Weak Simulated Extratropical Responses to Complete Tropical Deforestation
- 15 June 2006
- journal article
- Published by American Meteorological Society in Journal of Climate
- Vol. 19 (12) , 2835-2850
- https://doi.org/10.1175/jcli3737.1
Abstract
The Geophysical Fluid Dynamics Laboratory atmosphere–land model version 2 (AM2/LM2) coupled to a 50-m-thick slab ocean model has been used to investigate remote responses to tropical deforestation. Magnitudes and significance of differences between a control run and a deforested run are assessed through comparisons of 50-yr time series, accounting for autocorrelation and field significance. Complete conversion of the broadleaf evergreen forests of South America, central Africa, and the islands of Oceania to grasslands leads to highly significant local responses. In addition, a broad but mild warming is seen throughout the tropical troposphere (<0.2°C between 700 and 150 mb), significant in northern spring and summer. However, the simulation results show very little statistically significant response beyond the Tropics. There are no significant differences in any hydroclimatic variables (e.g., precipitation, soil moisture, evaporation) in either the northern or the southern extratropics. Small but... Abstract The Geophysical Fluid Dynamics Laboratory atmosphere–land model version 2 (AM2/LM2) coupled to a 50-m-thick slab ocean model has been used to investigate remote responses to tropical deforestation. Magnitudes and significance of differences between a control run and a deforested run are assessed through comparisons of 50-yr time series, accounting for autocorrelation and field significance. Complete conversion of the broadleaf evergreen forests of South America, central Africa, and the islands of Oceania to grasslands leads to highly significant local responses. In addition, a broad but mild warming is seen throughout the tropical troposphere (<0.2°C between 700 and 150 mb), significant in northern spring and summer. However, the simulation results show very little statistically significant response beyond the Tropics. There are no significant differences in any hydroclimatic variables (e.g., precipitation, soil moisture, evaporation) in either the northern or the southern extratropics. Small but...Keywords
This publication has 32 references indexed in Scilit:
- The underpinnings of land‐use history: three centuries of global gridded land‐use transitions, wood‐harvest activity, and resulting secondary landsGlobal Change Biology, 2006
- Simulated Response of the Atmosphere‐Ocean System to deforestation in the Indonesian ArchipelagoGeophysical Research Letters, 2001
- Biogeophysical versus biogeochemical feedbacks of large‐scale land cover changeGeophysical Research Letters, 2001
- Biogeophysical Consequences of a Tropical Deforestation Scenario: A GCM Simulation StudyJournal of Climate, 1996
- Global climate sensitivity to tropical deforestationGlobal and Planetary Change, 1995
- Estimates of Spatial Degrees of FreedomJournal of Climate, 1995
- The impact of African and Amazonian deforestation on tropical climateJournal of Hydrology, 1994
- Amazon Deforestation and Climate ChangeScience, 1990
- Simulation of the regional climatic impact of Amazon deforestationNature, 1989
- Modelling tropical deforestation: A study of GCM land‐surface parametrizationsQuarterly Journal of the Royal Meteorological Society, 1988