Concerning the Deposition and Diagenesis of Strata in Polar Firn
Abstract Depth hoar in polar firn forms when large temperature gradients act on low-density firn, but high-density firn does not develop into depth hoar. Low densities in firn may be depositional (burial of surface hoar or still-air snowfall) or diagenetic (mass loss to the free atmosphere, typicall...
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Cambridge University Press (CUP)
1988
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Online Access: | http://dx.doi.org/10.1017/s0022143000007024 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007024 |
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crcambridgeupr:10.1017/s0022143000007024 2024-09-15T18:15:39+00:00 Concerning the Deposition and Diagenesis of Strata in Polar Firn Alley, Richard B. 1988 http://dx.doi.org/10.1017/s0022143000007024 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007024 en eng Cambridge University Press (CUP) Journal of Glaciology volume 34, issue 118, page 283-290 ISSN 0022-1430 1727-5652 journal-article 1988 crcambridgeupr https://doi.org/10.1017/s0022143000007024 2024-07-10T04:04:37Z Abstract Depth hoar in polar firn forms when large temperature gradients act on low-density firn, but high-density firn does not develop into depth hoar. Low densities in firn may be depositional (burial of surface hoar or still-air snowfall) or diagenetic (mass loss to the free atmosphere, typically in autumn); however, diagenesis is sufficiently strong to cause significant mass loss only in the top 50–100 mm of firn. Between about 50–100 mm and 2 m depth, grain growth and densification are accelerated strongly by temperature-gradient effects; from 2 to 5 m, temperature gradients have a small but measurable effect on rates of processes in firn, and below 5 m rates essentially have isothermal values. Diagenetic depth-hoar layers typically develop in the autumn, are relatively thick, and have smooth bases. Depositional depth-hoar layers may develop at any season, are relatively thin, and have irregular bases. In low-accumulation regions, visual stratification may preserve only an annual signal, but in high-accumulation regions individual storms or other features may be recognizable. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 34 118 283 290 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Depth hoar in polar firn forms when large temperature gradients act on low-density firn, but high-density firn does not develop into depth hoar. Low densities in firn may be depositional (burial of surface hoar or still-air snowfall) or diagenetic (mass loss to the free atmosphere, typically in autumn); however, diagenesis is sufficiently strong to cause significant mass loss only in the top 50–100 mm of firn. Between about 50–100 mm and 2 m depth, grain growth and densification are accelerated strongly by temperature-gradient effects; from 2 to 5 m, temperature gradients have a small but measurable effect on rates of processes in firn, and below 5 m rates essentially have isothermal values. Diagenetic depth-hoar layers typically develop in the autumn, are relatively thick, and have smooth bases. Depositional depth-hoar layers may develop at any season, are relatively thin, and have irregular bases. In low-accumulation regions, visual stratification may preserve only an annual signal, but in high-accumulation regions individual storms or other features may be recognizable. |
format |
Article in Journal/Newspaper |
author |
Alley, Richard B. |
spellingShingle |
Alley, Richard B. Concerning the Deposition and Diagenesis of Strata in Polar Firn |
author_facet |
Alley, Richard B. |
author_sort |
Alley, Richard B. |
title |
Concerning the Deposition and Diagenesis of Strata in Polar Firn |
title_short |
Concerning the Deposition and Diagenesis of Strata in Polar Firn |
title_full |
Concerning the Deposition and Diagenesis of Strata in Polar Firn |
title_fullStr |
Concerning the Deposition and Diagenesis of Strata in Polar Firn |
title_full_unstemmed |
Concerning the Deposition and Diagenesis of Strata in Polar Firn |
title_sort |
concerning the deposition and diagenesis of strata in polar firn |
publisher |
Cambridge University Press (CUP) |
publishDate |
1988 |
url |
http://dx.doi.org/10.1017/s0022143000007024 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007024 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 34, issue 118, page 283-290 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000007024 |
container_title |
Journal of Glaciology |
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34 |
container_issue |
118 |
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283 |
op_container_end_page |
290 |
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1810453536540983296 |