The impact of global warming on seasonality of ocean primary production

The seasonal cycle (i.e. phenology) of oceanic primary production (PP) is expected to change in response to climate warming. Here, we use output from 6 global biogeochemical models to examine the response in the seasonal amplitude of PP and timing of peak PP to the IPCC AR5 warming scenario. We also...

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Published in:Biogeosciences
Main Authors: S. Henson, H. Cole, C. Beaulieu, A. Yool
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/bg-10-4357-2013
https://doaj.org/article/569846c44fca44aeb7d9e880064fbc87
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spelling ftdoajarticles:oai:doaj.org/article:569846c44fca44aeb7d9e880064fbc87 2023-05-15T14:59:53+02:00 The impact of global warming on seasonality of ocean primary production S. Henson H. Cole C. Beaulieu A. Yool 2013-06-01T00:00:00Z https://doi.org/10.5194/bg-10-4357-2013 https://doaj.org/article/569846c44fca44aeb7d9e880064fbc87 EN eng Copernicus Publications http://www.biogeosciences.net/10/4357/2013/bg-10-4357-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-10-4357-2013 1726-4170 1726-4189 https://doaj.org/article/569846c44fca44aeb7d9e880064fbc87 Biogeosciences, Vol 10, Iss 6, Pp 4357-4369 (2013) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/bg-10-4357-2013 2022-12-30T23:38:52Z The seasonal cycle (i.e. phenology) of oceanic primary production (PP) is expected to change in response to climate warming. Here, we use output from 6 global biogeochemical models to examine the response in the seasonal amplitude of PP and timing of peak PP to the IPCC AR5 warming scenario. We also investigate whether trends in PP phenology may be more rapidly detectable than trends in annual mean PP. The seasonal amplitude of PP decreases by an average of 1–2% per year by 2100 in most biomes, with the exception of the Arctic which sees an increase of ~1% per year. This is accompanied by an advance in the timing of peak PP by ~0.5–1 months by 2100 over much of the globe, and particularly pronounced in the Arctic. These changes are driven by an increase in seasonal amplitude of sea surface temperature (where the maxima get hotter faster than the minima) and a decrease in the seasonal amplitude of the mixed layer depth and surface nitrate concentration. Our results indicate a transformation of currently strongly seasonal (bloom forming) regions, typically found at high latitudes, into weakly seasonal (non-bloom) regions, characteristic of contemporary subtropical conditions. On average, 36 yr of data are needed to detect a climate-change-driven trend in the seasonal amplitude of PP, compared to 32 yr for mean annual PP. Monthly resolution model output is found to be inadequate for resolving phenological changes. We conclude that analysis of phytoplankton seasonality is not necessarily a shortcut to detecting climate change impacts on ocean productivity. Article in Journal/Newspaper Arctic Climate change Global warming Phytoplankton Directory of Open Access Journals: DOAJ Articles Arctic Biogeosciences 10 6 4357 4369
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
spellingShingle Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
S. Henson
H. Cole
C. Beaulieu
A. Yool
The impact of global warming on seasonality of ocean primary production
topic_facet Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
description The seasonal cycle (i.e. phenology) of oceanic primary production (PP) is expected to change in response to climate warming. Here, we use output from 6 global biogeochemical models to examine the response in the seasonal amplitude of PP and timing of peak PP to the IPCC AR5 warming scenario. We also investigate whether trends in PP phenology may be more rapidly detectable than trends in annual mean PP. The seasonal amplitude of PP decreases by an average of 1–2% per year by 2100 in most biomes, with the exception of the Arctic which sees an increase of ~1% per year. This is accompanied by an advance in the timing of peak PP by ~0.5–1 months by 2100 over much of the globe, and particularly pronounced in the Arctic. These changes are driven by an increase in seasonal amplitude of sea surface temperature (where the maxima get hotter faster than the minima) and a decrease in the seasonal amplitude of the mixed layer depth and surface nitrate concentration. Our results indicate a transformation of currently strongly seasonal (bloom forming) regions, typically found at high latitudes, into weakly seasonal (non-bloom) regions, characteristic of contemporary subtropical conditions. On average, 36 yr of data are needed to detect a climate-change-driven trend in the seasonal amplitude of PP, compared to 32 yr for mean annual PP. Monthly resolution model output is found to be inadequate for resolving phenological changes. We conclude that analysis of phytoplankton seasonality is not necessarily a shortcut to detecting climate change impacts on ocean productivity.
format Article in Journal/Newspaper
author S. Henson
H. Cole
C. Beaulieu
A. Yool
author_facet S. Henson
H. Cole
C. Beaulieu
A. Yool
author_sort S. Henson
title The impact of global warming on seasonality of ocean primary production
title_short The impact of global warming on seasonality of ocean primary production
title_full The impact of global warming on seasonality of ocean primary production
title_fullStr The impact of global warming on seasonality of ocean primary production
title_full_unstemmed The impact of global warming on seasonality of ocean primary production
title_sort impact of global warming on seasonality of ocean primary production
publisher Copernicus Publications
publishDate 2013
url https://doi.org/10.5194/bg-10-4357-2013
https://doaj.org/article/569846c44fca44aeb7d9e880064fbc87
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Global warming
Phytoplankton
genre_facet Arctic
Climate change
Global warming
Phytoplankton
op_source Biogeosciences, Vol 10, Iss 6, Pp 4357-4369 (2013)
op_relation http://www.biogeosciences.net/10/4357/2013/bg-10-4357-2013.pdf
https://doaj.org/toc/1726-4170
https://doaj.org/toc/1726-4189
doi:10.5194/bg-10-4357-2013
1726-4170
1726-4189
https://doaj.org/article/569846c44fca44aeb7d9e880064fbc87
op_doi https://doi.org/10.5194/bg-10-4357-2013
container_title Biogeosciences
container_volume 10
container_issue 6
container_start_page 4357
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