BWI Climate Data Analysis with MatLab
SO503 Spring 2013
(2/26/2013)
We will investigate the PGO (Professor Guth Oscillation), which proposes that severe snowfall occurs at BWI every year Professor Guth has a sabbatical (AY 95-96, 02-03, and 09-10). These are the years with the greatest snowfall on record.
This will be due at 1330 on Tues 5 March 2013.
There is an m file to get you started. The main learning point of this lab is to create a double loop, which this sample does, and deal with nasty climate data in matrix format.
Modified BWI temperature file for easy import to Matlab. This came from http://www.erh.noaa.gov/lwx/climate/bwi/bwitemps.txt. The website has the average monthly temperatures at the bottom of the table; you can either get them from the web, or compute them in Matlab or Excel.
The sample program uses a double loop to create time and temperature vectors. If you are feel adventurous, you could import this data as a matrix instead of vectors, and shorten the program substantially.
Much of the buzz about our weather has blamed El Nino. You can get the SOI (Southern Oscillation Index) at:
http://www.bom.gov.au/climate/glossary/soi.shtml, specifically ftp://ftp.bom.gov.au/anon/home/ncc/www/sco/soi/soiplaintext.html
Another source for this data is http://www.cgd.ucar.edu/cas/catalog/climind/soi.html but it is less up to date than then Ozzies.
Get the data, clean it up if required, and import it into Matlab. Call it the SOI.
To compare the BWI data with the SOI, we want to compute the monthly deviation in temperature (the anomaly) from average temperature for that month. Positive values will be higher than normal, and negative values lower. We will call this the BWI temperature anomaly. Note that http://www.erh.noaa.gov/lwx/climate/bwi/bwitemps.txt has monthly averages.
There is an NAO, Northern Oscillation Index, that might be more relevant to our snow
http://www.cpc.noaa.gov/products/precip/CWlink/pna/nao_index.html Note that at the bottom of the page there are two different formats for this data. Get whichever you think is easier.
http://www.ldeo.columbia.edu/res/pi/NAO/ discusses the NAO and how it relates to US climate.
Adjust the SOI and BWI temperature anomaly so they have the same length (they are much longer than the NAO). This will be your long time series.
Adjust all the time series so they start at the same time, and end at the same time. These will be your short time series.
Perform cross correlations for (insure that you get the symbol for squared, and not the ^2 or "squared" in your discussion). Get both the maximum and minimum r values, and the lags were each occurs.
SOI and NAO.
SOI can BWI temperature anomaly, in both the long and short series.
NAO and BWI temperature anomaly.
Requirements:
Create graphs with the following, in a format that they can be quickly compared to see if there are any relationships:
Temperature anomaly by month at BWI
SIO by month
NAO by month
Discuss what these show, including the results of your cross correlations.
Discuss whether the temperature variability is better shown as the temperature readings below, or as the anomaly.
Hints:
You are likely to encounter two types of errors:
| This shows the results from the time and temp arrays. While the graph looks fine (see below), there is actually a subtle error here in the time column. Look carefully at rows 4 and 5, or 16 and 17. You now have to go back to your code, and see what you did wrong. |
