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| Titel |
On the seasonal effect of orbital variations on the climates of the next 4000 years |
| VerfasserIn |
Julián Adem |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
0992-7689
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| Digitales Dokument |
URL |
| Erschienen |
In: Annales Geophysicae ; 14, no. 11 ; Nr. 14, no. 11, S.1198-1206 |
| Datensatznummer |
250012472
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| Publikation (Nr.) |
 copernicus.org/angeo-14-1198-1996.pdf |
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| Zusammenfassung |
| 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, 3000 and 4000 years after present (kyears AP). The numerical
simulations show that in the climates of the next 4000 years, due to the effect
of the orbital variations, springs and summers will be increasingly dryer and
falls and winters wetter than the present climate. |
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