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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: tdefj

parameter values are, , RHCRIT 0.6547, VF1 1.882, CT 0.0003021, CW_LAND 0.001688, CW_SEA 0.0004213, Z0FSEA 0.001195, KAY_GWAVE 1.992e%2B004, KAY_LEE_GWAVE 2.988e%2B005, ALPHAM 0.2152, DIFF_COEFF 4.078e%2B009, DIFF_COEFF_Q 2.335e%2B008, FNUB_SI 9.704e-006, KAPPA0_SI 9.704e-006, DKAPPA_DZ_SI 2.7e-008, FNU0_SI 0.005596, AM0_SI 1.387e%2B005, AM1_SI 1.387e%2B005, AHI1_SI 924.9, AHI2_SI 924.9, ATHKDF1_SI 924.9, ATHKDF2_SI 924.9.

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
Haney Forcing run for warm reduced gradient run. Parameters are the same as tcwiz, start dumps and reference ancil files as tcwiz6 (warm reduced pole to equator gradient in equilibrium). Strong Haney Forcing (163.76). 10 10 0 560 760 270 0 0 bigblue Intel_v10.1 2011_12_02_15_07 2012_02_28_09_30
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 tdefj

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)
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 Concentration
Stream Function at 200 hPa
Velocity Potential at 200 hPa
Divergence (Smoothed) at 200 hPa
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 10m
Ocean Mixed Layer DepthMass Streamfunction

Summary of Results for Experiment tdefj-tcyfa

Variable

DJFJJAANNMonthlyVariable
Surface Air TemperatureSurface Air Temperature Time Series
Total PrecipitationSurface Air Temperature Time Series (annual means)
Evaporation
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
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 10m
Ocean Mixed Layer DepthMass Streamfunction



Last updated This page is maintained by P.J.Valdes@bristol.ac.uk