Bristol Research Initiative for the Dynamic Global
Environment
Model Simulations
Experiment: temqa
This is the 00.0 kyr BP simulation for an extension of the temi series but with CO2 set to the 100 year means of the transient runs. Deglaciation BBC runs using Peltier6g and TRIFFID. Dynamic mode. Lots of STASH.
This job is a standard version of HadCM3M2.1D (dynamic TRIFFID) originally based on tdaae. However, it has a number of additions/changes. These include: (1) the dark_respiration update is included, (2) the updated (bug fixed) orbital update, (3) salinity conservation is included, (4) age of water tracer included (5) bottom friction and lots of bug fixes. One executable can be used for all time periods
The boundary conditions are (a) peltier6g, used in anomaly mode, (b) GHGs from the latest estimates, (c) global salinity is 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 continuation of temi series but lots of small improvements in the model plus orbital bug corrected
350
100
250
284
808
273
0
0
bc4
Intel_v17.0.1_bc4
2024_07_30_09_13
2024_07_30_09_13
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 temqa
Atlantic Meridional Overturning Strength
Depth of Max Atlantic Overturning
Latitude of Max Atlantic Overturning
Variable
DJF
JJA
ANN
Monthly
Variable
Surface Air Temperature
Surface Air Temperature Time Series
Total Precipitation
Surface Air Temperature Time Series (annual means)
Evaporation
Soil Moisture in Layer 4 (Deepest layer) (annual means)
Precipitation - Evaporation
Gregory Plot (10 year running mean)
Fractional Plant Stress (layer 1)
BIOME4
Mean Sea Level Pressure
BIOME4 with CO2 changed
Total Cloud Cover
BIOME4 with CO2 changed and anomaly of climate
Plantary Albedo
Warm Month Mean
Surface Albedo
Cold Month Mean
Sea Ice Concentration
Mean Annual Temperature Cycle
Stream Function at 200 hPa
Mean Annual Precipitation Cycle
Velocity Potential at 200 hPa
Vegetation Fractions
Divergence (Smoothed) at 200 hPa
Soil Carbon Time Series
Perturbation Height at 500 hPa
Vegetation-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
Ocean Potential Temperature at 5m
Ocean Potential Temperature at 2116m
Ocean Salinity at 5m
Ocean Salinity at 2116m
Ocean Currents at 5m
Ocean Currents at 2116m
Ocean Horizontal Streamfunction
Atmos/Ocean Heat Transport
Ocean Vertical Velocity at 10m
Ocean Vertical Velocity at 2424m
Ocean Mixed Layer Depth
Mass Streamfunction
Summary of Results for Experiment temqa-temia1
Atlantic Meridional Overturning Strength
Depth of Max Atlantic Overturning
Latitude of Max Atlantic Overturning
Variable
DJF
JJA
ANN
Monthly
Variable
Surface Air Temperature
Surface Air Temperature Time Series
Total Precipitation
Surface Air Temperature Time Series (annual means)
Evaporation
Soil Moisture in Layer 4 (Deepest layer) (annual means)
