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The Arctic Ocean ecosystems are experiencing rapid changes. This could have possible implications for aerosol and cloud feedbacks that are not currently represented in CMIP6 models. One important proxy for plankton life is oceanic chlorophyll. This study investigates the representation of chlorophyll in two CMIP6 models; GFDL-ESM4 and MPI-ESM1-2-LR, and compares it with satellite observations. The chlorophyll concentration elvovement in time is investigated in Bering Strait and Fram Strait. The satellite observations show a positive trend of 0.1 mg myear (Fram Strait) and 0.06 mg myear (Bering Strait) in maximum chlorophyll values. The projected changes in SSP2-4.5 in GFDL-ESM4 is a negative trend of -0.018 mg myear in maximum values, while MPI-ESM1-2-LR shows a positive trend of 0.011 mg myear in maximum values. Chlorophyll is compared with the other biological proxies bacterial carbon concentration and dissolved organic carbon. Chlorophyll is found to have a moderate correlation of 0.53 with bacterical carbon in GFDL-ESM4. No correlation is found with dissolved organic carbon, 0.09 for GFDL-ESM4 and 0.05 for MPI-ESM1-2-LR. GFDL-ESM4 and MPI-ESM1-2-LR also show diverging relationship between sea ice concentration and chlorophyll, where chlorophyll decreases along with declining sea ice at the end of SSP2-4.5, while chlorophyll increases in MPI-ESM1-2-LR with declining sea ice.
The computing resources used for this course have been kindly provided by Galaxy europe in the framework of the EOSC-Nordic and RELIANCE projects. The storage resources were provided by UNINETT Sigma2 - the Norwegian National Infrastructure for High Performance Computing and Data Storage in Norway as part of NS1000K project
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A song of Ice and Phytoplankton
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Gjelsvik, Astrid Bragstad, and Gabriel Freitas. "A song of Ice and Phytoplankton." ROHub. Mar 18 ,2022. https://w3id.org/ro-id/183f2862-7509-4343-8ec9-74775b642c8d.
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Time evolution of chlorophyll concentrations in Bering Strait and Fram Straits. Blue dots mark satellite measured values (MODIS-Aqua).
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To use it:
download the image file docker-climate-notebook-2021-03-18.tar
load it with docker with the command: docker load --input docker-climate-notebook-2021-03-18.tar
launch the Docker container binding of your data folder (on the local machine) with the /import folder i(inside the container) with the command: docker run -v my_data_folder:/import -p 7777:8888 quay.io/nordicesmhub/docker-climate-notebook:2021-03-18
start your favorite web browser and go to: http://localhost:7777/ipython/
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Jupyter Notebook for comparing model and observations of Chlorophyll concentrations over the Artic Ocean.
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GeoJSON for Bering and Fram Straits
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10.1038/s41467-021-25699-w
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The future response of marine ecosystem diversity to continued anthropogenic forcing is poorly constrained. Phytoplankton are a diverse set of organisms that form the base of the marine ecosystem. Currently, ocean biogeochemistry and ecosystem models used for climate change projections typically include only 2−3 phytoplankton types and are, therefore, too simple to adequately assess the potential for changes in plankton community structure. Here, we analyse a complex ecosystem model with 35 phytoplankton types to evaluate the changes in phytoplankton community composition, turnover and size structure over the 21st century. We find that the rate of turnover in the phytoplankton community becomes faster during this century, that is, the community structure becomes increasingly unstable in response to climate change. Combined with alterations to phytoplankton diversity, our results imply a loss of ecological resilience with likely knock-on effects on the productivity and functioning of the marine environment.
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Future phytoplankton diversity in a changing climate
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2022-03-26 14:57:16.359048+00:00
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ADAM DataCube August 2011 MODIS Chlorophyll-a Concentration(monthly)
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August 2011 MODIS Chlorophyll-a Concentration (monthly)
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This Jupyter notebook has been used to generate the Research Object and also to update it e.g. add all the internal and external resources used and generated during the eScience course.
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https://choosealicense.com/no-permission/
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Jupyter Notebook for creating RO and aggregating all the resources used/generated
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2022-03-26 14:58:16.654280+00:00
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ADAM DataCube July 2015 MODIS Chlorophyll-a Concentration(monthly)
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https://choosealicense.com/no-permission/
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July 2015 MODIS Chlorophyll-a Concentration (monthly)
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10.1038/nature05317
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2022-03-24 15:24:14.972649+00:00
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2022-03-26 13:43:49.949095+00:00
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Contributing roughly half of the biosphere's net primary production (NPP), photosynthesis by oceanic phytoplankton is a vital link in the cycling of carbon between living and inorganic stocks. Each day, more than a hundred million tons of carbon in the form of CO2 are fixed into organic material by these ubiquitous, microscopic plants of the upper ocean, and each day a similar amount of organic carbon is transferred into marine ecosystems by sinking and grazing. The distribution of phytoplankton biomass and NPP is defined by the availability of light and nutrients (nitrogen, phosphate, iron). These growth-limiting factors are in turn regulated by physical processes of ocean circulation, mixed-layer dynamics, upwelling, atmospheric dust deposition, and the solar cycle. Satellite measurements of ocean colour provide a means of quantifying ocean productivity on a global scale and linking its variability to environmental factors. Here we describe global ocean NPP changes detected from space over the past decade. The period is dominated by an initial increase in NPP of 1,930 teragrams of carbon a year (Tg C yr(-1)), followed by a prolonged decrease averaging 190 Tg C yr(-1). These trends are driven by changes occurring in the expansive stratified low-latitude oceans and are tightly coupled to coincident climate variability. This link between the physical environment and ocean biology functions through changes in upper-ocean temperature and stratification, which influence the availability of nutrients for phytoplankton growth. The observed reductions in ocean productivity during the recent post-1999 warming period provide insight on how future climate change can alter marine food webs.
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https://choosealicense.com/no-permission/
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http://schema.org/name
Climate-driven trends in contemporary ocean productivity
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2022-03-24 15:24:14.972649+00:00
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http://purl.org/ontology/bibo/doi
10.1016/j.dsr.2013.09.002
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mailto:nordicesmhub@gmail.com
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https://doi.org/10.1016/j.dsr.2013.09.002
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mailto:nordicesmhub@gmail.com
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2022-03-24 15:30:02.881364+00:00
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2022-03-26 13:43:36.150459+00:00
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The relationship between the spring bloom along the Primorye coast and the sea ice of the Tatarskiy Strait in the northern region of the East/Japan Sea, a semi-enclosed marginal sea in the North Pacific, was investigated using the ten-year SeaWiFS chlorophyll-a concentration data and DMSP/SSMI sea ice concentration data from 1998 to 2007. Year-to-year variations in the chlorophyll-a concentrations in the spring were positively correlated with those of the sea ice concentrations in the Tatarskiy Strait in the previous winter with a correlation coefficient of 0.77. Abrupt increases in nutrients, essential for the spring bloom in the upper ocean during spring, were supplied from sea ice-melted waters. Time series of vertical distributions of the nutrients indicated that phosphate concentrations were extremely elevated in the upper ocean (less than 100 m) without any connection to high concentrations in the deep waters below. The water mass from sea ice provided preferable conditions for the spring bloom through changes in the vertical stratification structure of the water columns. Along-coast ratios of stability parameters between two neighboring months clearly showed the rapid progression of the generation of a shallow pycnocline due to fresh water originating from sea ice. This study addressed the importance of the physical environment for biogeochemical processes in semi-enclosed marginal seas affected by local sea ice.
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https://choosealicense.com/no-permission/
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http://schema.org/name
Role of sea ice on satellite-observed chlorophyll-a concentration variations during spring bloom in the East/Japan sea
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2022-03-24 15:30:02.881364+00:00
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Occurrence of an algal bloom under Arctic pack ice
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