Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interface

Spatial and temporal trends of remotely sensed sea-ice cover, sea surface temperatures, chlorophyll-a concentration and primary production in the Baffin Bay, Davis Strait and Labrador Sea were analyzed for the 1998–2017 period. We found spatial variability in the trends of these cryospheric, biologi...

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Main Authors: Ashley V. York, Karen E. Frey, Luisa N. C. Young
Format: Article
Language:English
Published: Cambridge University Press 2020-12-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S026030552000066X/type/journal_article
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author Ashley V. York
Karen E. Frey
Luisa N. C. Young
author_facet Ashley V. York
Karen E. Frey
Luisa N. C. Young
author_sort Ashley V. York
collection DOAJ
description Spatial and temporal trends of remotely sensed sea-ice cover, sea surface temperatures, chlorophyll-a concentration and primary production in the Baffin Bay, Davis Strait and Labrador Sea were analyzed for the 1998–2017 period. We found spatial variability in the trends of these cryospheric, biologic and oceanographic phenomena. For example, in the northern Baffin Bay, we observed decreases in annual sea-ice persistence, yet increases along the Labrador Sea-ice edge during winter, with the latter having significant correlations with broader atmospheric patterns. In general, we observed increases in summer sea surface temperatures across the study region, except a small area of cooling along the southern Greenlandic coast. We also found significant negative trends in April chlorophyll-a and primary production followed by significant positive trends for both biological phenomena in May, owing to anomalously high values in 2014 and 2015. Notably, we found a significant positive correlation between days of monthly sea ice presence in April with May primary production quantities. Finally, we found a significant positive trend in total annual primary production over the study period. This novel finding suggests an important relationship between the timing of breakup along the sea-ice edge and peaks in biological production.
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spelling doaj.art-0899779eea244ec6800fb4580cfd3c832023-03-09T12:27:40ZengCambridge University PressAnnals of Glaciology0260-30551727-56442020-12-016142644010.1017/aog.2020.66Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interfaceAshley V. York0https://orcid.org/0000-0001-9058-3470Karen E. Frey1Luisa N. C. Young2Rowan University, Department of Geography, Planning and Sustainability, Glassboro, New Jersey, USA Clark University, Graduate School of Geography, Worcester, Massachusetts, USAClark University, Graduate School of Geography, Worcester, Massachusetts, USAClark University, Graduate School of Geography, Worcester, Massachusetts, USASpatial and temporal trends of remotely sensed sea-ice cover, sea surface temperatures, chlorophyll-a concentration and primary production in the Baffin Bay, Davis Strait and Labrador Sea were analyzed for the 1998–2017 period. We found spatial variability in the trends of these cryospheric, biologic and oceanographic phenomena. For example, in the northern Baffin Bay, we observed decreases in annual sea-ice persistence, yet increases along the Labrador Sea-ice edge during winter, with the latter having significant correlations with broader atmospheric patterns. In general, we observed increases in summer sea surface temperatures across the study region, except a small area of cooling along the southern Greenlandic coast. We also found significant negative trends in April chlorophyll-a and primary production followed by significant positive trends for both biological phenomena in May, owing to anomalously high values in 2014 and 2015. Notably, we found a significant positive correlation between days of monthly sea ice presence in April with May primary production quantities. Finally, we found a significant positive trend in total annual primary production over the study period. This novel finding suggests an important relationship between the timing of breakup along the sea-ice edge and peaks in biological production.https://www.cambridge.org/core/product/identifier/S026030552000066X/type/journal_articlePolar and subpolar oceansremote sensingsea ice
spellingShingle Ashley V. York
Karen E. Frey
Luisa N. C. Young
Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interface
Annals of Glaciology
Polar and subpolar oceans
remote sensing
sea ice
title Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interface
title_full Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interface
title_fullStr Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interface
title_full_unstemmed Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interface
title_short Changes at the edge: trends in sea ice, ocean temperature and ocean color at the Northwest Atlantic/Southern Arctic interface
title_sort changes at the edge trends in sea ice ocean temperature and ocean color at the northwest atlantic southern arctic interface
topic Polar and subpolar oceans
remote sensing
sea ice
url https://www.cambridge.org/core/product/identifier/S026030552000066X/type/journal_article
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AT luisancyoung changesattheedgetrendsinseaiceoceantemperatureandoceancoloratthenorthwestatlanticsouthernarcticinterface