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Earth Systems Modelling Results

Bristol Research Initiative for the Dynamic Global Environment

Model Simulations

Experiment: tfjja

A long description of this run is currently not available

Brief Description Fuller Description Total Length of Run (in years) Averaging period (in years) Spinup period (in years) CO2 (in ppmv) CH4 (in ppbv) N2O (in ppbv) CFC11 (in pptv) CFC12 (in pptv) Computer used for simulation Compiler used for simulation Date of first entry in datebase Date of most recent modification to entry in database
Chg_Phase7 Changhsingian simulation. New Phys (CCN/desert/diff). New CO2 (2x Foster, et al.) Initialised from tfgsi (3419 years in). 6000 100 5900 1712 760 270 0 0 bc4 Intel_v17_0.1_bc4 2022_04_01_15_11 2022_04_01_15_11
You can access the means from this run, by going here
You can access the ocean integrals from this run, by going here
And noise diagnostics here


This page shows a small subset of images from this simulation. They have already been produced and there are no optional choices. If you want to do a more detailed examination of the model results, you can go to the main page and select one of the Parts. This will give you full access the system



Summary of Results for Experiment tfjja

Atlantic Meridional Overturning StrengthDepth of Max Atlantic OverturningLatitude of Max Atlantic Overturning

Variable

DJFJJAANNMonthlyVariable
Surface Air TemperatureSurface Air Temperature Time Series
Total PrecipitationSurface Air Temperature Time Series (annual means)
EvaporationSoil Moisture in Layer 4 (Deepest layer) (annual means)
Precipitation - EvaporationGregory Plot (10 year running mean)
Fractional Plant Stress (layer 1)BIOME4
Mean Sea Level PressureBIOME4 with CO2 changed
Total Cloud Cover
Plantary AlbedoWarm Month Mean
Surface AlbedoCold Month Mean
Sea Ice ConcentrationMean Annual Temperature Cycle
Stream Function at 200 hPaMean Annual Precipitation Cycle
Velocity Potential at 200 hPaVegetation Fractions
Divergence (Smoothed) at 200 hPa
Perturbation Height at 500 hPaVegetation-Climate
Meridional Stream Function
High Pass Eddy Kinetic Energy at 200 hPa
Low Pass Eddy Kinetic Energy at 200 hPa
High Pass Temperature Flux at 850 hPa
Ocean Potential Temperature at 5mOcean Potential Temperature at 2116m
Ocean Salinity at 5mOcean Salinity at 2116m
Ocean Currents at 5mOcean Currents at 2116m
Ocean Horizontal StreamfunctionAtmos/Ocean Heat Transport
Ocean Vertical Velocity at 10mOcean Vertical Velocity at 2424m
Ocean Mixed Layer DepthMass Streamfunction



Last updated Tue Jun 21 22:54:49 BST 2022 This page is maintained by P.J.Valdes@bristol.ac.uk