diff --git a/.github/workflows/export-cmor-cvs-table.yaml b/.github/workflows/export-cmor-cvs-table.yaml index 6511b32f..7669fce2 100644 --- a/.github/workflows/export-cmor-cvs-table.yaml +++ b/.github/workflows/export-cmor-cvs-table.yaml @@ -26,7 +26,7 @@ jobs: ESGVOC_REVISION: "5145b8f6d8b1859c663e63fb7b0bad952e8bc7b5" # Modify these as needed UNIVERSE_CVS_FORK: "znichollscr" - UNIVERSE_CVS_BRANCH: "cmip-description" + UNIVERSE_CVS_BRANCH: "add-piclim-experiments" CMIP7_CVS_FORK: ${{ github.event.pull_request.head.repo.owner.login }} CMIP7_CVS_BRANCH: ${{ github.head_ref || github.ref_name }} run: | diff --git a/activity/aerchemmip.json b/activity/aerchemmip.json index 337b0574..792d56c8 100644 --- a/activity/aerchemmip.json +++ b/activity/aerchemmip.json @@ -7,6 +7,11 @@ "esm-scen7-h-aq", "esm-scen7-vl-aer", "esm-scen7-vl-aq", + "piclim-ch4", + "piclim-n2o", + "piclim-nox", + "piclim-ods", + "piclim-so2", "scen7-h-aer", "scen7-h-aq", "scen7-vl-aer", diff --git a/activity/cmip.json b/activity/cmip.json index 497fa5ca..fea28c3a 100644 --- a/activity/cmip.json +++ b/activity/cmip.json @@ -11,6 +11,9 @@ "esm-picontrol", "esm-picontrol-spinup", "historical", + "piclim-4xco2", + "piclim-anthro", + "piclim-control", "picontrol", "picontrol-spinup" ], diff --git a/activity/rfmip.json b/activity/rfmip.json new file mode 100644 index 00000000..3c9a88c8 --- /dev/null +++ b/activity/rfmip.json @@ -0,0 +1,14 @@ +{ + "@context": "000_context.jsonld", + "id": "rfmip", + "type": "activity", + "experiments": [ + "piclim-aer", + "piclim-histaer", + "piclim-histall" + ], + "urls": [ + "https://doi.org/10.5194/acp-20-9591-2020", + "https://doi.org/10.5194/gmd-9-3447-2016" + ] +} diff --git a/cmor-cvs.json b/cmor-cvs.json index 5b88b86b..90613abb 100644 --- a/cmor-cvs.json +++ b/cmor-cvs.json @@ -10,10 +10,11 @@ "AerChemMIP": "Aerosols and chemistry model intercomparison project: exploration of aerosol chemistry.", "C4MIP": "Coupled climate carbon cycle model intercomparison project: exploration of the response of the coupled carbon-climate system.", "CFMIP": "Cloud feedback model intercomparison project. Focussed primarily on cloud feedbacks with a secondary focus on understanding of response to forcing, model biases, circulation, regional-scale precipitation, and non-linear changes.", - "CMIP": "CMIP core common experiments i.e. the DECK (Diagnostic, Evaluation and Characterization of Klima) and historical.", + "CMIP": "CMIP core common experiments i.e. the DECK (Diagnostic, Evaluation and Characterization of Klima).", "DAMIP": "Detection and attribution model intercomparison project: exploration of the role of individual forcings (both anthropogenic and natural) in past and future climate change.", "GeoMIP": "Geoengineering model intercomparison project: exploration of the climate response to solar radiation manipulation.", "PMIP": "Palaeoclimate modelling intercomparison project: assessment of paleoclimate i.e. climate thousands of years or more in the past.", + "RFMIP": " Radiative Forcing Model Intercomparison Project: characterisation of radiative forcing within models.", "ScenarioMIP": "Future scenario experiments. Exploration of the future climate under a (selected) range of possible boundary conditions. In CMIP7, the priority tier for experiments is conditional on whether you are doing emissions- or concentration-driven simulations. There is no way to express this in the CVs (nor time to implement something to handle this conditionality). This means that, for your particular situation, some experiments may be at a lower tier than is listed in the CVs. For example, the `vl` scenario is tier 1 for concentration-driven models and tier 2 for emissions-driven models. However, in the CVs, we have used the highest priority tier (across all the possible conditionalities). Hence `vl` is listed as tier 1 in the CVs (even though it is actually tier 2 for emissions-driven models).For details, please see the full description in the ScenarioMIP description papers." }, "area_label": { @@ -361,6 +362,42 @@ "start_year": 2022, "tier": 1 }, + "esm-scen7-h-AQ": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `esm-scen7-h-Aer` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `esm-scen7-h-Aer` instead.", + "experiment_id": "esm-scen7-h-AQ", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "esm-hist" + ], + "start_year": 2022, + "tier": 1 + }, + "esm-scen7-h-Aer": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `esm-scen7-h-Aq` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `esm-scen7-h-Aq` instead.", + "experiment_id": "esm-scen7-h-Aer", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "esm-hist" + ], + "start_year": 2022, + "tier": 1 + }, "esm-scen7-h-ext": { "activity_id": [ "ScenarioMIP" @@ -577,6 +614,42 @@ "start_year": 2022, "tier": 1 }, + "esm-scen7-vl-AQ": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `esm-scen7-vl-Aer` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `esm-scen7-vl-Aer` instead.", + "experiment_id": "esm-scen7-vl-AQ", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "esm-hist" + ], + "start_year": 2022, + "tier": 1 + }, + "esm-scen7-vl-Aer": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `esm-scen7-vl-Aq` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `esm-scen7-vl-Aq` instead.", + "experiment_id": "esm-scen7-vl-Aer", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "esm-hist" + ], + "start_year": 2022, + "tier": 1 + }, "esm-scen7-vl-ext": { "activity_id": [ "ScenarioMIP" @@ -667,6 +740,160 @@ "start_year": 1850, "tier": 1 }, + "piClim-4xCO2": { + "activity_id": [ + "CMIP" + ], + "description": "In combination with `piClim-control`, quantifies a quadrupling of atmospheric carbon dioxide's (4xCO2's) effective radiative forcing (ERF). Same as `piClim-control`, except atmospheric carbon dioxide concentrations are set to four times `piControl` levels.", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies a quadrupling of atmospheric carbon dioxide's (4xCO2's) effective radiative forcing (ERF). Same as `piClim-control`, except atmospheric carbon dioxide concentrations are set to four times `piControl` levels.", + "experiment_id": "piClim-4xCO2", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-CH4": { + "activity_id": [ + "AerChemMIP" + ], + "description": "In combination with `piClim-control`, quantifies present-day methane effective radiative forcing (ERF). Same as `piClim-control`, except methane concentrations or emissions (as appropriate for the model) use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies present-day methane effective radiative forcing (ERF). Same as `piClim-control`, except methane concentrations or emissions (as appropriate for the model) use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "experiment_id": "piClim-CH4", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-N2O": { + "activity_id": [ + "AerChemMIP" + ], + "description": "In combination with `piClim-control`, quantifies present-day nitrous oxide effective radiative forcing (ERF). Same as `piClim-control`, except nitrous oxide concentrations or emissions (as appropriate for the model) use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies present-day nitrous oxide effective radiative forcing (ERF). Same as `piClim-control`, except nitrous oxide concentrations or emissions (as appropriate for the model) use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "experiment_id": "piClim-N2O", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-NOx": { + "activity_id": [ + "AerChemMIP" + ], + "description": "In combination with `piClim-control`, quantifies present-day nitrous oxide (NOx) effective radiative forcing (ERF). Same as `piClim-control`, except nitrous oxide (NOx) emissions use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies present-day nitrous oxide (NOx) effective radiative forcing (ERF). Same as `piClim-control`, except nitrous oxide (NOx) emissions use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "experiment_id": "piClim-NOx", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-ODS": { + "activity_id": [ + "AerChemMIP" + ], + "description": "In combination with `piClim-control`, quantifies present-day ozone-depleting substances' effective radiative forcing (ERF). Same as `piClim-control`, except ozone-depleting substances concentrations use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies present-day ozone-depleting substances' effective radiative forcing (ERF). Same as `piClim-control`, except ozone-depleting substances concentrations use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "experiment_id": "piClim-ODS", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-SO2": { + "activity_id": [ + "AerChemMIP" + ], + "description": "In combination with `piClim-control`, quantifies present-day sulfur (dioxide) effective radiative forcing (ERF). Same as `piClim-control`, except sulfur emissions use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies present-day sulfur (dioxide) effective radiative forcing (ERF). Same as `piClim-control`, except sulfur emissions use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "experiment_id": "piClim-SO2", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-aer": { + "activity_id": [ + "RFMIP" + ], + "description": "In combination with `piClim-control`, quantifies present-day aerosol effective radiative forcing (ERF). Same as `piClim-control`, except anthropogenic aerosol emissions use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies present-day aerosol effective radiative forcing (ERF). Same as `piClim-control`, except anthropogenic aerosol emissions use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "experiment_id": "piClim-aer", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-anthro": { + "activity_id": [ + "CMIP" + ], + "description": "In combination with `piClim-control`, quantifies present-day total anthropogenic effective radiative forcing (ERF). Same as `piClim-control`, except all anthropogenic forcings use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "end_year": "", + "experiment": "In combination with `piClim-control`, quantifies present-day total anthropogenic effective radiative forcing (ERF). Same as `piClim-control`, except all anthropogenic forcings use present-day values (typically the last year of the `historical` simulation within the same CMIP era e.g. 2014 values for CMIP6, 2021 values for CMIP7).", + "experiment_id": "piClim-anthro", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-control": { + "activity_id": [ + "CMIP" + ], + "description": "Baseline for effective radiative forcing (ERF) calculations. `piControl` with prescribed sea-surface temperatures and sea-ice concentrations.", + "end_year": "", + "experiment": "Baseline for effective radiative forcing (ERF) calculations. `piControl` with prescribed sea-surface temperatures and sea-ice concentrations.", + "experiment_id": "piClim-control", + "min_number_yrs_per_sim": 30, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": "", + "tier": 1 + }, + "piClim-histaer": { + "activity_id": [ + "RFMIP" + ], + "description": "Simulation of the historical and future period with prescribed sea-surface temperatures and sea-ice concentrations (the slightly confusing name is a legacy thing). Aerosol emissions follow the `historical` experiment then the `scen7-m` or `esm-scen7-m` experiment (whichever is relevant to your model setup) while all other forcings follow `piControl` to allow for a (approximate) diagnosis of transient historical aerosol effective radiative forcing (ERF) (can be compared with `piClim-aer` which provides a more precise quantification of present-day aerosol ERF).", + "end_year": 2100, + "experiment": "Simulation of the historical and future period with prescribed sea-surface temperatures and sea-ice concentrations (the slightly confusing name is a legacy thing). Aerosol emissions follow the `historical` experiment then the `scen7-m` or `esm-scen7-m` experiment (whichever is relevant to your model setup) while all other forcings follow `piControl` to allow for a (approximate) diagnosis of transient historical aerosol effective radiative forcing (ERF) (can be compared with `piClim-aer` which provides a more precise quantification of present-day aerosol ERF).", + "experiment_id": "piClim-histaer", + "min_number_yrs_per_sim": 251, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": 1850, + "tier": 1 + }, + "piClim-histall": { + "activity_id": [ + "RFMIP" + ], + "description": "Simulation of the historical period with prescribed sea-surface temperatures and sea-ice concentrations (the slightly confusing name is a legacy thing). All forcings follow the `historical` experiment then the `scen7-m` or `esm-scen7-m` experiment (whichever is relevant to your model setup) to allow for a (approximate) diagnosis of transient historical effective radiative forcing (ERF) (can be compared with the `piClim-*` experiments which provide a more precise quantification of present-day ERF from various forcers).", + "end_year": 2100, + "experiment": "Simulation of the historical period with prescribed sea-surface temperatures and sea-ice concentrations (the slightly confusing name is a legacy thing). All forcings follow the `historical` experiment then the `scen7-m` or `esm-scen7-m` experiment (whichever is relevant to your model setup) to allow for a (approximate) diagnosis of transient historical effective radiative forcing (ERF) (can be compared with the `piClim-*` experiments which provide a more precise quantification of present-day ERF from various forcers).", + "experiment_id": "piClim-histall", + "min_number_yrs_per_sim": 251, + "parent_activity_id": [], + "parent_experiment_id": [], + "start_year": 1850, + "tier": 1 + }, "piControl": { "activity_id": [ "CMIP" @@ -717,6 +944,42 @@ "start_year": 2022, "tier": 1 }, + "scen7-h-AQ": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `scen7-h-Aer` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `scen7-h-Aer` instead.", + "experiment_id": "scen7-h-AQ", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "historical" + ], + "start_year": 2022, + "tier": 1 + }, + "scen7-h-Aer": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `scen7-h-Aq` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP high emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `scen7-h-Aq` instead.", + "experiment_id": "scen7-h-Aer", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "historical" + ], + "start_year": 2022, + "tier": 1 + }, "scen7-h-ext": { "activity_id": [ "ScenarioMIP" @@ -933,6 +1196,42 @@ "start_year": 2022, "tier": 1 }, + "scen7-vl-AQ": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `scen7-vl-Aer` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models with interactive chemistry. Models without interactive chemistry should run `scen7-vl-Aer` instead.", + "experiment_id": "scen7-vl-AQ", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "historical" + ], + "start_year": 2022, + "tier": 1 + }, + "scen7-vl-Aer": { + "activity_id": [ + "AerChemMIP" + ], + "description": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `scen7-vl-Aq` instead.", + "end_year": 2100, + "experiment": "PLACEHOLDER TBC. CMIP7 ScenarioMIP very low emissions future. Altered to use high aerosol and tropospheric non-methane ozone precursor emissions. This is for models without interactive chemistry. Models with interactive chemistry should run `scen7-vl-Aq` instead.", + "experiment_id": "scen7-vl-Aer", + "min_number_yrs_per_sim": 79, + "parent_activity_id": [ + "CMIP" + ], + "parent_experiment_id": [ + "historical" + ], + "start_year": 2022, + "tier": 1 + }, "scen7-vl-ext": { "activity_id": [ "ScenarioMIP" @@ -1055,10 +1354,10 @@ "seaIce": "Dataset of primary interest in studying sea ice." }, "region": { - "30S-90S": "The region south of the latitude 30S.", + "30S-90S": "The geographical region of the Earth\u2019s surface between 30 and 90 degrees south.", "ata": "Antarcica.", - "glb": "The entire globe i.e. earth.", - "grl": "Greenland.", + "glb": "The geographical region of the whole of the Earth\u2019s surface, as defined by the CF conventions.", + "grl": "The geographical region of Greenland, as defined by the CF conventions.", "nh": "The Northern Hemisphere.", "sh": "The Southern Hemisphere." }, @@ -1153,6 +1452,7 @@ "h40": "Data is reported at 40 height levels", "ol": "Data is reported on the model's ocean model levels.", "olh": "Data is reported on the model's ocean model half-levels (i.e. at the interfaces between model vertical layers).", + "ols": "Data is reported for the surface level of the model's ocean model.", "op4": "Data is reported at 4 ocean pressure layers.", "p19": "Data is reported at 19 pressure levels.", "p27": "Data is reported at 27 pressure levels.", diff --git a/create-cmor-cvs-table-export-environment.sh b/create-cmor-cvs-table-export-environment.sh index 4539b83f..e4a16f94 100644 --- a/create-cmor-cvs-table-export-environment.sh +++ b/create-cmor-cvs-table-export-environment.sh @@ -7,9 +7,9 @@ python3.13 -m venv venv ESGVOC_FORK="znichollscr" ESGVOC_REVISION="5145b8f6d8b1859c663e63fb7b0bad952e8bc7b5" UNIVERSE_CVS_FORK="znichollscr" -UNIVERSE_CVS_BRANCH="cmip-description" +UNIVERSE_CVS_BRANCH="add-piclim-experiments" CMIP7_CVS_FORK="znichollscr" -CMIP7_CVS_BRANCH="cmip-description" +CMIP7_CVS_BRANCH="add-piclim-experiments" venv/bin/pip install -r requirements-cmor-cvs-table.txt venv/bin/pip install --no-deps "git+https://github.com/$ESGVOC_FORK/esgf-vocab.git@$ESGVOC_REVISION" diff --git a/experiment/piclim-4xco2.json b/experiment/piclim-4xco2.json new file mode 100644 index 00000000..8f088713 --- /dev/null +++ b/experiment/piclim-4xco2.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-4xco2", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-aer.json b/experiment/piclim-aer.json new file mode 100644 index 00000000..9e808a8e --- /dev/null +++ b/experiment/piclim-aer.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-aer", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-anthro.json b/experiment/piclim-anthro.json new file mode 100644 index 00000000..5c8be007 --- /dev/null +++ b/experiment/piclim-anthro.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-anthro", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-ch4.json b/experiment/piclim-ch4.json new file mode 100644 index 00000000..3c7bd73d --- /dev/null +++ b/experiment/piclim-ch4.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-ch4", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-control.json b/experiment/piclim-control.json new file mode 100644 index 00000000..0091204b --- /dev/null +++ b/experiment/piclim-control.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-control", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-histaer.json b/experiment/piclim-histaer.json new file mode 100644 index 00000000..80b51bd5 --- /dev/null +++ b/experiment/piclim-histaer.json @@ -0,0 +1,10 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-histaer", + "type": "experiment", + "description": "Simulation of the historical and future period with prescribed sea-surface temperatures and sea-ice concentrations (the slightly confusing name is a legacy thing). Aerosol emissions follow the `historical` experiment then the `scen7-m` or `esm-scen7-m` experiment (whichever is relevant to your model setup) while all other forcings follow `piControl` to allow for a (approximate) diagnosis of transient historical aerosol effective radiative forcing (ERF) (can be compared with `piClim-aer` which provides a more precise quantification of present-day aerosol ERF).", + "start_timestamp": "1850-01-01", + "end_timestamp": "2100-12-31", + "min_number_yrs_per_sim": 251.0, + "tier": 1 +} diff --git a/experiment/piclim-histall.json b/experiment/piclim-histall.json new file mode 100644 index 00000000..3a74ba4c --- /dev/null +++ b/experiment/piclim-histall.json @@ -0,0 +1,10 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-histall", + "type": "experiment", + "description": "Simulation of the historical period with prescribed sea-surface temperatures and sea-ice concentrations (the slightly confusing name is a legacy thing). All forcings follow the `historical` experiment then the `scen7-m` or `esm-scen7-m` experiment (whichever is relevant to your model setup) to allow for a (approximate) diagnosis of transient historical effective radiative forcing (ERF) (can be compared with the `piClim-*` experiments which provide a more precise quantification of present-day ERF from various forcers).", + "start_timestamp": "1850-01-01", + "end_timestamp": "2100-12-31", + "min_number_yrs_per_sim": 251.0, + "tier": 1 +} diff --git a/experiment/piclim-n2o.json b/experiment/piclim-n2o.json new file mode 100644 index 00000000..44ce24f8 --- /dev/null +++ b/experiment/piclim-n2o.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-n2o", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-nox.json b/experiment/piclim-nox.json new file mode 100644 index 00000000..8fe3df24 --- /dev/null +++ b/experiment/piclim-nox.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-nox", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-ods.json b/experiment/piclim-ods.json new file mode 100644 index 00000000..6a43c8af --- /dev/null +++ b/experiment/piclim-ods.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-ods", + "type": "experiment", + "tier": 1 +} diff --git a/experiment/piclim-so2.json b/experiment/piclim-so2.json new file mode 100644 index 00000000..076820e9 --- /dev/null +++ b/experiment/piclim-so2.json @@ -0,0 +1,6 @@ +{ + "@context": "000_context.jsonld", + "id": "piclim-so2", + "type": "experiment", + "tier": 1 +} diff --git a/vertical_label/ols.json b/vertical_label/ols.json new file mode 100644 index 00000000..708dbd4d --- /dev/null +++ b/vertical_label/ols.json @@ -0,0 +1,5 @@ +{ + "@context": "000_context.jsonld", + "id": "ols", + "type": "vertical_label" +}