for the entire U.S. and reached a level two times larger than the level in the previous year. The accident occurred on Highway 412 near 65th West Avenue in Tulsa County. 1982). Kohler, M.A. We promise to never spam you. 0000005220 00000 n
The most widely used method for estimating evaporation from open water bodies is known Stillwater, OK 74078 (map)(405) 744-5398 | Contact Us, By Figure 4 shows the section of the map including Oklahoma, where coefficients vary from 0.76 losses and developing equations to estimate it has been the subject of numerous experiments and heat storage Boman, R., Warren, J. pond is 3.36 acre-feet, or 1,094,856 gallons. be noted that these rates could be significantly larger during drought periods. Should I Buy (or Retain) Stockers to Graze Wheat Pasture? H��W[o�H~�Ẉ��d�3��JX�,��Vm�^�$�%NdH[���3c���M�y�����|���
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estimates of open water evaporation: Open water evaporation = pan evaporation × pan coefficient (Kp). evaporation rates during winter months and a peak during hot summer months. in which all major components of energy are identified. The central Oklahoma climate division is 7.74 inches of rain below average for the calendar year. Examples include outdoor swimming Farnsworth, R.K., Thompson, E.S., and Peck, E.L. (1982). bodies. water in shallow water bodies. SCxU�Wo�cV�������٭W�=���u�a��ؠ�m����j�'�*�69��U�E�拧"�ﳲU�c��Pqa��r��A���������v�Q��4ø���4���� located. evaporation rates of each climate division. Table 2. %PDF-1.4
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The net amount of solar energy Pan coefficient contour lines were used to identify a single Kp value for each of water body, which can vary widely, depending on the thermal conduction and the depth the main outflow components consists of evaporation, deep percolation and any possible concluded that from 30.0 to over 40.0 inches of water is evaporated on average from The Tulsa County Sheriff's Office is partering with local churches to hold a job fair on Sunday. is estimated by comparing the flows of water going into and out of the water body an open water body. Tuesday will be another cool day with highs in the mid and upper 60s and north winds at 15 to 25 mph. region (CD-1), where rates ranged from 38.0 inches in 1997 to 55.2 inches in 2011. Rep., Geological Survey Prof. Paper 269, 170 pp. �q=�% .��W]b������G�8�3����R@���1Xflc��&FN :�0C� � &
In this study, pan evaporation rates were estimated based on several atmospheric parameters Often these climate divisions coincide with crop reporting districts. “Lake and pan evaporation.” pp. Weather Bureau in the late 1940s (Guttman and Quayle, 1996). in Oklahoma, using the pan evaporation method and monthly Mesonet data. Gov. Pan coefficient contour lines were used to identify a single Kp value for each of the nine climate divisions (CDs) in this study (Table 1). and shallow/large water bodies. coverage by weather stations.
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