In the exercise you will set up and test a simple climate model that considers solar radiation, greenhouse gases and clouds. For an overview of how the model works visit this webpage.
MATLAB is available on the University clusters. Do not worry if you are unsure how to use it: by week 4 you will have been introduced to it in the data analysis course.The following MATLAB files can be downloaded and put into your working directory in MATLAB:
Once downloaded, open up the files and look at the code. Try to understand what each part of the code does, with reference to the climatesim page. To run the albedo01.m
type batch_albedo01
on the MATLAB command line.
If you really prefer not to use MATLAB a simpler version of the climate model has been written in Excel:
Once downloaded, open up the file and look sheet 1 and 2. Sheet 1 is a basic climate model with one type of clouds, whereas sheet 2 is similar but containing a fraction of clouds that have been geoengineered. Try to understand what each part of the Excel file does, with reference to the climatesim page. The idea is you change some of the variables in the file and use the results to generate plots.
Tutorial 3: carbon dioxide concentrations #1.
MATLAB users
Now type batch_albedo01a
in MATLAB and you will get two figures: one of the Global Temperature vs the Cloud albedo and CO2 mixing ratio and the other of the Radiative Forcing vs the same variables. Print out your figures, produced in MATLAB, and write down what they show. Bring the figures and your descriptions to the next tutorial for discussion
Take a look at the latest IPCC report (the bit on radiative forcing). Radiative forcing can be expressed as the amount of energy going into the earth-atmosphere-ocean system due to a specific component (e.g. CO2, or clouds).
- Find the figure on radiative forcing and determine how large the CO2 component is.
- Try to understand what your two plots are showing. How can you use the plots to estimate the radiative forcing due to CO2?
- Now uncomment lines 40 to 42 of
batch_albedo01a.m
, save, and run again.
- Look at what is being plotted on line 41. Save this new figure too and bring all three figures to the next tutorial.
- Your mark for the tutorial will be based on your completion / attempt of the tasks and contribution to the discussion. If you do not complete you will lose 16% of the marks for this part of the assessment.
Excel warriors
You should use sheet 1 to calculate the surface temperature for a range of values of CO2 mixing ratio (decide the range yourself). Plot this out. On the same graph do the same plot but for an increase in the cloud albedo. Repeat this for a few different cloud albedo values, so you have 4 line plots of surface temperature on the y-axis against CO2 mixing ratio on the x-axis and bring it to the next tutorial for discussion
Take a look at the latest IPCC report (the bit on radiative forcing). Radiative forcing can be expressed as the amount of energy going into the earth-atmosphere-ocean system due to a specific component (e.g. CO2, or clouds).
- Find the figure on radiative forcing and determine how large the CO2 component is.
- Using sheet 1 generate a similar plot to above but instead of plotting the surface temperature on the y-axis plot the energy going into the system (calculated in cell B37).
- Better still, generate a plot similar to plot in the above bulletpoint but instead of the energy going into the system plot the difference between the energy going in and the energy going in for preindustrial concentrations of CO2.
- Try to understand what these two plots are showing. How can you use the plots to estimate the radiative forcing due to CO2?
- Your mark for the tutorial will be based on your completion / attempt of the tasks and contribution to the discussion. If you do not complete you will lose 16% of the marks for this part of the assessment.
Tutorial 4: carbon dioxide concentrations #2.
We will discuss your results and what they mean as part of the tutorial.
MATLAB users
Take a look at chapter 12 of the IPCC report (the bit on long-term climate change). Find the plot of global surface warming for different emissions scenarios (zero emissions and constant emissions).
Excel warriors
Take a look at chapter 12 of the IPCC report (the bit on long-term climate change). Find the plot of global surface warming for different emissions scenarios (zero emissions and constant emissions).
Tutorial 5: methane concentrations #1.
Take a look at a recent (controversial) Nature letter on atmospheric methane here by Whiteman et al. (you may need to be on campus / use vpn to download it). In addition take a look at this communication about the Whiteman paper.
- Bring and comments to the next tutorial.
- For discussion in the tutorial: how would you use results from this paper to estimate increases in atmospheric methane due to melting permafrost? (hint: the communication on the Whiteman paper may contain the information you need).
- Your mark for the tutorial will be based on your contribution to the discussion. If you do not contribute anything you will be penalised 16% for this assessment
Tutorial 6: methane concentrations #2.
In tutorial 5 you will have discussed how to estimate the amount of methane released into the atmosphere via the idea proposed in the Nature letter.
- Use the MATLAB climate model or the Excel spreadsheet to estimate how this release may potentially affect the global temperature. The approach is similar to that in tutorial 4 where different values of CO2 were used. Whereas for this exercise you may wnat to change just the methane, or both the CO2 and the methane and plot out the results.
- Discuss any assumptions behind your calculations
- For discussion in the tutorial: bring any figures to the next tutorial. You will lose 16% of the marks for this
Tutorial 7: Clouds / geoengineering.
In the tutorial we will discuss your figures and what they mean, failure to bring the figures / contribute will result in 20% penalty for this assessment. We will also discuss the concept of the marine cloud brightening scheme of geoengineering. This MATLAB script: albedo_geo.m can be used to look at the effects of geoengineering on the global temperature, discuss how the albedo of a geoengineered planet is calculated.
Try the following:
albedo_geog=linspace(0.356,0.6,50);
co2ppm=385:5:2*385;
for i=1:length(albedo_geog)
for j=1:length(co2ppm)
tsurface(i,j)=albedo_geo(albedo_geog(i),1,co2ppm(j));
end
end
figure
pcolor(co2ppm,albedo_geog,tsurface);shading flat
You aim is to leave the tutorial with an understanding of what this means and why it has been considered as a means to mitigate rising CO2.
For the next tutorial you will prepare a PowerPoint as a group and present it in the final tutorial.