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Meteorological Data <br />Precipitation data ie collected lrom a Balfozt Weighing Bucket Rain Gaga situated ndj scent <br />to Sita SW-SZW-FG1. Data for this yeaz may be found in Table 1. Total monthly <br />precipitation data collected at this Pita alnca Water 7[aaz 1990 are presented in Table 2. <br />The Senaea II-W precipitation gage measured 28.25 inches this year. Thle valve is 9.98 <br />inches (554) greater than the 1990-1997 average. Temperature, rind speed, and direction <br />data from the Senacs II-W Meteorologic Station aza presented in ~^~~^+= H. <br />Data from the National Climatic Data Center for the Eayden Station rae uead to ewlvate <br />the precipitation trend. For this yeaz, 28.53 inches of precipitation rae meaeurad, xhich <br />rae 11.69 inrhee (694) greater than the 1961-1990 average. All months but December, <br />February, Mazch, end June rare above average. Snorpack runolf, ae estimated by totaling <br />November through April precipitation wlvea, ras 11.66 inches, xhiCh xne 3.25 inches (394) <br />above the 1961-1990 average. <br />Cround Water <br />Water Lawle. Water levels for all relle that aza in the current monitoring program aza <br />praaaated i.n Appandiz C. eydzogsapha o! all historic data for each cell aza presented <br />prior to the rater level raporte (Por all data since 1991) for each seepectiw sell in the <br />same appendix. Hy presenting all historic data, trends related to naaeonal and annual <br />variability are more clearly evident. Water level measurements aza taken rith an <br />electrical rater level indicator, or in the case of a fax shallox alluvial rolls, directly <br />from a steal tape. Site information, including sampling frequencies, is presented in <br />Table 3 (Appendiz A), S••~^^~ry o! Ground Wstar Monitoring Walls. Gzound rates level <br />monitoring frequencies aza listed on Page 15-3-3 of the Seneca II-W PAP. <br /> <br />• <br />Alluvium. Tha alluvial monitoring Wells W8AL6-1, 6-2, 6-3, 6-~, and 7-2 aza located along <br />eubbareon Gulrh. All relle azhibit rates level seaeonsl vazintrona typical for the <br />alluvium, i.e., ehallor alias the eprinq xerhazge, deepening toxazds the fall. Water <br />levels at Wells 6-1 to 6-3 aza nor higher than they rould normally ba in May through July <br />due to recently intzoducad (May, 1989) irrigation in that area. Well WRAL10 is situated <br />approzimataly one-half mile domstream of the NPDE9 006 pond on a tributary to eubberaon <br />2 <br />