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Simulation of the Last Glacial Maximum using a two- dimensional energy balance model Modeling Past and Future Climate Changes A. Paul and M. Schulz.

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Presentation on theme: "Simulation of the Last Glacial Maximum using a two- dimensional energy balance model Modeling Past and Future Climate Changes A. Paul and M. Schulz."— Presentation transcript:

1 Simulation of the Last Glacial Maximum using a two- dimensional energy balance model Modeling Past and Future Climate Changes A. Paul and M. Schulz

2 Reading Hartmann, D. L., 1994: Global physical climatology, Academic Press. –Section 11.6: Modeling of Ice Age Climates –Section 9.4: Ice-albedo feedback North, G. R., Mengel, J. G. and Short, D. A.: Simple energy balance model resolving the seasons and the continents: Application to the astronomical theory of the ice ages. Journal of Geophysical Research 88, , 1983.

3 Fundamental equation Basic assumption: everything about climate can be characterized by surface temperature Conservation of energy in terms of –Absorbed solar energy –Emitted terrestrial energy –Energy removed by horizontal energy transport

4 time rate of change of the energy content of an atmosphere-ocean column of unit horizontal area outgoing longwave radiation incoming solar radiation removal of energy by horizontal transport in the atmosphere and ocean = - -

5 Parameterizations Horizontal energy transport is assumed to be diffusive Outgoing longwave radiation is assumed to be a linear function of surface temperature and a logarithmic function of the atmospheric CO 2 concentration.

6 Discretization The horizontal resolution  x   y is 10°  10° –36  18 grid cells The time step  t is about one day.

7 Numerical experiments Experiment E1: control experiment, present-day land fraction, land-ice cover and CO 2 Experiment E2: glacial land-ice distribution (but still present-day land fraction) –co2ccn=280, ice_yr= Experiment E3: glacial CO 2 concentration –co2ccn=180, ice_yr=0.0 Experiment E4: glacial land-ice distribution and CO 2 concentration –co2ccn=180, ice_yr=

8 Go to the website: bremen.de/~apau/models/ebm_2d/ Downlowd the zip -file ebm_2d_1.1.zip (1.8 MB) to your “My Documents” directory Click on right-hand mouse button to „Extract All…“ files to a directory called: ebm_2d_1.1

9 Directory structure: –doc : contains the ppt file of the exercise –output : contains example MATLAB M-files (adapt to your needs) import_data : to import model output in netCDF format plot_data : to plot a specific variable from the model output plot_diff : to import the model output of two experiments to plot the difference in one specific variable global_mean : to compute the area-weighted global mean of a latitude-longitude field

10 work : –contains the executable program ebm_2d.exe for Windows, as well as compile scripts and a makefile if you want to build the model from the sources. –contains the parameter input file ebm.in

11 For all experiments, the run length runlen is taken to be 50 years (which is roughly the equilibrium timescale of the ocean mixed layer), and the time step dt is set to 1 day. The total CPU time required for one experiment : about 13 s (for Intel Pentium GHz)

12 Boundary conditions Land fraction and land-ice fraction are read from file. Surface albedo is read from file (data from McGuffie and Henderson-Sellers, zonally averaged). Atmospheric CO 2 concentration can be changed through namelist.

13 Land fraction - fraction of 10°  10° grid cell covered by land: 1.0  grid cell is completely land-covered, 0.0  grid cell is completely ocean-covered.

14 Present-day land-ice fraction - fraction of 10°  10° grid cell covered by land ice: 1.0  grid cell is completely land ice-covered, 0.0  grid cell is completely land ice-free. E1/E3

15 LGM land-ice fraction - fraction of 10°  10° grid cell covered by land ice: 1.0  grid cell is completely land ice-covered, 0.0  grid cell is completely land ice-free. E2/E4

16 Exercise Carry out experiments E1 to E4, one after the other. Prepare a table that lists the global-mean temperature for each experiment. Plot the time-averaged sea-level air temperature for each experiment, as well as the change from one experiment to the next. –Describe characteristic features (maximum changes, patterns) of the temperature anomalies. Key question: From your series of experiments, which mechanism makes ice ages simultaneous in both hemispheres?

17 Experimental procedure To run the model, first double-click on start_cygwin To check and change the model parameters, type notepad ebm.in & on the cygwin commandline and press. –For your first experiment “E1”, set ice_yr to 0.0 and co2ccn to To start the model, type ebm_2d on the cygwin command line and press. Upon completion of the run, the model outputs the total number of time steps performed ittmax, the number of time steps per year ntyear and the area-weighted global mean temperature at the end of the experiment in °C tgmean.

18 After running the model, rename the output file. –For example, from snapshot_ebm.nc to snapshot_ebm_E1.nc Visualize the output using MATLAB. –Alternatively, you could use ferret or Panoply. To prepare the next experiment, change the input parameter(s) in the file ebm.in accordingly –For example, change ice_yr from 0.0 to

19 Sample MATLAB session Start MATLAB. Point “Current Directory” to output (the full path name is probably: C:\Documents and Settings\geo\My Documents\ebm_2d_1.1\output ) Take the time to inspect the M-files provided in the MATLAB editor (you can open them using File > Open ). Initialize all MATLAB paths by typing start in the “Command Window”. Import the model output using: import_data –This M-file script lists the variables contained in the model output file (see table). To plot, e.g. the time-averaged sea-level air temperature ta_at, try: plot_data. –If you want to plot a different variable, edit the M-file script plot_data.m accordingly, or use the MATALAB Command Window.

20 Variables contained in model output file lfrac land fraction of a grid cell aicel land-ice fraction of a grid cell slat sea-level air temperature ta_at time-averaged sea-level air temperature apln planetary albedo netswpln net shortwave planetary radiation netlwpln net longwave planetary radiation tmax annual maximum temperature

21 To plot the temperature difference between two experiments, inspect the M- file script: plot_diff.m To compute the area-weighted global mean of a latitude-longitude field like ta_at, use global_mean(xt,yt,ta_at)

22 Sample ferret session Double_click start_ferret in output folder Type ferret and press Type use snapshot_ebm (and press ) To shade sea-level air temperature: type shade ta_at To compute global-mean temperature: type list

23 Sym- bol Fortran name DescriptionUnit runlen length of runyears tt dt time stepdays h ice_yr ice-sheet forcing year (-/+ = BC/AD) yr tinit initial temperature°C ice_albedo_feedback flag for ice-albedo feedback Input parameters in file “ebm.in”:

24 Differences to text book example Experiment missing with respect to Section 11.6 by Hartmann (1994): Change in snow-free surface albedo that would correspond to the land conditions for the last glacial age –associated with changes in the vegetation and soil Furthemore, 2D EBM does not contain explicit „50-m-deep mixed-layer ocean“, which would allow the prediction of SST.


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