Role of vegetation and soil in the Holocene megathermal climate over China
- 27 April 1999
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 104 (D8) , 9361-9367
- https://doi.org/10.1029/1999jd900049
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- On multiple solutions of the atmosphere–vegetation system in present‐day climateGlobal Change Biology, 1998
- A fully coupled GCM simulation of the climate of the mid‐HoloceneGeophysical Research Letters, 1998
- Modelling global terrestrial vegetation–climate interactionPhilosophical Transactions Of The Royal Society B-Biological Sciences, 1998
- Response of the African Monsoon to Orbital Forcing and Ocean Feedbacks in the Middle HoloceneScience, 1997
- The Greening of the Sahara during the Mid-Holocene: Results of an Interactive Atmosphere-Biome ModelGlobal Ecology and Biogeography Letters, 1997
- Vegetation and soil feedbacks on the response of the African monsoon to orbital forcing in the early to middle HoloceneNature, 1996
- Possible role of atmosphere‐biosphere interactions in triggering the Last GlaciationGeophysical Research Letters, 1996
- Feedbacks between climate and boreal forests during the Holocene epochNature, 1994
- On coupling global biome models with climate modelsClimate Research, 1994
- Continental vegetation as a dynamic component of a global climate model: a preliminary assessmentClimatic Change, 1993