On the Transfer of Visible Radiation through Sea Ice and Snow
Abstract Coefficients of absorption of visible radiation are determined for sea ice and snow as a function of porosity of the medium and wave-length of energy refracted into it. A comparison is made between the values derived and those obtained by other investigators under similar snow conditions. A...
| Published in: | Journal of Glaciology |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Cambridge University Press (CUP)
1963
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0022143000027921 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027921 |
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crcambridgeupr:10.1017/s0022143000027921 |
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openpolar |
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crcambridgeupr:10.1017/s0022143000027921 2024-09-15T18:15:39+00:00 On the Transfer of Visible Radiation through Sea Ice and Snow W. Thomas, Charles 1963 http://dx.doi.org/10.1017/s0022143000027921 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027921 en eng Cambridge University Press (CUP) Journal of Glaciology volume 4, issue 34, page 481-484 ISSN 0022-1430 1727-5652 journal-article 1963 crcambridgeupr https://doi.org/10.1017/s0022143000027921 2024-07-31T04:04:28Z Abstract Coefficients of absorption of visible radiation are determined for sea ice and snow as a function of porosity of the medium and wave-length of energy refracted into it. A comparison is made between the values derived and those obtained by other investigators under similar snow conditions. A difference in results suggests a significant rôle of crystal size and orientation in the absorption properties of sea ice and snow. Article in Journal/Newspaper Journal of Glaciology Sea ice Cambridge University Press Journal of Glaciology 4 34 481 484 |
| institution |
Open Polar |
| collection |
Cambridge University Press |
| op_collection_id |
crcambridgeupr |
| language |
English |
| description |
Abstract Coefficients of absorption of visible radiation are determined for sea ice and snow as a function of porosity of the medium and wave-length of energy refracted into it. A comparison is made between the values derived and those obtained by other investigators under similar snow conditions. A difference in results suggests a significant rôle of crystal size and orientation in the absorption properties of sea ice and snow. |
| format |
Article in Journal/Newspaper |
| author |
W. Thomas, Charles |
| spellingShingle |
W. Thomas, Charles On the Transfer of Visible Radiation through Sea Ice and Snow |
| author_facet |
W. Thomas, Charles |
| author_sort |
W. Thomas, Charles |
| title |
On the Transfer of Visible Radiation through Sea Ice and Snow |
| title_short |
On the Transfer of Visible Radiation through Sea Ice and Snow |
| title_full |
On the Transfer of Visible Radiation through Sea Ice and Snow |
| title_fullStr |
On the Transfer of Visible Radiation through Sea Ice and Snow |
| title_full_unstemmed |
On the Transfer of Visible Radiation through Sea Ice and Snow |
| title_sort |
on the transfer of visible radiation through sea ice and snow |
| publisher |
Cambridge University Press (CUP) |
| publishDate |
1963 |
| url |
http://dx.doi.org/10.1017/s0022143000027921 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027921 |
| genre |
Journal of Glaciology Sea ice |
| genre_facet |
Journal of Glaciology Sea ice |
| op_source |
Journal of Glaciology volume 4, issue 34, page 481-484 ISSN 0022-1430 1727-5652 |
| op_doi |
https://doi.org/10.1017/s0022143000027921 |
| container_title |
Journal of Glaciology |
| container_volume |
4 |
| container_issue |
34 |
| container_start_page |
481 |
| op_container_end_page |
484 |
| _version_ |
1810453584479780864 |