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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: tcosd

This run acts as the control global pre-industrial LAM run for Europe (tcosa)

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
Global_Driver_for_LAM_tcmfa This simulation was used to create the driving lateral boundary condition files for the European LAM for pre-industrial conditions. Configured using SST and sea ice from tcmfa3 but otherwise all boundary conditions same as standard. 40 25 15 280 760 270 0 0 bigblue Intel_v10.1 2009_06_08_21_25 2009_06_08_21_25
You can access the means 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 tcosd

Variable

DJFJJAANNMonthlyVariable
Surface Air TemperatureSurface Air Temperature Time Series
Total PrecipitationSurface Air Temperature Time Series (annual means)
EvaporationSoil Moisture in Layer 4 (Deepest layer)
Precipitation - EvaporationSoil Moisture in Layer 4 (Deepest layer) (annual means)
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 hPa
Divergence (Smoothed) at 200 hPa
Perturbation Height at 500 hPa
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

Summary of Results for Experiment tcosd-tcosc

Variable

DJFJJAANNMonthlyVariable
Surface Air TemperatureSurface Air Temperature Time Series
Total PrecipitationSurface Air Temperature Time Series (annual means)
EvaporationSoil Moisture in Layer 4 (Deepest layer)
Precipitation - EvaporationSoil Moisture in Layer 4 (Deepest layer) (annual means)
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 hPa
Divergence (Smoothed) at 200 hPa
Perturbation Height at 500 hPa
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



Last updated Wed Nov 18 13:17:19 GMT 2015 This page is maintained by P.J.Valdes@bristol.ac.uk