Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing

River water is the main source of dissolved organic carbon (DOC) in the Arctic Ocean. DOC plays an important role in the Arctic carbon cycle, and its export from land to sea is expected to increase as ongoing climate change accelerates permafrost thaw. However, transport pathways and transformation...

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Published in:Biogeosciences
Main Authors: Juhls, Bennet, Overduin, Pier Paul, Hölemann, Jens, Hieronymi, Martin, Matsuoka, Atsushi, Heim, Birgit, Fischer, Jürgen
Format: Article in Journal/Newspaper
Language:unknown
Published: COPERNICUS GESELLSCHAFT MBH 2019
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Online Access:https://epic.awi.de/id/eprint/50021/
https://epic.awi.de/id/eprint/50021/1/bg-16-2693-2019.pdf
https://hdl.handle.net/10013/epic.be21ad0f-5b94-4b62-b050-044e193b2be9
id ftawi:oai:epic.awi.de:50021
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spelling ftawi:oai:epic.awi.de:50021 2024-09-15T17:54:18+00:00 Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing Juhls, Bennet Overduin, Pier Paul Hölemann, Jens Hieronymi, Martin Matsuoka, Atsushi Heim, Birgit Fischer, Jürgen 2019 application/pdf https://epic.awi.de/id/eprint/50021/ https://epic.awi.de/id/eprint/50021/1/bg-16-2693-2019.pdf https://hdl.handle.net/10013/epic.be21ad0f-5b94-4b62-b050-044e193b2be9 unknown COPERNICUS GESELLSCHAFT MBH https://epic.awi.de/id/eprint/50021/1/bg-16-2693-2019.pdf Juhls, B. orcid:0000-0002-5844-6318 , Overduin, P. P. orcid:0000-0001-9849-4712 , Hölemann, J. orcid:0000-0001-5102-4086 , Hieronymi, M. , Matsuoka, A. , Heim, B. orcid:0000-0003-2614-9391 and Fischer, J. (2019) Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing , Biogeosciences, 16 , pp. 2693-2713 . doi:10.5194/bg-16-2693-2019 <https://doi.org/10.5194/bg-16-2693-2019> , hdl:10013/epic.be21ad0f-5b94-4b62-b050-044e193b2be9 EPIC3Biogeosciences, COPERNICUS GESELLSCHAFT MBH, 16, pp. 2693-2713, ISSN: 1726-4170 Article isiRev 2019 ftawi https://doi.org/10.5194/bg-16-2693-2019 2024-06-24T04:22:11Z River water is the main source of dissolved organic carbon (DOC) in the Arctic Ocean. DOC plays an important role in the Arctic carbon cycle, and its export from land to sea is expected to increase as ongoing climate change accelerates permafrost thaw. However, transport pathways and transformation of DOC in the land-to-ocean transition are mostly unknown. We collected DOC and aCDOM(λ) samples from 11 expeditions to river, coastal and offshore waters and present a new DOC–aCDOM(λ) model for the fluvial–marine transition zone in the Laptev Sea. The aCDOM(λ) characteristics revealed that the dissolved organic matter (DOM) in samples of this dataset are primarily of terrigenous origin. Observed changes in aCDOM(443) and its spectral slopes indicate that DOM is modified by microbial and photo-degradation. Ocean colour remote sensing (OCRS) provides the absorption coefficient of coloured dissolved organic matter (aCDOM(λ)sat) at λ=440 or 443 nm, which can be used to estimate DOC concentration at high temporal and spatial resolution over large regions. We tested the statistical performance of five OCRS algorithms and evaluated the plausibility of the spatial distribution of derived aCDOM(λ)sat. The OLCI (Sentinel-3 Ocean and Land Colour Instrument) neural network swarm (ONNS) algorithm showed the best performance compared to in situ aCDOM(440) (r2=0.72). Additionally, we found ONNS-derived aCDOM(440), in contrast to other algorithms, to be partly independent of sediment concentration, making ONNS the most suitable aCDOM(λ)sat algorithm for the Laptev Sea region. The DOC–aCDOM(λ) model was applied to ONNS-derived aCDOM(440), and retrieved DOC concentration maps showed moderate agreement to in situ data (r2=0.53). The in situ and satellite-retrieved data were offset by up to several days, which may partly explain the weak correlation for this dynamic region. Satellite-derived surface water DOC concentration maps from Medium Resolution Imaging Spectrometer (MERIS) satellite data demonstrate rapid removal of DOC within ... Article in Journal/Newspaper Arctic Ocean Climate change laptev Laptev Sea permafrost Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Biogeosciences 16 13 2693 2713
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description River water is the main source of dissolved organic carbon (DOC) in the Arctic Ocean. DOC plays an important role in the Arctic carbon cycle, and its export from land to sea is expected to increase as ongoing climate change accelerates permafrost thaw. However, transport pathways and transformation of DOC in the land-to-ocean transition are mostly unknown. We collected DOC and aCDOM(λ) samples from 11 expeditions to river, coastal and offshore waters and present a new DOC–aCDOM(λ) model for the fluvial–marine transition zone in the Laptev Sea. The aCDOM(λ) characteristics revealed that the dissolved organic matter (DOM) in samples of this dataset are primarily of terrigenous origin. Observed changes in aCDOM(443) and its spectral slopes indicate that DOM is modified by microbial and photo-degradation. Ocean colour remote sensing (OCRS) provides the absorption coefficient of coloured dissolved organic matter (aCDOM(λ)sat) at λ=440 or 443 nm, which can be used to estimate DOC concentration at high temporal and spatial resolution over large regions. We tested the statistical performance of five OCRS algorithms and evaluated the plausibility of the spatial distribution of derived aCDOM(λ)sat. The OLCI (Sentinel-3 Ocean and Land Colour Instrument) neural network swarm (ONNS) algorithm showed the best performance compared to in situ aCDOM(440) (r2=0.72). Additionally, we found ONNS-derived aCDOM(440), in contrast to other algorithms, to be partly independent of sediment concentration, making ONNS the most suitable aCDOM(λ)sat algorithm for the Laptev Sea region. The DOC–aCDOM(λ) model was applied to ONNS-derived aCDOM(440), and retrieved DOC concentration maps showed moderate agreement to in situ data (r2=0.53). The in situ and satellite-retrieved data were offset by up to several days, which may partly explain the weak correlation for this dynamic region. Satellite-derived surface water DOC concentration maps from Medium Resolution Imaging Spectrometer (MERIS) satellite data demonstrate rapid removal of DOC within ...
format Article in Journal/Newspaper
author Juhls, Bennet
Overduin, Pier Paul
Hölemann, Jens
Hieronymi, Martin
Matsuoka, Atsushi
Heim, Birgit
Fischer, Jürgen
spellingShingle Juhls, Bennet
Overduin, Pier Paul
Hölemann, Jens
Hieronymi, Martin
Matsuoka, Atsushi
Heim, Birgit
Fischer, Jürgen
Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing
author_facet Juhls, Bennet
Overduin, Pier Paul
Hölemann, Jens
Hieronymi, Martin
Matsuoka, Atsushi
Heim, Birgit
Fischer, Jürgen
author_sort Juhls, Bennet
title Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing
title_short Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing
title_full Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing
title_fullStr Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing
title_full_unstemmed Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing
title_sort dissolved organic matter at the fluvial–marine transition in the laptev sea using in situ data and ocean colour remote sensing
publisher COPERNICUS GESELLSCHAFT MBH
publishDate 2019
url https://epic.awi.de/id/eprint/50021/
https://epic.awi.de/id/eprint/50021/1/bg-16-2693-2019.pdf
https://hdl.handle.net/10013/epic.be21ad0f-5b94-4b62-b050-044e193b2be9
genre Arctic Ocean
Climate change
laptev
Laptev Sea
permafrost
genre_facet Arctic Ocean
Climate change
laptev
Laptev Sea
permafrost
op_source EPIC3Biogeosciences, COPERNICUS GESELLSCHAFT MBH, 16, pp. 2693-2713, ISSN: 1726-4170
op_relation https://epic.awi.de/id/eprint/50021/1/bg-16-2693-2019.pdf
Juhls, B. orcid:0000-0002-5844-6318 , Overduin, P. P. orcid:0000-0001-9849-4712 , Hölemann, J. orcid:0000-0001-5102-4086 , Hieronymi, M. , Matsuoka, A. , Heim, B. orcid:0000-0003-2614-9391 and Fischer, J. (2019) Dissolved organic matter at the fluvial–marine transition in the Laptev Sea using in situ data and ocean colour remote sensing , Biogeosciences, 16 , pp. 2693-2713 . doi:10.5194/bg-16-2693-2019 <https://doi.org/10.5194/bg-16-2693-2019> , hdl:10013/epic.be21ad0f-5b94-4b62-b050-044e193b2be9
op_doi https://doi.org/10.5194/bg-16-2693-2019
container_title Biogeosciences
container_volume 16
container_issue 13
container_start_page 2693
op_container_end_page 2713
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