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<br /> <br />0020gS <br /> <br />w <br />0: <br />=> <br />t- <br />~V> <br />~2 <br />ifi::J <br />>-ws <br />0:0 <br />~ffi <br /><(w <br />;00: <br />zlB <br /><1i 0 0 <br />;:o'!; <br />o - <br />z~ <br />o <br />~ -s <br />J: <br /> <br />~.20 <br />u; <br />u:l <br />o <br />ffl <br />w <br />~ IS <br />w <br />o <br />'!; <br /> <br />310 <br />w <br />o <br />=> <br />t- <br />12 <br />~ S <br /> <br />3.0 <br />V> <br />z <br /><( <br />Ci 2.8 <br />~ <br />z <br />-:: 2.6 <br />~ <br />~2.4 <br />to <br />~ <br />~2.2 <br />J: <br />.. <br />2.0 <br />SOOO <br /> <br />ALTITUDE, IN METERS ABOVE MEAN SEA LEVEL <br />1600 1800 2000 2200 2400 2600 2800 3000 <br />10 <br /> <br /> <br />. <br /> <br />M = 20.8 - 0.0022x <br />(altitude in feet) <br /> <br />. <br /> <br />Correlation coefficient <br />(r) =0.80 <br />Standard error of estimate <br />ISe)=1.6 <br /> <br />. <br /> <br /> <br /> <br />Regression line <br />Ir =0.20} <br />(Se=2.31 <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />Mean (Ai = 10.0 <br />Standard deviation <br />S)-2.3 <br /> <br />. .. ... . <br /> <br />. <br /> <br />. .. <br />. <br />..-r <br />. <br /> <br />. <br /> <br /> <br />.. <br /> <br /> <br />. <br /> <br />. <br /> <br />.. ... <br /> <br />Mean 1(")=2.6 <br />IS 0.09S) <br /> <br />. <br /> <br />. <br /> <br />. ... <br />Regression line <br />(r=0.60) <br />ISe= 0.078) <br /> <br />. <br /> <br />. <br /> <br /> <br />6000 7000 8000 9000 10,000 <br />ALTITUDE, I N FEET A80VE MEAN SEA LEVEL <br /> <br />Figure 4.-- Relationships between stream- temperature <br />harmonic- analysis coefficients and altitude for <br />streams in the Yampa River basin, 1960-75. <br /> <br />20 <br /> <br />.' <br />