4.6 Article

Biological processes dominate seasonality of remotely sensed canopy greenness in an Amazon evergreen forest

Journal

NEW PHYTOLOGIST
Volume 217, Issue 4, Pages 1507-1520

Publisher

WILEY
DOI: 10.1111/nph.14939

Keywords

canopy phenology; leaf age; leaf optics; LiDAR canopy structure; MODIS EVI; WorldView-2

Categories

Funding

  1. NASA [NNX11AH24G, NNX17AF56G]
  2. NSF (PIRE) [0730305]
  3. US DOE, Office of Science, Office of Biological and Environmental Research [DE-SC0012704]
  4. JAXA GCOM-C [111]
  5. JSPS KAKENHI [16H02948]
  6. NSF [EF1550686, EF-1340604]
  7. Australian Research Council - Discovery Project [ARC-DP140102698]
  8. Direct For Biological Sciences
  9. Division Of Environmental Biology [1340604, 1340624] Funding Source: National Science Foundation
  10. Emerging Frontiers
  11. Direct For Biological Sciences [1340649] Funding Source: National Science Foundation
  12. Office Of The Director
  13. Office Of Internatl Science &Engineering [0730305] Funding Source: National Science Foundation
  14. Grants-in-Aid for Scientific Research [16H02948] Funding Source: KAKEN
  15. NASA [NNX11AH24G, 1002206, NNX17AF56G, 144811] Funding Source: Federal RePORTER

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Satellite observations of Amazon forests show seasonal and interannual variations, but the underlying biological processes remain debated. Here we combined radiative transfer models (RTMs) with field observations of Amazon forest leaf and canopy characteristics to test three hypotheses for satellite-observed canopy reflectance seasonality: seasonal changes in leaf area index, in canopy-surface leafless crown fraction and/or in leaf demography. Canopy RTMs (PROSAIL and FLiES), driven by these three factors combined, simulated satellite-observed seasonal patterns well, explaining c. 70% of the variability in a key reflectance-based vegetation index (MAIAC EVI, which removes artifacts that would otherwise arise from clouds/aerosols and sun-sensor geometry). Leaf area index, leafless crown fraction and leaf demography independently accounted for 1, 33 and 66% of FLiES-simulated EVI seasonality, respectively. These factors also strongly influenced modeled near-infrared (NIR) reflectance, explaining why both modeled and observed EVI, which is especially sensitive to NIR, captures canopy seasonal dynamics well. Our improved analysis of canopy-scale biophysics rules out satellite artifacts as significant causes of satellite-observed seasonal patterns at this site, implying that aggregated phenology explains the larger scale remotely observed patterns. This work significantly reconciles current controversies about satellite-detected Amazon phenology, and improves our use of satellite observations to study climate-phenology relationships in the tropics.

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