RESEARCH· ·1970·
RESEARCH· ·1970·
RESEARCH· ·1970·
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B218<br />
SURFACE WATER<br />
TABLE 4.-Variation in regression coefficients of annual precipitation, in millimeters/year, with length of record<br />
Station name<br />
20 40 60<br />
Length of record (years)<br />
80 100 120 140 160 180<br />
Adelaide, Australia _________ -5.37 -0.407 0. 211<br />
Ban galore, India ___________ 3. 05 5. 23 . 988<br />
Copenhagen, Denmark _____ 9. 39 2. 63 1. 15<br />
Milan, Italy----___________ 10.6 4. 00 -1. 31<br />
Portsmouth, Ohio ________ -- 1. 23 -2.30 . 450<br />
St. Paul, Minn ____________ -5.28 . 0142 -2.30<br />
-0.0729 -0.276<br />
1. 11 . 376 -0. 0079<br />
. 958 . 775 . 496 0. 314<br />
-1.93 -. 746 -1. 19 -. 794 -0. 580 -0. 219<br />
. 345 . 691 . 395<br />
-1.27 -1.30 -. 645<br />
conclusions by several investigators that trends .are not<br />
generally apparent in runoff for streams in the United<br />
States since about the turn of the century. A study by<br />
Y evdjevich ( 1963) has indicated that runoff in Europe<br />
and the United States inay be trend free since at least<br />
1810.<br />
There is strong evidence that temperature trends<br />
exist. Temperature trends 1nay imply evapotranspiration<br />
trends. However, observed tmnperature trends<br />
have been sinall, about 1 °F over the 60-year period<br />
1880-1940. The effects on runoff of such a small temperature<br />
trend are probably not significant.<br />
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