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<br />Water Temperature - CHLP experienced an unusually wann March in 2004. Surface water <br />temperatures reached 18.C nearly 3 weeks earlier compared to the two previous years (Figure 2). <br />Bonytail have spawned in past years when surface temperatures reached 18.C. They did again <br />this year, nearly a month earlier. <br /> <br />Surface temperatures ranged between 12 and 34.C, reaching the highest temperatures in July <br />(Figure 3). The coolest temperature during that month was 30.8.C. Minimum water <br />temperatures by the end of July exceeded 30.C at all depths. Daily temperatures fluctuated <br />2-3'C between day and night cycles, reaching highs in mid-afternoon and lows near dawn. The <br />combination of water influx from the river and the diel temperature cycle may help prevent <br />strong thermal or chemical stratification from developing. <br /> <br />1-+-2002 -- 2003 -- 20041 <br /> <br />35 <br />30 ------ <br /> <br />26 <br />~24 <br />-22 <br />'" <br />;; 20 <br />~18 <br />:.; 16 <br />c.. <br />E 14 <br />~12 <br />10 <br /> <br /> <br />~ 25 <br /> <br />f 20 <br />~ <br />... <br />:;; 15 <br /><>. <br />~ 10 <br />I- <br /> <br />-,;-: . <br /> <br />-+- Jan-27 <br />__ Feb-24 <br />__Mar-10 <br />-'>E- Apr-26 <br />__ May-4 <br />-+-May-19 <br />-+- Jun-23 <br />- Jul-27 <br /> <br /> <br />..... <br /> <br />5 <br />o . <br /> <br />~ ~ ~ ~ ~~ .~ .~ :~ <br /><<.~ ~'Ii ~~ ~'l><: ~<::i. ~<::$: ~<::$: ~<::$: <br />Time afYear <br /> <br />c.,<b <br />~'Ii <br />~~ <br /> <br />.... <br /> <br />'" <br /> <br />n, <br /> <br />Depth (m) <br /> <br />Figure 2. Surface water temperatures <br />taken at Cibola High Levee Pond <br />during 2002, 2003 and 2004 (February <br />through April). <br /> <br />Figure 3. Water column temperatures <br />taken at 0.5 m intervals at Cibola <br />High Levee Pond spawning period <br />during 2004. <br /> <br />Dissolved Oxygen - Dissolved oxygen levels at CHLP stayed remarkably high during summer <br />months. More than 95% ofthe pond's volume maintained levels over 6 mg/L (Figure 4). We <br />did not find any evidence of anoxic conditions. The lowest concentration was 3 mg/L; this is <br />more than sufficient to support fish. <br /> <br />.. <br /> <br />Oxygenation is influenced by a combination of factors, possibly the most important stemming <br />from the pond's hydraulic connection with the river. Low conductances at greater depths <br />suggest that groundwater upwelling provides circulation that helps prevent stagnation. Another <br />contributing factor may be the diel temperature fluctuation (2-30C) that may partially disrupt <br />stratification. This high level of oxygenation undoubtedly contributes to the pond's high level of <br />productivity. <br /> <br />3 <br />