Role of orbitally induced changes in tundra area in the onset of glaciation
- 1 June 1996
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 381 (6582), 503-505
- https://doi.org/10.1038/381503a0
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Sensitivity Studies of Northern Hemisphere Glaciation Using an Atmospheric General Circulation ModelJournal of Climate, 1995
- Snow cover and sea ice sensitivity to generic changes in Earth orbital parametersJournal of Geophysical Research: Atmospheres, 1995
- The Response to Orbital Perturbations in an Atmospheric Model Coupled to a Slab OceanJournal of Climate, 1994
- On the structure and origin of major glaciation cycles 2. The 100,000‐year cyclePaleoceanography and Paleoclimatology, 1993
- Modelling of palaeoclimates: examples from the recent pastPhilosophical Transactions Of The Royal Society B-Biological Sciences, 1993
- On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch ForcingPaleoceanography and Paleoclimatology, 1992
- Can Milankovitch orbital variations initiate the growth of ice sheets in a general circulation model?Journal of Geophysical Research: Atmospheres, 1989
- A Sensitivity Experiment to Astronomical Forcing with a Spectral GCM: Simulation of the Annual Cycle at 125 000 BP and 115 000 BPPublished by Springer Nature ,1984
- Modeling the Climatic Response to Orbital VariationsScience, 1980
- Variations in the Earth's Orbit: Pacemaker of the Ice AgesScience, 1976