Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts

Utilizing the reduced-complexity model Hector, a regional scale analysis was conducted quantifying the possible effects climate change may have on dimethyl sulfide (DMS) emissions within the oceans. The investigation began with a review of the sulfur cycle in modern Earth system models. We then expa...

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Published in:Atmosphere
Main Authors: Zachary M. Menzo, Scott Elliott, Corinne A. Hartin, Forrest M. Hoffman, Shanlin Wang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/atmos9050167
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spelling ftmdpi:oai:mdpi.com:/2073-4433/9/5/167/ 2023-08-20T04:08:56+02:00 Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts Zachary M. Menzo Scott Elliott Corinne A. Hartin Forrest M. Hoffman Shanlin Wang agris 2018-05-01 application/pdf https://doi.org/10.3390/atmos9050167 EN eng Multidisciplinary Digital Publishing Institute Biosphere/Hydrosphere/Land–Atmosphere Interactions https://dx.doi.org/10.3390/atmos9050167 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 9; Issue 5; Pages: 167 dimethyl sulfide marine biogeochemical feedback climate change phytoplankton ocean acidification community shifts Phaeocystis Text 2018 ftmdpi https://doi.org/10.3390/atmos9050167 2023-07-31T21:30:01Z Utilizing the reduced-complexity model Hector, a regional scale analysis was conducted quantifying the possible effects climate change may have on dimethyl sulfide (DMS) emissions within the oceans. The investigation began with a review of the sulfur cycle in modern Earth system models. We then expanded the biogeochemical representation within Hector to include a natural ocean component while accounting for acidification and planktonic community shifts. The report presents results from both a latitudinal and a global perspective. This new approach highlights disparate outcomes which have been inadequately characterized via planetary averages in past publications. Our findings suggest that natural sulfur emissions (ESN) may exert a forcing up to 4 times that of the CO2 marine feedback, 0.62 and 0.15 Wm−2, respectively, and reverse the radiative forcing sign in low latitudes. Additionally, sensitivity tests were conducted to demonstrate the need for further examination of the DMS loop. Ultimately, the present work attempts to include dynamic ESN within reduced-complexity simulations of the sulfur cycle, illustrating its impact on the global radiative budget. Text Ocean acidification MDPI Open Access Publishing Hector ENVELOPE(-63.376,-63.376,-64.579,-64.579) Atmosphere 9 5 167
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic dimethyl sulfide
marine biogeochemical feedback
climate change
phytoplankton
ocean acidification
community shifts
Phaeocystis
spellingShingle dimethyl sulfide
marine biogeochemical feedback
climate change
phytoplankton
ocean acidification
community shifts
Phaeocystis
Zachary M. Menzo
Scott Elliott
Corinne A. Hartin
Forrest M. Hoffman
Shanlin Wang
Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts
topic_facet dimethyl sulfide
marine biogeochemical feedback
climate change
phytoplankton
ocean acidification
community shifts
Phaeocystis
description Utilizing the reduced-complexity model Hector, a regional scale analysis was conducted quantifying the possible effects climate change may have on dimethyl sulfide (DMS) emissions within the oceans. The investigation began with a review of the sulfur cycle in modern Earth system models. We then expanded the biogeochemical representation within Hector to include a natural ocean component while accounting for acidification and planktonic community shifts. The report presents results from both a latitudinal and a global perspective. This new approach highlights disparate outcomes which have been inadequately characterized via planetary averages in past publications. Our findings suggest that natural sulfur emissions (ESN) may exert a forcing up to 4 times that of the CO2 marine feedback, 0.62 and 0.15 Wm−2, respectively, and reverse the radiative forcing sign in low latitudes. Additionally, sensitivity tests were conducted to demonstrate the need for further examination of the DMS loop. Ultimately, the present work attempts to include dynamic ESN within reduced-complexity simulations of the sulfur cycle, illustrating its impact on the global radiative budget.
format Text
author Zachary M. Menzo
Scott Elliott
Corinne A. Hartin
Forrest M. Hoffman
Shanlin Wang
author_facet Zachary M. Menzo
Scott Elliott
Corinne A. Hartin
Forrest M. Hoffman
Shanlin Wang
author_sort Zachary M. Menzo
title Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts
title_short Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts
title_full Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts
title_fullStr Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts
title_full_unstemmed Climate Change Impacts on Natural Sulfur Production: Ocean Acidification and Community Shifts
title_sort climate change impacts on natural sulfur production: ocean acidification and community shifts
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/atmos9050167
op_coverage agris
long_lat ENVELOPE(-63.376,-63.376,-64.579,-64.579)
geographic Hector
geographic_facet Hector
genre Ocean acidification
genre_facet Ocean acidification
op_source Atmosphere; Volume 9; Issue 5; Pages: 167
op_relation Biosphere/Hydrosphere/Land–Atmosphere Interactions
https://dx.doi.org/10.3390/atmos9050167
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos9050167
container_title Atmosphere
container_volume 9
container_issue 5
container_start_page 167
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