The Summer Climate in the Accumulation Area of the Salmon Glacier

Abstract During the summer of 1957 a party visited the Salmon Glacier in British Columbia. A meteorological station was established in the accumulation area at an altitude of 1700 m. From 12 June to 16 August pressure, temperature and humidity were recorded continuously and the daily totals of preci...

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Published in:Journal of Glaciology
Main Author: Adkins, C. J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1958
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000024242
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024242
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spelling crcambridgeupr:10.1017/s0022143000024242 2024-03-03T08:46:00+00:00 The Summer Climate in the Accumulation Area of the Salmon Glacier Adkins, C. J. 1958 http://dx.doi.org/10.1017/s0022143000024242 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024242 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 23, page 194-206 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1958 crcambridgeupr https://doi.org/10.1017/s0022143000024242 2024-02-08T08:40:23Z Abstract During the summer of 1957 a party visited the Salmon Glacier in British Columbia. A meteorological station was established in the accumulation area at an altitude of 1700 m. From 12 June to 16 August pressure, temperature and humidity were recorded continuously and the daily totals of precipitation, ablation and percolation were obtained. Periodic measurements of snow density were made; on the first occasion to a depth of 4.7 m. and later near the surface only. Occasional observations of snow temperatures to a depth of 12 m. were also made. Towards the end of the season the heat balance of the snow surface was examined in detail. The various contributions to the melting are evaluated for several short periods and their relative magnitudes compared. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 3 23 194 206
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Adkins, C. J.
The Summer Climate in the Accumulation Area of the Salmon Glacier
topic_facet Earth-Surface Processes
description Abstract During the summer of 1957 a party visited the Salmon Glacier in British Columbia. A meteorological station was established in the accumulation area at an altitude of 1700 m. From 12 June to 16 August pressure, temperature and humidity were recorded continuously and the daily totals of precipitation, ablation and percolation were obtained. Periodic measurements of snow density were made; on the first occasion to a depth of 4.7 m. and later near the surface only. Occasional observations of snow temperatures to a depth of 12 m. were also made. Towards the end of the season the heat balance of the snow surface was examined in detail. The various contributions to the melting are evaluated for several short periods and their relative magnitudes compared.
format Article in Journal/Newspaper
author Adkins, C. J.
author_facet Adkins, C. J.
author_sort Adkins, C. J.
title The Summer Climate in the Accumulation Area of the Salmon Glacier
title_short The Summer Climate in the Accumulation Area of the Salmon Glacier
title_full The Summer Climate in the Accumulation Area of the Salmon Glacier
title_fullStr The Summer Climate in the Accumulation Area of the Salmon Glacier
title_full_unstemmed The Summer Climate in the Accumulation Area of the Salmon Glacier
title_sort summer climate in the accumulation area of the salmon glacier
publisher Cambridge University Press (CUP)
publishDate 1958
url http://dx.doi.org/10.1017/s0022143000024242
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000024242
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 3, issue 23, page 194-206
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000024242
container_title Journal of Glaciology
container_volume 3
container_issue 23
container_start_page 194
op_container_end_page 206
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