Surface Energy Dynamics and Canopy Structural Properties in Intact and Disturbed Forests in the Southern Amazon

Author:

Rangel Pinagé Ekena12ORCID,Bell David M.3,Longo Marcos45ORCID,Silva Carlos A.6,Csillik Ovidiu4ORCID,Huete Alfredo1ORCID

Affiliation:

1. School of Life Sciences University of Technology Sydney Ultimo NSW Australia

2. College of Forestry Oregon State University Corvallis OR USA

3. Pacific Northwest Research Station USDA Forest Service Corvallis OR USA

4. Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA

5. Climate and Ecosystem Sciences Division Lawrence Berkeley National Laboratory Berkeley CA USA

6. Forest Biometrics, Remote Sensing and Artificial Intelligence Laboratory School of Forest, Fisheries and Geomatics Sciences University of Florida Gainesville FL USA

Abstract

AbstractThe Brazilian Amazon has been a focus of land development with large swaths of forests converted to agriculture. Forest degradation by selective logging and fires has accompanied the agricultural frontier and has resulted in significant impacts on Amazonian ecosystems. Changes in forest structure resulting from forest disturbances have large impacts on the surface energy balance, including on land surface temperature (LST) and evapotranspiration (ET). This study's objective is to assess the effects of forest disturbances on water fluxes and forest structure in a transitional forest site in the Southern Amazon. We used ET and LST products from MODIS and Landsat 8 and GEDI‐derived forest structure data to address our research questions. We found that disturbances induced seasonal water stress, more pronounced in croplands/pastures than in forests (differences up to 20% in the dry season), and more pronounced in second‐growth and recently burned areas than in logged and intact forests (differences up to 12% in the dry season). Moreover, ET and LST were negatively related, with more consistent relationships across disturbance classes in the dry season (R2: 0.41–0.87) than in the wet season (R2: 0.18–0.49). Forest and cropland or pasture classes showed contrasting relationships in the dry season. Finally, we found that forest structure exhibited stronger relationships with ET and LST in the most disturbed forests (R2: 0.01–0.43) than in the least disturbed forests (R2 < 0.05). Our findings help to elucidate degraded forests functioning under a changing climate and to improve estimates of water and energy fluxes in Amazonian degraded forests.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

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