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Earth Systems Modelling Results

Bristol Research Initiative for the Dynamic Global Environment

with the

University of Reading, Open University, and the British Antarctic Survey.

Model Simulations

Experiment: texPc2

Scientifically as benchmark except using water age update, dark respiration, salinity conservation and revised ozone. Also using new orbital and solar update, and outputting leaf CO2.

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
142_4_MaBP This is the 142.4 Ma simulation using the Scotese palaeogeographies. 3000 100 2900 831.71 760 270 0 0 bc4 Intel_v17_0.1_bc4 2018_12_14_10_49 2018_12_16_21_13
You can access the means from this run, by going here
You can access the ocean integrals from this run, by going 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 texPc2

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 Concentration
Stream Function at 200 hPa
Velocity Potential at 200 hPaVegetation Fractions
Divergence (Smoothed) at 200 hPaSoil Carbon Time Series
Perturbation Height at 500 hPa
Meridional Stream Function
Ocean Potential Temperature at 5mOcean Potential Temperature at 2116m
Ocean Salinity at 5mOcean Salinity at 2116m
Ocean Currents at 5mOcean Currents at 2116m
Ocean Vertical Velocity at 10mOcean Vertical Velicity at 2424m
Ocean Mixed Layer DepthMass Streamfunction

Summary of Results for Experiment texPc2-texPc1

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 - Evaporation
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 Concentration
Stream Function at 200 hPa
Velocity Potential at 200 hPaVegetation Fractions
Divergence (Smoothed) at 200 hPaSoil Carbon Time Series
Perturbation Height at 500 hPa
Meridional Stream Function
Ocean Potential Temperature at 5mOcean Potential Temperature at 2116m
Ocean Salinity at 5mOcean Salinity at 2116m
Ocean Currents at 5mOcean Currents at 2116m
Ocean Vertical Velocity at 10mOcean Vertical Velicity at 2424m
Ocean Mixed Layer DepthMass Streamfunction



Last updated Mon May 20 02:12:39 BST 2019 This page is maintained by P.J.Valdes@bristol.ac.uk