predictable cause-and-effect relationship between loading and algal growth. <br /> Figure 5 shows that in upper Falls Lake (upstream of Interstate 85), chlorophyll-a concentrations <br /> have been declining since the 1980s. This part of the lake historically had more variability in <br /> chlorophyll-a concentrations as demonstrated by the longer boxes and whiskers in Figure 5. <br /> Chlorophyll-a data were not <br /> collected in the upper lake <br /> between 2008 and 2012. Since 250- upper <br /> data collection restarted in 2013, 200- <br /> 150 - <br /> chlorophyll-a concentrations have 100 0 <br /> been relatively stable. The middle 50 <br /> part of the lake (between Interstate J ° <br /> M Idd le <br /> 85 and Highway 50) has lower ab 250 <br /> " <br /> chlorophyll-a concentrations and 200X50 <br /> less variability than the upper lake. a 100 <br /> Chlorophyll-a concentrations in this o 50 $7 d�—_ ��, $* Eli — <br /> segment have been relatively <br /> (� Lower <br /> stable since 2001. In the lower 250- <br /> 200- <br /> part <br /> 5020apart of the lake (downstream of 150 <br /> Highway 50), chlorophyll-a 100 <br /> concentrations have been relatively 50 <br /> stable over the life of the reservoir, IT 0 ID °� ���""�""°{�' ° �M C N� �r��"C °M <br /> rn rn!c rn rn rn m rn m rn T rn rn o 0 0 0 0 0 0©c 0 0 0 0 0 0 0 0 <br /> even in the 1980s when <br /> TT TTT <br /> concentrations in the upper lake Figure 5.Distribution of Chlorophyll-a Measurements in Upper Falls Lake <br /> (upstream of Interstate 85),Middle Falls Lake(between Interstate 85 and <br /> were much higher. During the Highway 50)and Lower Falls Lake(downstream of Highway 50 to the Dam) <br /> UNRBA 2014 to 2018 monitoring <br /> period, chlorophyll-a <br /> concentrations in Falls Lake were <br /> highest in 2017 (especially below Highway 50) compared to other UNRBA monitoring years, but <br /> nutrient loads that year were approximately half(see the following discussion of UNRBA Watershed <br /> Modeling for more information on this characteristic). <br /> 11 <br />