Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019

Global warming is not often discussed in the context of light availability within the water column. However, the light regimes in the Arctic Ocean are controlled by three factors that are influenced by climate changes which are the sea ice albedo feedback, glacial meltwater runoff and marine primary...

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Published in:Frontiers in Marine Science
Main Authors: Marta Konik, Mirosław Darecki, Alexey K. Pavlov, Sławomir Sagan, Piotr Kowalczuk
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2021
Subjects:
Q
Online Access:https://doi.org/10.3389/fmars.2021.699318
https://doaj.org/article/3cc61e92325443dca977120f74661c5c
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spelling ftdoajarticles:oai:doaj.org/article:3cc61e92325443dca977120f74661c5c 2023-05-15T13:11:43+02:00 Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019 Marta Konik Mirosław Darecki Alexey K. Pavlov Sławomir Sagan Piotr Kowalczuk 2021-10-01T00:00:00Z https://doi.org/10.3389/fmars.2021.699318 https://doaj.org/article/3cc61e92325443dca977120f74661c5c EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fmars.2021.699318/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2021.699318 https://doaj.org/article/3cc61e92325443dca977120f74661c5c Frontiers in Marine Science, Vol 8 (2021) Svalbard fjords IOPs remote sensing coastal darkening phytoplankton Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2021 ftdoajarticles https://doi.org/10.3389/fmars.2021.699318 2022-12-31T05:06:13Z Global warming is not often discussed in the context of light availability within the water column. However, the light regimes in the Arctic Ocean are controlled by three factors that are influenced by climate changes which are the sea ice albedo feedback, glacial meltwater runoff and marine primary production. Based on a satellite data series acquired during time period 1997 – 2019, we inspected long-term changes of the three commonly used optical characteristics Chla, atot(443), and Kd(490) within the Svalbard fjords and on the West Spitsbergen Shelf. We revealed evident positive trends in summer (July – September) in the Isfjorden, the Kongsfjorden, the Hornsund fjord, and the Bellsund. Moreover, between 1997 and 2019 at the majority of locations we observed a regime shift toward darker waters. We showed that light availability has changed in the Svalbard fjords since 1997, which may be a symptom of transformations in the environment that should be further investigated and monitored. Article in Journal/Newspaper albedo Arctic Arctic Ocean Bellsund Global warming Hornsund Isfjord* Isfjord* Isfjorden Isfjorden Kongsfjord* Kongsfjorden Phytoplankton Sea ice Svalbard Spitsbergen Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Svalbard Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Bellsund ENVELOPE(14.226,14.226,77.662,77.662) Frontiers in Marine Science 8
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Svalbard fjords
IOPs
remote sensing
coastal darkening
phytoplankton
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
spellingShingle Svalbard fjords
IOPs
remote sensing
coastal darkening
phytoplankton
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
Marta Konik
Mirosław Darecki
Alexey K. Pavlov
Sławomir Sagan
Piotr Kowalczuk
Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019
topic_facet Svalbard fjords
IOPs
remote sensing
coastal darkening
phytoplankton
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
description Global warming is not often discussed in the context of light availability within the water column. However, the light regimes in the Arctic Ocean are controlled by three factors that are influenced by climate changes which are the sea ice albedo feedback, glacial meltwater runoff and marine primary production. Based on a satellite data series acquired during time period 1997 – 2019, we inspected long-term changes of the three commonly used optical characteristics Chla, atot(443), and Kd(490) within the Svalbard fjords and on the West Spitsbergen Shelf. We revealed evident positive trends in summer (July – September) in the Isfjorden, the Kongsfjorden, the Hornsund fjord, and the Bellsund. Moreover, between 1997 and 2019 at the majority of locations we observed a regime shift toward darker waters. We showed that light availability has changed in the Svalbard fjords since 1997, which may be a symptom of transformations in the environment that should be further investigated and monitored.
format Article in Journal/Newspaper
author Marta Konik
Mirosław Darecki
Alexey K. Pavlov
Sławomir Sagan
Piotr Kowalczuk
author_facet Marta Konik
Mirosław Darecki
Alexey K. Pavlov
Sławomir Sagan
Piotr Kowalczuk
author_sort Marta Konik
title Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019
title_short Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019
title_full Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019
title_fullStr Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019
title_full_unstemmed Darkening of the Svalbard Fjords Waters Observed With Satellite Ocean Color Imagery in 1997–2019
title_sort darkening of the svalbard fjords waters observed with satellite ocean color imagery in 1997–2019
publisher Frontiers Media S.A.
publishDate 2021
url https://doi.org/10.3389/fmars.2021.699318
https://doaj.org/article/3cc61e92325443dca977120f74661c5c
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
ENVELOPE(14.226,14.226,77.662,77.662)
geographic Arctic
Arctic Ocean
Svalbard
Hornsund
Bellsund
geographic_facet Arctic
Arctic Ocean
Svalbard
Hornsund
Bellsund
genre albedo
Arctic
Arctic Ocean
Bellsund
Global warming
Hornsund
Isfjord*
Isfjord*
Isfjorden
Isfjorden
Kongsfjord*
Kongsfjorden
Phytoplankton
Sea ice
Svalbard
Spitsbergen
genre_facet albedo
Arctic
Arctic Ocean
Bellsund
Global warming
Hornsund
Isfjord*
Isfjord*
Isfjorden
Isfjorden
Kongsfjord*
Kongsfjorden
Phytoplankton
Sea ice
Svalbard
Spitsbergen
op_source Frontiers in Marine Science, Vol 8 (2021)
op_relation https://www.frontiersin.org/articles/10.3389/fmars.2021.699318/full
https://doaj.org/toc/2296-7745
2296-7745
doi:10.3389/fmars.2021.699318
https://doaj.org/article/3cc61e92325443dca977120f74661c5c
op_doi https://doi.org/10.3389/fmars.2021.699318
container_title Frontiers in Marine Science
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