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Earth Systems Modelling Results

Bristol Research Initiative for the Dynamic Global Environment

Model Simulations

Experiment: xptdn

Present Day Orbit.

Set the Eurasia_Africa_India landmass to be reference landmass, the North pole island and South pole island to be islands/comparision landmasses. New simplified and moved Eurasia_Africa_India landmass and Tibet if compare to Idealized_NoRidge series.


And noise diagnostics here
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
LSM-EuraIndAfrNA_SST-EuraIndAfr HadAM3 model. Land-sea mask is the same with job xptdf-EuraIndAfrNA_NoTibet, while SST and sea ice are using the 4400-4500 year climatologly of job xptdc-Eurasia_Africa_India. 300 100 200 280 760 270 0 0 bc4 Intel_v17_0.1_bc4 2024_03_21_18_22 2024_11_11_19_41
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 xptdn

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 ConcentrationMean Annual Temperature Cycle
Stream Function at 200 hPaMean Annual Precipitation Cycle
Velocity Potential at 200 hPaVegetation Fractions
Divergence (Smoothed) at 200 hPaSoil Carbon Time Series
Perturbation Height at 500 hPaVegetation-Climate
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 Tue Dec 3 20:36:51 GMT 2024 This page is maintained by P.J.Valdes@bristol.ac.uk