Iceberg Melting and Climate Change in NW Atlantic Waters

Climate change is predicted to cause increases in sea surface temperature (SST), as well as decreases in sea-ice cover, wind and current velocities. These changes will have a marked effect on iceberg melting in the shipping lanes off Newfoundland and Labrador, Canada. Icebergs that today can cross...

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Main Authors: Sergio Perez-Gruszkiewicz, William Peterson
Format: Article
Language:English
Published: Gdynia Maritime University 2018-09-01
Series:TransNav: International Journal on Marine Navigation and Safety of Sea Transportation
Subjects:
Online Access:http://www.transnav.eu/files/Iceberg Melting and Climate Change in NW Atlantic Waters,829.pdf
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spelling doaj-868b747a2d3b444392719fb8fac3ffea2020-11-25T00:03:10ZengGdynia Maritime UniversityTransNav: International Journal on Marine Navigation and Safety of Sea Transportation2083-64732083-64812018-09-0112345946710.12716/1001.12.03.04829Iceberg Melting and Climate Change in NW Atlantic WatersSergio Perez-Gruszkiewicz0William Peterson1United States Merchant Marine Academy, Kings Point, New York, United States of AmericaUnited States Merchant Marine Academy, Kings Point, New York, United States of AmericaClimate change is predicted to cause increases in sea surface temperature (SST), as well as decreases in sea-ice cover, wind and current velocities. These changes will have a marked effect on iceberg melting in the shipping lanes off Newfoundland and Labrador, Canada. Icebergs that today can cross from northern Labrador to Newfoundland without melting will in the future have to be much larger to survive the transit. For example, icebergs at N Labrador in December of 2016 that are smaller than 156 m will melt before reaching 48N, but in year 2100 the length increases to 228 m. In addition, if future iceberg size distributions off Labrador are the same as today, icebergs will experience roughly 50% reductions in numbers in the NW Atlantic shipping lanes by year 2100. The increased melting rates are due to, in order of importance, increased sea-surface temperatures (responsible for 66% of the increase in the minimum transit size), decreasing current velocities (31%), and decreasing sea-ice cover (3%). Decreasing sea-ice tends to increase wave heights as well as accelerate the effects of wave erosion; however, for the areas studied the wave height is predicted to decrease moderately in year 2100, by a maximum of about 10% in December.http://www.transnav.eu/files/Iceberg Melting and Climate Change in NW Atlantic Waters,829.pdfArctic ShippingClimate ChangeIcebergAtlantic OceanNW AtlanticIceberg MeltingLabradorInternational Ice Patrol (IIP)
collection DOAJ
language English
format Article
sources DOAJ
author Sergio Perez-Gruszkiewicz
William Peterson
spellingShingle Sergio Perez-Gruszkiewicz
William Peterson
Iceberg Melting and Climate Change in NW Atlantic Waters
TransNav: International Journal on Marine Navigation and Safety of Sea Transportation
Arctic Shipping
Climate Change
Iceberg
Atlantic Ocean
NW Atlantic
Iceberg Melting
Labrador
International Ice Patrol (IIP)
author_facet Sergio Perez-Gruszkiewicz
William Peterson
author_sort Sergio Perez-Gruszkiewicz
title Iceberg Melting and Climate Change in NW Atlantic Waters
title_short Iceberg Melting and Climate Change in NW Atlantic Waters
title_full Iceberg Melting and Climate Change in NW Atlantic Waters
title_fullStr Iceberg Melting and Climate Change in NW Atlantic Waters
title_full_unstemmed Iceberg Melting and Climate Change in NW Atlantic Waters
title_sort iceberg melting and climate change in nw atlantic waters
publisher Gdynia Maritime University
series TransNav: International Journal on Marine Navigation and Safety of Sea Transportation
issn 2083-6473
2083-6481
publishDate 2018-09-01
description Climate change is predicted to cause increases in sea surface temperature (SST), as well as decreases in sea-ice cover, wind and current velocities. These changes will have a marked effect on iceberg melting in the shipping lanes off Newfoundland and Labrador, Canada. Icebergs that today can cross from northern Labrador to Newfoundland without melting will in the future have to be much larger to survive the transit. For example, icebergs at N Labrador in December of 2016 that are smaller than 156 m will melt before reaching 48N, but in year 2100 the length increases to 228 m. In addition, if future iceberg size distributions off Labrador are the same as today, icebergs will experience roughly 50% reductions in numbers in the NW Atlantic shipping lanes by year 2100. The increased melting rates are due to, in order of importance, increased sea-surface temperatures (responsible for 66% of the increase in the minimum transit size), decreasing current velocities (31%), and decreasing sea-ice cover (3%). Decreasing sea-ice tends to increase wave heights as well as accelerate the effects of wave erosion; however, for the areas studied the wave height is predicted to decrease moderately in year 2100, by a maximum of about 10% in December.
topic Arctic Shipping
Climate Change
Iceberg
Atlantic Ocean
NW Atlantic
Iceberg Melting
Labrador
International Ice Patrol (IIP)
url http://www.transnav.eu/files/Iceberg Melting and Climate Change in NW Atlantic Waters,829.pdf
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