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If you want a measure of exposure, i. e., heat, I suggest using the 
"heatload" transformation suggested by McCune and Grace (2002). Their 
assumption is that mid-afternoon, when the sun is in the southwest, is 
usually the warmest time of day. The formula at the end of Chapter 3 
follows:

heat load index=(1-cos(degrees-45))/2

McCune, Bruce and James B. Grace. 2002. Analysis of ecological 
communities. MJM Software Design. Gleneden Beach, Oregon. USA

Mike Marsh
On 10/16/2013 3:00 AM, r-sig-ecology-request at r-project.org wrote: