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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: tcnpd

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
Pre-Ind_HadCM3 This is Emmas HadCM3 MOSES2.1 new pre-industrial control which uses new boundary conditions over Greenland based on the Letreguilly grid. It can be compared to the pre-industrial control tcnpc. 100 30 70 280 760 270 0 0 quest1 unknown 2008_07_23_16_50 2008_07_25_11_31
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 tcnpd

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 hPaVegetation Fractions
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
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 tcnpd-tcnpc

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 hPaVegetation Fractions
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
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 Nov 9 11:08:21 GMT 2015 This page is maintained by P.J.Valdes@bristol.ac.uk