Land use and local climate: A case study near Santa Cruz, Bolivia

SummaryThe Tierras Bajas regions of eastern Santa Cruz, Bolivia have undergone among the most rapid rates of concentrated deforestation during the 1980s and 1990s. We investigate the sensitivity of local climate to these land cover changes as observed from Landsat images acquired between 1975 and 1999. The Simple Biosphere model (SiB2) is used to assess the effects of both morphological and physiological changes in vegetation and the implications for fluxes of water, energy and carbon between the vegetation and the atmosphere during the rainy season.Conversion from tropical forest to cropland implicates morphological changes in vegetation as the primary drivers for a daily maximum warming of about 2 °C and a slight nighttime cooling, suggesting that clearing of tropical forests for agricultural use may increase the diurnal temperature range, mainly by increasing the maximum temperature. On the other hand, the conversion of wooded grassland to cropland resulted in a similar daily warming and drying but exclusively due to vegetation physiological activity.The area-averaged monthly mean response for each conversion type resulted in a warming of about 0.6 °C for the conversion of broadleaf evergreen and 1.2 °C for conversion of wooded grassland. These temperature differences represent an augmentation in the local heat source associated with a reduction in evapotranspiration due to land cover conversion and do not reflect variations forced by changes in atmospheric circulation.When averaged over the entire domain, the effect of landscape conversion results in a reduction of the latent heat flux and an increase in sensible heat flux, producing a large-scale apparent heat source of 0.5 °C during January. This warming is in line with an increasing trend observed in monthly mean temperature in Santa Cruz, Bolivia during the same period.

[1]  S. Running,et al.  Simulated impacts of historical land cover changes on global climate in northern winter , 2000 .

[2]  C. Tucker,et al.  Clearance and Fragmentation of Tropical Deciduous Forest in the Tierras Bajas, Santa Cruz, Bolivia , 2001 .

[3]  P. Sellers Canopy reflectance, photosynthesis, and transpiration. II. the role of biophysics in the linearity of their interdependence , 1987 .

[4]  Ann Henderson-Sellers,et al.  Global climate sensitivity to tropical deforestation , 1995 .

[5]  C. Justice,et al.  A revised land surface parameterization (SiB2) for GCMs. Part III: The greening of the Colorado State University general circulation model , 1996 .

[6]  Thomas C. Peterson,et al.  Maximum and Minimum Temperature Trends for the Globe , 1997 .

[7]  G. Hornberger,et al.  Empirical equations for some soil hydraulic properties , 1978 .

[8]  R. DeFries,et al.  Human modification of the landscape and surface climate in the next fifty years , 2002 .

[9]  Ann Henderson-Sellers,et al.  Tropical deforestation: Modeling local‐ to regional‐scale climate change , 1993 .

[10]  R. DeFries,et al.  Effects of Land Cover Conversion on Surface Climate , 2002 .

[11]  A. Scott Denning,et al.  Simulations of terrestrial carbon metabolism and atmospheric CO2 in a general circulation model: Part 1: Surface carbon fluxes , 1996 .

[12]  K. Fraedrich,et al.  A Green Planet Versus a Desert World: Estimating the Maximum Effect of Vegetation on the Land Surface Climate , 2000 .

[13]  L. Stefanova Sensitivity of seasonal forecast to the parameterization of land surface processes , 2001 .

[14]  Compton J. Tucker,et al.  Sensitivity of Climate to Changes in NDVI , 2000 .

[15]  Mei Zhao,et al.  The impact of land cover change on the atmospheric circulation , 2001 .

[16]  D. Randall,et al.  A Revised Land Surface Parameterization (SiB2) for Atmospheric GCMS. Part I: Model Formulation , 1996 .

[17]  J. Townshend,et al.  Global land cover classi(cid:142) cation at 1 km spatial resolution using a classi(cid:142) cation tree approach , 2004 .

[18]  Roger A. Pielke,et al.  Interactions between the atmosphere and terrestrial ecosystems: influence on weather and climate , 1998 .

[19]  J. Shukla,et al.  Amazon Deforestation and Climate Change , 1990, Science.

[20]  Piers J. Sellers,et al.  Amazonian Deforestation and Regional Climate Change , 1991 .

[21]  C. Tucker,et al.  Interactions between vegetation and climate: radiative and physiological effects of doubled atmospheric co2 , 1999 .

[22]  Kevin P. Gallo,et al.  A new perspective on recent global warming: asymmetric trends of daily maximum and minimum temperature , 1993 .

[23]  Gordon B. Bonan,et al.  Effects of Land Use on the Climate of the United States , 1997 .

[24]  A. Pitman,et al.  The relative impact of observed change in land cover and carbon dioxide as simulated by a climate model , 2000 .

[25]  Compton J. Tucker,et al.  Tropical deforestation in the Bolivian Amazon , 2000, SPIE Defense + Commercial Sensing.

[26]  J. Foley,et al.  Combined Effects of Deforestation and Doubled Atmospheric CO2 Concentrations on the Climate of Amazonia , 2000 .

[27]  D. Randall,et al.  Simulations of terrestrial carbon metabolism and atmospheric CO2 in a general circulation model: Part 2: Simulated CO2 concentrations , 1996 .

[28]  Susan E. Lee,et al.  Contrasting physiological and structural vegetation feedbacks in climate change simulations , 1997, Nature.

[29]  A. Pitman,et al.  The regional scale impact of land cover change simulated with a climate model , 2002 .