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Title: Do dynamic global vegetation models capture the seasonality of carbon fluxes in the Amazon basin? A data-model intercomparison

Journal Article · · Global Change Biology
DOI:https://doi.org/10.1111/gcb.13442· OSTI ID:1341704
ORCiD logo [1]; ORCiD logo [2];  [3];  [4];  [5];  [6];  [7];  [6];  [8];  [9];  [10];  [11];  [12];  [4]
  1. Univ. of Technology Sydney, Sydney, NSW (Australia). Plant Functional Biology and Climate Change Cluster; Univ. of Arizona, Tucson, AZ (United States). Dept. of Ecology and Evolutionary Biology
  2. Univ. of Southern California, Los Angeles, CA (United States). Dept. of Biological Sciences; Harvard Univ., Cambridge, MA (United States). Dept. of Organismic and Evolutionary Biology
  3. Univ. of Arizona, Tucson, AZ (United States). Dept. of Ecology and Evolutionary Biology; Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Univ. of Arizona, Tucson, AZ (United States). Dept. of Atmospheric Sciences
  4. Univ. of Arizona, Tucson, AZ (United States). Dept. of Ecology and Evolutionary Biology
  5. Univ. of Arizona, Tucson, AZ (United States). Dept. of Ecology and Evolutionary Biology; Brookhaven National Lab, Upton, NY (United States). Biological, Environmental & Climate Sciences Dept.
  6. Federal Univ. of Vicosa, Vicosa (Brazil). Dept. of Agricultural Engineering
  7. Univ. of Leeds, Leeds (United Kingdom). School of Geography
  8. Inst. Nacional de Pesquisas da Amazonia (INPA), Manaus (Brazil)
  9. Inst. Nacional de Pesquisas da Amazonia (INPA), Manaus (Braz; Embrapa Amazonia Oriental, Belem (Brazil)
  10. Univ. of Oxford (United Kingdom). Environmental Change Inst.
  11. Univ. of Arizona, Tucson, AZ (United States). Dept. of of Atmospheric Sciences
  12. Harvard Univ., Cambridge, MA (United States). Dept. of Organismic and Evolutionary Biology

To predict forest response to long-term climate change with high confidence requires that dynamic global vegetation models (DGVMs) be successfully tested against ecosystem response to short-term variations in environmental drivers, including regular seasonal patterns. Here, we used an integrated dataset from four forests in the Brasil flux network, spanning a range of dry-season intensities and lengths, to determine how well four state-of-the-art models (IBIS, ED2, JULES, and CLM3.5) simulated the seasonality of carbon exchanges in Amazonian tropical forests. We found that most DGVMs poorly represented the annual cycle of gross primary productivity (GPP), of photosynthetic capacity (Pc), and of other fluxes and pools. Models simulated consistent dry-season declines in GPP in the equatorial Amazon (Manaus K34, Santarem K67, and Caxiuanã CAX); a contrast to observed GPP increases. Model simulated dry-season GPP reductions were driven by an external environmental factor, ‘soil water stress’ and consequently by a constant or decreasing photosynthetic infrastructure (Pc), while observed dry-season GPP resulted from a combination of internal biological (leaf-flush and abscission and increased Pc) and environmental (incoming radiation) causes. Moreover, we found models generally overestimated observed seasonal net ecosystem exchange (NEE) and respiration (Re) at equatorial locations. In contrast, a southern Amazon forest (Jarú RJA) exhibited dry-season declines in GPP and Re consistent with most DGVMs simulations. While water limitation was represented in models and the primary driver of seasonal photosynthesis in southern Amazonia, changes in internal biophysical processes, light-harvesting adaptations (e.g., variations in leaf area index (LAI) and increasing leaf-level assimilation rate related to leaf demography), and allocation lags between leaf and wood, dominated equatorial Amazon carbon flux dynamics and were deficient or absent from current model formulations. In conclusion, correctly simulating flux seasonality at tropical forests requires a greater understanding and the incorporation of internal biophysical mechanisms in future model developments.

Research Organization:
Brookhaven National Laboratory (BNL), Upton, NY (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
SC00112704
OSTI ID:
1341704
Report Number(s):
BNL-113452-2017-JA; R&D Project: 21087; YN0100000
Journal Information:
Global Change Biology, Vol. 23, Issue 1; ISSN 1354-1013
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 97 works
Citation information provided by
Web of Science

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Drought, Heat, and the Carbon Cycle: a Review journal June 2018
Dry-Season Greening and Water Stress in Amazonia: The Role of Modeling Leaf Phenology journal June 2018
Large‐Scale Droughts Responsible for Dramatic Reductions of Terrestrial Net Carbon Uptake Over North America in 2011 and 2012 journal July 2018
Surface‐Atmosphere Coupling Scale, the Fate of Water, and Ecophysiological Function in a Brazilian Forest journal August 2019
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Current and future patterns of fire-induced forest degradation in Amazonia journal September 2017
Regional contribution to variability and trends of global gross primary productivity journal September 2017
Higher absorbed solar radiation partly offset the negative effects of water stress on the photosynthesis of Amazon forests during the 2015 drought journal March 2018
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Widespread reduction in sun-induced fluorescence from the Amazon during the 2015/2016 El Niño
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journal October 2018
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The biophysics, ecology, and biogeochemistry of functionally diverse, vertically and horizontally heterogeneous ecosystems: the Ecosystem Demography model, version 2.2 – Part 2: Model evaluation for tropical South America journal January 2019
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Upside-down fluxes Down Under: CO 2 net sink in winter and net source in summer in a temperate evergreen broadleaf forest journal January 2018
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