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<br />Stlrren: Initial operation of the system showed <br />that temperature gradients were established from <br />the coil to the water surface. The gradient caused <br />only a slight decrease of 1-2 degrees on the water <br />surface with a decrease of 5-15 degrees next to the <br />coils. Wilkins-Anderson (Waco Supreme) labora- <br />tory stirrers were therefore installed on the side of <br />the pan to circulate (destratify) the cooled water <br />uniformly. The slow-speed. two-bladed prop <br />caused nlinimal surface disturbances in a small <br />area adjacent to the shaft. A stirrer was also <br />mounted on the normal pan to keep conditions <br />uniform between the three pans. These stirrers <br />eliminated the temperature gradient and kept the <br />pans constantly mixed. <br /> <br />Temperature recording <br /> <br />Re<Order: A Sanborn eight channel D.C. <br />amplifier recorder was used to monitor air and <br />water temperatures. It featured general purpose <br />resistance measurements and recording on eight <br />separate 5 centimeter channels fed from a single <br />roll chart. A timing circuit was connected to the <br />Sanborn recorder to take readings at 20 minute <br />intervals. All eight channels were used to monitor <br />resistances for these temperatures as follows: <br /> <br />1. North pan surface temperature <br /> <br />2. North pan bottom temperature <br /> <br />3. Center pan bottom temperature <br /> <br />4. Cenler pan surface temperature <br /> <br />5. South pan surface temperature <br /> <br />6. South pan bottom temperature <br /> <br />7. Air temperature <br /> <br />8. Dew point <br /> <br />Channel calibrations were made in DC to allow the <br />reading of temperatures directly from the chart. <br /> <br />ThermIBton: Yellow Springs Instrument <br />Thermistors (No. 44033) were used for all <br />temperature measurements. The air temperature <br />thennistors was placed inside an instrument shelter <br />and all of the water temperature thermistors were <br />mounted on brackets 1 inch away from the side of <br />lhe pan. The surface thermistor was approximately <br />I inch below the water surface; the bottom <br />thermistor was 1 inch above the cooling coils. The <br />thermistors were mounted on the shady side of the <br />pan to avoid any direct solar radiation. All <br />thermistors and electrical equipment were con- <br /> <br />necled to a coaxial cable which linked them to the <br />Sanborn recorder and power supplies. housed in a <br />nearby equipment shed. <br /> <br />CaIlbradoD: All eight channels were calibrated <br />at the start of a daily recor~. A resistance circuit <br />was designed to cover the daily temperature ranges. <br />These resistances came from calibration curves <br />included with each thermistor. Readings were <br />initially tested against accurate thermometers. The <br />verified calibration marks were recorded daily for <br />each channel. <br /> <br />Dew point <br /> <br />The dew point was measured with a CoR <br />Hygrometer which was also connected to the <br />Sanborn recorder. This unit operated on the <br />controlled resistance of a lithium chloride film. It <br />has a dew point range of -20DC to +30DC with an <br />accuracy of :t.5DC. The hygrometer was kept in the <br />sun screen shelter along with the air temperature <br />thermistor. Temperature readings taken from the <br />LiCI film were used in a conversion chart to get the <br />dew point value. <br /> <br />PreclpltadoD <br /> <br />A Belfort weighing recording rain gage was <br />used to monitor precipitation at the station. A <br />7-day trace was examined once a week during the <br />dry weather. but charts were removed after every <br />storm with significant precipitation. <br /> <br />Wind <br /> <br />A circular-dial, three cup Belfort Anemometer <br />was used to record total wind in miles per day. The <br />anemometer was mounted on the center evapora- <br />tion pan platform at the 2-foot level. The wind <br />movement, recorded mechanically on two circular <br />scales. was read once a day. A small, four cup <br />anemometer and electronic counter were also <br />installed initially but were removed after the <br />Belfort calibration was verified. <br /> <br />Empirical .Dpp.....loD resullll <br /> <br />The evaporation station was operational and <br />recording on August 19, 1974. Records were <br />maintained until the night time temperatures <br />dropped to freezing, which was up through <br />October 25, 1974. A table of the recorded data is <br />listed in Appendix B. <br /> <br />Every three consecutive temperatlii~ measure- <br />ments from the recorder chart were averaged <br />together for one hourly value. The pan water <br />temperature, air temperature, and dew point were <br /> <br />16 <br />