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Figure 8 <br />$5,000 <br />e <br />0 <br />September - Oember <br />Green River disharge at Jensen, Utah 1981 <br />• <br />Figure 9 <br />E. <br />u <br />E <br />= 1 <br />a <br />o <br />P R PO P R PO P R PO P R PO P R- PO -P =R --PO <br />0 <br />A B C D E F <br />STRATA <br />Mean depth by strata and runoff period (P=prerunof£, R7-runoff, <br />PO=postrunof£). Green River, Utah, June 1979 - June 1981. <br />and colder than other strata due to shading from canyon walls. No dis- <br />cernible pattern was identified among mean conductivity and turbidity for <br />each stratum during a given sampling period (Table 6). However, differ- <br />ences occurred between sampling periods for most strata. Conductivities <br />were much lower (x = 324) during runoff than during prerunoff (x = 666) <br />or postrunoff (x = 760). Conversely, except for strata B and F, turbidi- <br />ties were higher during runoff than during pre- or postrunoff. Increased <br />24