|
|
| 1. |
Vertical Temperature Distribution in the Great Lakes |
| |
Journal of the Fisheries Board of Canada,
Volume 9,
Issue 7,
1952,
Page 325-328
H. B. Hachey,
Preview
|
PDF (151KB)
|
|
摘要:
On the basis of temperature observations made in the Great Lakes in the summer months it has been shown that: (a) the maximum depth of the thermocline does not exceed 50 feet, (b) the temperature gradient within the thermocline may be as much as 26 degrees Fahrenheit in 10 feet, (c) the thickness of the surface layer varies considerably with time and position, and can under certain circumstances be entirely removed from an area, and (d) the temperature of the deeper waters approximates to that of the maximum density of fresh water.
ISSN:0706-652X
DOI:10.1139/f52-017
出版商:NRC Research Press
年代:1952
数据来源: NRC
|
| 2. |
Surface Temperatures of the Great Lakes |
| |
Journal of the Fisheries Board of Canada,
Volume 9,
Issue 7,
1952,
Page 329-394
F. Graham Millar,
Preview
|
PDF (3355KB)
|
|
摘要:
Thermographs were installed on the condenser intakes of several steamships on the Great Lakes, with which the water temperature was recorded for five to ten years. Averages are presented in tables, maps, and diagrams. The temperature varies considerably over a lake surface in a manner determined by the depths and currents. Standard deviations and serial correlations are found for some of the data.
ISSN:0706-652X
DOI:10.1139/f52-018
出版商:NRC Research Press
年代:1952
数据来源: NRC
|
|
首页
