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    <http://schema.org/dateCreated> "2022-03-18 17:20:59.339997+00:00" ;
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    <http://schema.org/description> """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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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
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    <http://schema.org/dateCreated> "2022-03-29 18:11:50.096041+00:00" ;
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    <http://schema.org/description> "This GeoJSON file contains two areas e.g. Bering Strait and Fram Strait. Model and observations of Chlorophyll concentrations are compared over these two areas." ;
    <http://schema.org/license> <https://choosealicense.com/no-permission/> ;
    <http://schema.org/name> "GeoJSON for Bering and Fram Straits" ;
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    <http://schema.org/contentUrl> "https://doi.org/10.1038/s41467-021-25699-w" ;
    <http://schema.org/creator> <mailto:nordicesmhub@gmail.com> ;
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    <http://schema.org/dateModified> "2022-03-26 13:44:02.088613+00:00" ;
    <http://schema.org/description> "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." ;
    <http://schema.org/license> <https://choosealicense.com/no-permission/> ;
    <http://schema.org/name> "Future phytoplankton diversity in a changing climate" ;
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