East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice

Hudson Bay experiences a complete cryogenic cycle, which has been well documented since 1971. We developed a temperature proxy method to extend the sea ice record back to 1944, using mean temperatures for Churchill and Inukjuak and the difference between these means at two different seasonal periods...

Full description

Bibliographic Details
Published in:ARCTIC
Main Authors: McGovern, Peter G., Gough, William A.
Format: Article in Journal/Newspaper
Language:unknown
Published: The Arctic Institute of North America 2015
Subjects:
Online Access:http://dx.doi.org/10.14430/arctic4522
http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/viewFile/4522/4673
id crarcticinstna:10.14430/arctic4522
record_format openpolar
spelling crarcticinstna:10.14430/arctic4522 2024-09-15T17:49:53+00:00 East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice McGovern, Peter G. Gough, William A. 2015 http://dx.doi.org/10.14430/arctic4522 http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/viewFile/4522/4673 unknown The Arctic Institute of North America ARCTIC volume 68, issue 4, page 445 ISSN 1923-1245 0004-0843 journal-article 2015 crarcticinstna https://doi.org/10.14430/arctic4522 2024-06-25T04:00:29Z Hudson Bay experiences a complete cryogenic cycle, which has been well documented since 1971. We developed a temperature proxy method to extend the sea ice record back to 1944, using mean temperatures for Churchill and Inukjuak and the difference between these means at two different seasonal periods. This method proved to reproduce the 1971 to 2011 ice-free season length record with an error just over eight days (6%). This relationship was used to hindcast ice-free season length to 1944. This hindcast was subsequently appended to the existing 1971–2011 record to form a 68-year sea ice record. This extended record shows that the recent statistically significant increase in length of the ice-free season was not the result of a natural oscillation of less than 68 years and is consistent with a net warming due to increasing greenhouse gases. Article in Journal/Newspaper Arctic Hudson Bay Inukjuak Sea ice Arctic Institute of North America ARCTIC 68 4 445
institution Open Polar
collection Arctic Institute of North America
op_collection_id crarcticinstna
language unknown
description Hudson Bay experiences a complete cryogenic cycle, which has been well documented since 1971. We developed a temperature proxy method to extend the sea ice record back to 1944, using mean temperatures for Churchill and Inukjuak and the difference between these means at two different seasonal periods. This method proved to reproduce the 1971 to 2011 ice-free season length record with an error just over eight days (6%). This relationship was used to hindcast ice-free season length to 1944. This hindcast was subsequently appended to the existing 1971–2011 record to form a 68-year sea ice record. This extended record shows that the recent statistically significant increase in length of the ice-free season was not the result of a natural oscillation of less than 68 years and is consistent with a net warming due to increasing greenhouse gases.
format Article in Journal/Newspaper
author McGovern, Peter G.
Gough, William A.
spellingShingle McGovern, Peter G.
Gough, William A.
East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice
author_facet McGovern, Peter G.
Gough, William A.
author_sort McGovern, Peter G.
title East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice
title_short East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice
title_full East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice
title_fullStr East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice
title_full_unstemmed East-West Asymmetry in Coastal Temperatures of Hudson Bay as a Proxy for Sea Ice
title_sort east-west asymmetry in coastal temperatures of hudson bay as a proxy for sea ice
publisher The Arctic Institute of North America
publishDate 2015
url http://dx.doi.org/10.14430/arctic4522
http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/viewFile/4522/4673
genre Arctic
Hudson Bay
Inukjuak
Sea ice
genre_facet Arctic
Hudson Bay
Inukjuak
Sea ice
op_source ARCTIC
volume 68, issue 4, page 445
ISSN 1923-1245 0004-0843
op_doi https://doi.org/10.14430/arctic4522
container_title ARCTIC
container_volume 68
container_issue 4
container_start_page 445
_version_ 1810291662574845952