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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: temma

This is a continuation of temaa except that (a) the mass of the atmosphere has been corrected to the same as the control. and (b) we are not longer using the salinity conservation update but instead using a revised waterfix.

This job is a standard version of HadCM3M2.1D (dynamic TRIFFID) based on tdaae. However, it has a number of small additions/changes. These include: (1) the dark_respiration update is included, (2) the orbital update as in FAMOUS, (3) salinity conservation is included, (4) age of water tracer included. One executable can be used for all time periods

The boundary conditions are (a) GLAC-1D, used in anomaly mode, (b) GHGs from the latest estimates, (c) global salinity approx 1PSU more at LGM and scaled with sealevel for other periods (d) orbital changes via FAMOUS update (default is Berger and Loutre 1991)

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
00.0kyr_BP This is the 00.0 kyr BP simulation for a new set of deglaciation BBC runs using GLAC-1D and TRIFFID. Dynamic mode. No meltwater. Russian rivers routed to Med but only during height of glacial. 880 100 780 284 808 273 0 0 bc4 Intel_v17_0.1_bc4 2018_01_17_16_28 2018_01_17_16_32
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 temma

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) (annual means)
Precipitation - EvaporationGregory Plot (10 year running mean)
Fractional Plant Stress (layer 1)BIOME4
Mean Sea Level PressureBIOME4 with CO2 changed
Total Cloud CoverBIOME4 with CO2 changed and anomaly of climate
Plantary AlbedoWarm Month Mean
Surface AlbedoCold Month Mean
Sea Ice Concentration
Stream Function at 200 hPa
Velocity Potential at 200 hPaVegetation Fractions
Divergence (Smoothed) at 200 hPaSoil Carbon Time Series
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 10mOcean Vertical Velicity at 2424m
Ocean Mixed Layer DepthMass Streamfunction

Summary of Results for Experiment temma-temka

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) (annual means)
Precipitation - Evaporation
Fractional Plant Stress (layer 1)BIOME4
Mean Sea Level PressureBIOME4 with CO2 changed
Total Cloud CoverBIOME4 with CO2 changed and anomaly of climate
Plantary AlbedoWarm Month Mean
Surface AlbedoCold Month Mean
Sea Ice Concentration
Stream Function at 200 hPa
Velocity Potential at 200 hPaVegetation Fractions
Divergence (Smoothed) at 200 hPaSoil Carbon Time Series
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 10mOcean Vertical Velicity at 2424m
Ocean Mixed Layer DepthMass Streamfunction



Last updated Tue May 26 05:37:58 BST 2020 This page is maintained by P.J.Valdes@bristol.ac.uk