The contribution of evaporation from the Great Lakes to the continental atmosphere: estimate based on stable isotope data
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Abstract
The isotopic composition of precipitation and river runoff in the vicinity of the North American Great Lakes is characterized by a higher deuterium-excess value than observed in the advecting air masses. It is suggested that this indicates that evaporated moisture from the surface waters is mixed with the atmosphere waters. A preliminary estimate of the atmospheric water balance during summer and autumn indicates that between 4.6%–15.7% of the atmospheric water content downwind from the Great Lakes is derived from lake evaporation during summer.
Suggested Citation
Gat, J.R., Bowser, C.J., Kendall, C., 1994, The contribution of evaporation from the Great Lakes to the continental atmosphere: estimate based on stable isotope data: Geophysical Research Letters, v. 21, no. 7, p. 557-560, https://doi.org/10.1029/94GL00069.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | The contribution of evaporation from the Great Lakes to the continental atmosphere: estimate based on stable isotope data |
| Series title | Geophysical Research Letters |
| DOI | 10.1029/94GL00069 |
| Volume | 21 |
| Issue | 7 |
| Publication Date | December 07, 2012 |
| Year Published | 1994 |
| Language | English |
| Publisher | Wiley |
| Description | 4 p. |
| First page | 557 |
| Last page | 560 |