The climate of ten thousand years ago: a numerical simulation
Para simular el clima de hace 10 000 años se aplica un modelo termodinámico que incluye el ciclo anual, una capa oceánica mezclada y una capa de hielo y nieve variable.Se demuestra que en latitudes bajas las anomalías de insolación debidas a las variaciones orbitales fueron el factor principal que p...
Main Author: | J. Adem |
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Format: | Article |
Language: | English |
Published: |
Universidad Nacional Autónoma de México, Instituto de Geofísica
1985-07-01
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Series: | Geofísica Internacional |
Subjects: | |
Online Access: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1024 |
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