| Reference Type | Journal (article/letter/editorial) |
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| Title | Cryoconite hole thermodynamics |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | McIntyre, N. F. | Author |
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| Year | 1984 (February 1) | Volume | 21 |
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| Issue | 2 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e84-016Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 478170 | Long-form Identifier | mindat:1:5:478170:1 |
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| GUID | 0 |
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| Full Reference | McIntyre, N. F. (1984) Cryoconite hole thermodynamics. Canadian Journal of Earth Sciences, 21 (2) 152-156 doi:10.1139/e84-016 |
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| Plain Text | McIntyre, N. F. (1984) Cryoconite hole thermodynamics. Canadian Journal of Earth Sciences, 21 (2) 152-156 doi:10.1139/e84-016 |
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| In | (1984, February) Canadian Journal of Earth Sciences Vol. 21 (2) Canadian Science Publishing |
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| Abstract/Notes | Energy sources governing the growth of cryoconite holes have been investigated by monitoring the meteorological balance at the surface of the Manatee Glacier, British Columbia, the dimensions of 125 holes, and the thermal conditions within them. Cryoconite holes are shown to be rough indicators of the energy balance at the glacier surface. Both atmospheric and biological energy sources operate, thereby suggesting a genetic classification of holes with "solar" and "biological" end members. |
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