On the seasonal effect of orbital variations on the climates of the next 4000 years
A northern hemisphere thermodynamic climate model is used to compute the effect of the insolation anomalies due to orbital variations in the climates for the next 4000 years. Berger's mean monthly anomalies of insolation are used in the computations, which are carried out for 1000, 2000, 30...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
1996-11-01
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| Series: | Annales Geophysicae |
| Online Access: | https://www.ann-geophys.net/14/1198/1996/angeo-14-1198-1996.pdf |