Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut

A 130 km 2 tabular iceberg calved from Petermann Glacier in northwestern Greenland on 5 August 2012. Subsequent fracturing generated many individual large “ice islands”, including Petermann ice island (PII)-A-1-f, which drifted between Nares Strait and the North Atlantic. Thinning caused by basal an...

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Published in:The Cryosphere
Main Authors: A. J. Crawford, D. Mueller, G. Crocker, L. Mingo, L. Desjardins, D. Dumont, M. Babin
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-1067-2020
https://doaj.org/article/d6b24e2c1881443097f06329e62a9dba
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spelling ftdoajarticles:oai:doaj.org/article:d6b24e2c1881443097f06329e62a9dba 2023-05-15T15:35:07+02:00 Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut A. J. Crawford D. Mueller G. Crocker L. Mingo L. Desjardins D. Dumont M. Babin 2020-03-01T00:00:00Z https://doi.org/10.5194/tc-14-1067-2020 https://doaj.org/article/d6b24e2c1881443097f06329e62a9dba EN eng Copernicus Publications https://www.the-cryosphere.net/14/1067/2020/tc-14-1067-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-1067-2020 1994-0416 1994-0424 https://doaj.org/article/d6b24e2c1881443097f06329e62a9dba The Cryosphere, Vol 14, Pp 1067-1081 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/tc-14-1067-2020 2022-12-31T15:47:45Z A 130 km 2 tabular iceberg calved from Petermann Glacier in northwestern Greenland on 5 August 2012. Subsequent fracturing generated many individual large “ice islands”, including Petermann ice island (PII)-A-1-f, which drifted between Nares Strait and the North Atlantic. Thinning caused by basal and surface ablation increases the likelihood that these ice islands will fracture and disperse further, thereby increasing the risk to marine transport and infrastructure as well as affecting the distribution of freshwater from the polar ice sheets. We use a unique stationary and mobile ice-penetrating radar dataset collected over four campaigns to PII-A-1-f to quantify and contextualize ice island surface and basal ablation rates and calibrate a forced convection basal ablation model. The ice island thinned by 4.7 m over 11 months. The majority of thinning (73 %) resulted from basal ablation, but the volume loss associated with basal ablation was ∼12 times less than that caused by areal reduction (e.g. wave erosion, calving, and fracture). However, localized thinning may have influenced a large fracture event that occurred along a section of ice that was ∼40 m thinner than the remainder of the ice island. The calibration of the basal ablation model, the first known to be conducted with field data, supports assigning the theoretically derived value of 1.2×10 −5 m 2∕5 s <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><msup><mi/><mrow><mo>-</mo><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">5</mn></mrow></msup></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="21pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="dc3a2b0c77aa6bbfb7ca38686ad27960"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-14-1067-2020-ie00001.svg" width="21pt" height="11pt" src="tc-14-1067-2020-ie00001.png"/></svg:svg> ... Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin glacier Greenland Nares strait North Atlantic Nunavut Petermann glacier The Cryosphere Directory of Open Access Journals: DOAJ Articles Baffin Bay Greenland Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Nunavut The Cryosphere 14 3 1067 1081
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
A. J. Crawford
D. Mueller
G. Crocker
L. Mingo
L. Desjardins
D. Dumont
M. Babin
Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description A 130 km 2 tabular iceberg calved from Petermann Glacier in northwestern Greenland on 5 August 2012. Subsequent fracturing generated many individual large “ice islands”, including Petermann ice island (PII)-A-1-f, which drifted between Nares Strait and the North Atlantic. Thinning caused by basal and surface ablation increases the likelihood that these ice islands will fracture and disperse further, thereby increasing the risk to marine transport and infrastructure as well as affecting the distribution of freshwater from the polar ice sheets. We use a unique stationary and mobile ice-penetrating radar dataset collected over four campaigns to PII-A-1-f to quantify and contextualize ice island surface and basal ablation rates and calibrate a forced convection basal ablation model. The ice island thinned by 4.7 m over 11 months. The majority of thinning (73 %) resulted from basal ablation, but the volume loss associated with basal ablation was ∼12 times less than that caused by areal reduction (e.g. wave erosion, calving, and fracture). However, localized thinning may have influenced a large fracture event that occurred along a section of ice that was ∼40 m thinner than the remainder of the ice island. The calibration of the basal ablation model, the first known to be conducted with field data, supports assigning the theoretically derived value of 1.2×10 −5 m 2∕5 s <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><msup><mi/><mrow><mo>-</mo><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">5</mn></mrow></msup></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="21pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="dc3a2b0c77aa6bbfb7ca38686ad27960"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-14-1067-2020-ie00001.svg" width="21pt" height="11pt" src="tc-14-1067-2020-ie00001.png"/></svg:svg> ...
format Article in Journal/Newspaper
author A. J. Crawford
D. Mueller
G. Crocker
L. Mingo
L. Desjardins
D. Dumont
M. Babin
author_facet A. J. Crawford
D. Mueller
G. Crocker
L. Mingo
L. Desjardins
D. Dumont
M. Babin
author_sort A. J. Crawford
title Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut
title_short Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut
title_full Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut
title_fullStr Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut
title_full_unstemmed Ice island thinning: rates and model calibration with in situ observations from Baffin Bay, Nunavut
title_sort ice island thinning: rates and model calibration with in situ observations from baffin bay, nunavut
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-1067-2020
https://doaj.org/article/d6b24e2c1881443097f06329e62a9dba
long_lat ENVELOPE(158.167,158.167,-81.450,-81.450)
geographic Baffin Bay
Greenland
Nares
Nunavut
geographic_facet Baffin Bay
Greenland
Nares
Nunavut
genre Baffin Bay
Baffin Bay
Baffin
glacier
Greenland
Nares strait
North Atlantic
Nunavut
Petermann glacier
The Cryosphere
genre_facet Baffin Bay
Baffin Bay
Baffin
glacier
Greenland
Nares strait
North Atlantic
Nunavut
Petermann glacier
The Cryosphere
op_source The Cryosphere, Vol 14, Pp 1067-1081 (2020)
op_relation https://www.the-cryosphere.net/14/1067/2020/tc-14-1067-2020.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-14-1067-2020
1994-0416
1994-0424
https://doaj.org/article/d6b24e2c1881443097f06329e62a9dba
op_doi https://doi.org/10.5194/tc-14-1067-2020
container_title The Cryosphere
container_volume 14
container_issue 3
container_start_page 1067
op_container_end_page 1081
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