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Earth Systems Modelling Results

Bristol Research Initiative for the Dynamic Global Environment

Model Simulations

Experiment: xptda

Eurasia: 22.5-70N, 0-142.5E. UM designed bottom friction-spinup01. Present Day Orbit. Add two bathymetric ridges linking North pole and Eurasia, North America (if has) separately, with bathymetric: central -3500m, layer 18, surrounding -4500m, layer 19.

Set the Eurasia landmass to be reference landmass, the North pole island and South pole island to be islands/comparision landmasses. This series set new simplified and moved Eurasia landmass (22.5-70N, 0-142.5E) and Tibet (25-40N, 67.5-101.25E) if compare to Idealized_NoRidge series.

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
Eura_NoTibet Landmasses represent Eurasia, no Tibet. 4500 100 4400 280 760 270 0 0 bc4 Intel_v17_0.1_bc4 2024_01_03_21_34 2024_11_11_15_03
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 xptda

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

Variable

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



Last updated Tue Dec 3 19:36:20 GMT 2024 This page is maintained by P.J.Valdes@bristol.ac.uk