The considerable influence of the masses of water in the Great Lakes on the weather over and around the Lakes is reviewed and the average lake-related weather alterations are indicated. Particular emphasis is placed on delineating the known facts and those that are inadequately known. The lack of extensive continuous weather measurements, particularly over the lakes, makes definitive areal assessments of lake influences on the weather around them difficult. Whether the lakes act as the energy sources or sinks on a daily or seasonal basis depends on the relative temperature of the waters and the overlying air. Over the lakes and their downwind shore areas, the lake-caused average changes in cloud and precipitation amounts represent 5–15% reductions in summer and 5–45% increases in winter in comparison with upwind values.
[1]
P. C. Day.
PRECIPITATION IN THE DRAINAGE AREA OF THE GREAT LAKES, 1875–1924
,
1926
.
[2]
W. Hoppel,et al.
Electrification processes over Lake Superior
,
1970
.
[3]
S. Changnon.
Precipitation climatology of Lake Michigan Basin
,
1968
.
[4]
H. C. Willett.
American air mass properties
,
1933
.
[5]
Val L. Eichenlaub.
Lake Effect Snowfall to the Lee of the Great Lakes: Its Role in Michigan.
,
1970
.
[6]
B. G. Decooke,et al.
Comparison of precipitation on islands of Lake Michigan with precipitation on the perimeter of the lake
,
1960
.
[7]
S. Petterssen,et al.
ON SOME WEATHER INFLUENCES DUE TO WARMING OF THE AIR BY THE GREAT LAKES IN WINTER
,
1959
.