Abstract
The earth's orbital parameters, precession, obliquity and eccentricity, produce solar radiation differences (compared to present) of ca.7% at the solstices 9000 years before present (B.P.) : more radiation in June-July-August, less in December-January-February. When this amplified seasonal cycle of solar radiation is used to drive a low-resolution general circulation model, an intensified monsoon circulation is simulated for Northern Hemisphere summer. Certain features of the simulated monsoon climate from this orbital-parameter sensitivity experiment agree with the paleoclimatic evidence. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1177-1188 |
| Number of pages | 12 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 39 |
| Issue number | 6 |
| DOIs | |
| State | Published - 1982 |
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