| [Thread Prev] | [Thread Next] | [Thread Index] | [Date Prev] | [Date Next] | [Date Index] |
I used a modification of Berger's 1978 Fortran program for calculating insolation. This program gives the top-of-atmosphere insolation for any date/year and latitude. I then ran the program to give the insolation at 60N at the summer solstice, at 100K intervals, for the last 300 my. The resulting plot showed clear cycles on the order of 25my. Needless to say , this was exciting! But when when I reran it starting 50k ago, the pattern was much more obscure. I then tried it at a 2k interval (lots of data points!), at different latitudes, at different seasons, looked at summer-winter contrast, rates of change, etc. etc. You could kind of see a pattern, but it was unclear. The clearest pattern I get is a ca. 50 my cycle in the variance. A big caveat: the current cycles are not stationary! I was mostly interested in the idea of interference patterns, rather thatn in precise dates. The big surprise to me was the scale of insolation variations during the cycle, especially at eccentricity and obliquity maximums. On the order of 15-20% at higher latitudes! This has to have a effect on ecosystems, even ignoring the climatic effects. - Roy -- Roy E. Plotnick Geological Sciences University of Illinois at Chicago 845 W. Taylor St. Chicago, IL 60607 plotnick@plotnick.geol.uic.edu phone: 312-996-2111 fax: 312-413-2279
Partial index: