Effects of land-cover changes on the partitioning of surface energy and water fluxes in Amazonia using high-resolution satellite imagery

被引:21
|
作者
de Oliveira, Gabriel [1 ]
Brunsell, Nathaniel A. [1 ]
Moraes, Elisabete C. [2 ]
Shimabukuro, Yosio E. [2 ]
dos Santo, Thiago, V [3 ]
von Randow, Celso [4 ]
de Aguiar, Renata G. [5 ]
Aragao, Luiz E. O. C. [2 ,6 ]
机构
[1] Univ Kansas, Dept Geog & Atmospher Sci, 1475 Jayhawk Blvd, Lawrence, KS 66045 USA
[2] Brazilian Natl Inst Space Res, Remote Sensing Div, 1758 Astronautas Ave, BR-12227010 Sao Jose Dos Campos, SP, Brazil
[3] Univ Michigan, Dept Climate & Space Sci & Engn, 2455 Howard St, Ann Arbor, MI 48109 USA
[4] Natl Inst Space Resarch, Earth Syst Sci Ctr, Sao Jose Dos Campos, SP, Brazil
[5] Fed Univ Rondonia, Dept Environm Engn, BR-76900726 Ji Parana, RO, Brazil
[6] Univ Exeter, Coll Life & Environm Sci, Rennes Dr, Exeter EX4 4RJ, Devon, England
关键词
Amazonia; ASTER images; evapotranspiration; land-cover changes; spatial variation; SPACEBORNE THERMAL EMISSION; REFLECTION RADIOMETER ASTER; LATENT-HEAT FLUXES; BALANCE ALGORITHM; SEBAL MODEL; EVAPOTRANSPIRATION ESTIMATION; SECONDARY VEGETATION; RADIATION BALANCE; EDDY COVARIANCE; TROPICAL FOREST;
D O I
10.1002/eco.2126
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Spatial variability of surface energy and water fluxes at local scales is strongly controlled by soil and micrometeorological conditions. Thus, the accurate estimation of these fluxes from space at high spatial resolution has the potential to improve prediction of the impact of land-use changes on the local environment. In this study, Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) and Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) data were used to examine the partitioning of surface energy and water fluxes over different land-cover types in one wet year (2004) and one drought year (2005) in eastern Rondonia state, Brazil. The spatial variation of albedo, net radiation (Rn), soil (G) and sensible (H) heat fluxes, evapotranspiration (ET), and evaporative fraction (EF) were primarily related to the lower presence of forest (primary [PF] or secondary [SF]) in the western side of the Ji-Parana River in comparison with the eastern side, located within the Jaru Biological Reserve protected area. Water limitation in this part of Amazonia tends to affect anthropic (pasture [PA] and agriculture [AG]) ecosystems more than the natural land covers (PF and SF). We found statistically significant differences on the surface fluxes prior to and similar to 1 year after the deforestation. Rn over forested areas is similar to 10% greater in comparison with PA and AG. Deforestation and consequent transition to PA or AG increased the total energy (similar to 200-400%) used to heat the soil subsurface and raise air temperatures. These differences in energy partitioning contributed to approximately three times higher ET over forested areas in comparison with nonforested areas. The conversion of PF to AG is likely to have a higher impact in the local climate in this part of Amazonia when compared with the change to PA and SF, respectively. These results illustrate the importance of conserving secondary forest areas in Amazonia.
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页数:18
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