Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago

Equations relating the accretion and decay of sea ice to standard meteorological data are derived empirically from observations at Alert, Eureka, Isachsen, Mould Bay, and Resolute, 1947-1957. The differential equations permit calculation of ice growth by increments, and contain a separate term allow...

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Published in:ARCTIC
Main Author: Bilello, Michael A.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1961
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66708
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/66708 2023-05-15T14:19:21+02:00 Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago Bilello, Michael A. 1961-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66708 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66708/50621 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66708 ARCTIC; Vol. 14 No. 1 (1961): March: 1–80; 2-24 1923-1245 0004-0843 Ablation Accumulation Atmospheric temperature Climatology Growth Mathematical models Sea ice Snow Snow cover Thickness Alert Nunavut Eureka Isachsen Mould Bay (Weather Station) N.W.T Resolute info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1961 ftunivcalgaryojs 2022-03-22T21:23:31Z Equations relating the accretion and decay of sea ice to standard meteorological data are derived empirically from observations at Alert, Eureka, Isachsen, Mould Bay, and Resolute, 1947-1957. The differential equations permit calculation of ice growth by increments, and contain a separate term allowing for variations in snow-cover depths. The use of the formulas requires only a knowledge of air temperatures and snow depths. Good correlation is found between decrease in ice thickness and accumulated degree-days above -1.8°C. The stations' locations and names of adjacent water bodies are indicated with the approximate water depths where ice thickness measurements were made. Techniques used in the measurements are described; data on observed ice thickness, accumulated degree-days of frost, and average snow depths for 20-cm increments of ice growth are tabulated.--From CRREL. Article in Journal/Newspaper Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Eureka Isachsen Mould Bay Nunavut Sea ice University of Calgary Journal Hosting Arctic Canadian Arctic Archipelago Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Isachsen ENVELOPE(-103.505,-103.505,78.785,78.785) Mould Bay ENVELOPE(-119.436,-119.436,76.197,76.197) Nunavut ARCTIC 14 1
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Ablation
Accumulation
Atmospheric temperature
Climatology
Growth
Mathematical models
Sea ice
Snow
Snow cover
Thickness
Alert
Nunavut
Eureka
Isachsen
Mould Bay (Weather Station)
N.W.T
Resolute
spellingShingle Ablation
Accumulation
Atmospheric temperature
Climatology
Growth
Mathematical models
Sea ice
Snow
Snow cover
Thickness
Alert
Nunavut
Eureka
Isachsen
Mould Bay (Weather Station)
N.W.T
Resolute
Bilello, Michael A.
Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago
topic_facet Ablation
Accumulation
Atmospheric temperature
Climatology
Growth
Mathematical models
Sea ice
Snow
Snow cover
Thickness
Alert
Nunavut
Eureka
Isachsen
Mould Bay (Weather Station)
N.W.T
Resolute
description Equations relating the accretion and decay of sea ice to standard meteorological data are derived empirically from observations at Alert, Eureka, Isachsen, Mould Bay, and Resolute, 1947-1957. The differential equations permit calculation of ice growth by increments, and contain a separate term allowing for variations in snow-cover depths. The use of the formulas requires only a knowledge of air temperatures and snow depths. Good correlation is found between decrease in ice thickness and accumulated degree-days above -1.8°C. The stations' locations and names of adjacent water bodies are indicated with the approximate water depths where ice thickness measurements were made. Techniques used in the measurements are described; data on observed ice thickness, accumulated degree-days of frost, and average snow depths for 20-cm increments of ice growth are tabulated.--From CRREL.
format Article in Journal/Newspaper
author Bilello, Michael A.
author_facet Bilello, Michael A.
author_sort Bilello, Michael A.
title Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago
title_short Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago
title_full Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago
title_fullStr Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago
title_full_unstemmed Formation, Growth, and Decay of Sea-Ice in the Canadian Arctic Archipelago
title_sort formation, growth, and decay of sea-ice in the canadian arctic archipelago
publisher The Arctic Institute of North America
publishDate 1961
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66708
long_lat ENVELOPE(-85.940,-85.940,79.990,79.990)
ENVELOPE(-103.505,-103.505,78.785,78.785)
ENVELOPE(-119.436,-119.436,76.197,76.197)
geographic Arctic
Canadian Arctic Archipelago
Eureka
Isachsen
Mould Bay
Nunavut
geographic_facet Arctic
Canadian Arctic Archipelago
Eureka
Isachsen
Mould Bay
Nunavut
genre Arctic
Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Eureka
Isachsen
Mould Bay
Nunavut
Sea ice
genre_facet Arctic
Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Eureka
Isachsen
Mould Bay
Nunavut
Sea ice
op_source ARCTIC; Vol. 14 No. 1 (1961): March: 1–80; 2-24
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66708/50621
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66708
container_title ARCTIC
container_volume 14
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