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Department of Hydrology and Water Resources

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1 Department of Hydrology and Water Resources
Assessing the limiting factors of CO2 exchange in the Amazon rainforest during the dry season using the Simple Biosphere Model 3 Rafael Rosolem Department of Hydrology and Water Resources May 6th, 2008

2 Motivation Saleska et al (Science) Myneni et al (PNAS)

3 Motivation Nemani et al (Science)

4 Hypothesis How to solve this issue?
- No water stress is observed during the dry season because deep roots can still extract water from the soil; Dry season = less cloud development; as a result more incoming solar energy to the vegetation which enhances photosynthesis. How to solve this issue? Vegetation phenology Soil-water dynamics Available water depth Stockli et al. (in preparation)

5 Objective Identify the mechanisms associated with the dry season “green-up” of the Amazon rainforest using a widely known land surface parameterization scheme; - Understand the soil-water dynamics component of the model;

6 Site location Located at FLONA (“Floresta Nacional”) Tapajós (lat/lon S / W); Vegetation: tropical humid forest on a broad flat plateau; The soil is mainly clay with some patches of sandy soil

7 Simple Biosphere 3 (SiB3) – Colorado State University
New Features: - Prognostic T, e, CO2, other tracers in “canopy air space”; - 10-layer soil (T and w), with adjustable water extraction profile (roots); - Snowpack of 0-5 layers; - Mixed canopy physiology (e.g., savanna); and - Stable isotope fractionation of CO2. Adapted from Dr. Denning slides

8 Model configuration Forcing data: Temp. (oC), q (g kg-1), U (m s-1), Press. (hPa), Sdown (W m-2), Ldown (W m-2), and Prec. (mm hr-1): 1 hr timestep available from Jan/2001- Dec/2003; Highly parameterized scheme (36 parameters + 8 time-varying inputs); Soil and veg. type dependent parameters: SiB2 look-up tables applied to UMD vegetation and FAO soil maps; biophysical parameters and time-varying inputs: global version of the European Fourier-Adjusted and Interpolated NDVI (EFAI-NDVI): 20 year long NASA/NOAA AVHRR Pathfinder NDVI data (10-day temporal and 0.1 degree spatial resolution) at No model calibration and validation experiments: LARGE SOURCE OF UNCERTAINTY!!! 30-yr spin-up has been applied to stabilized soil moisture and carbon quantities in the model;

9 Simulation experiments
Control Saturation Saturation - Control

10 Results: Monthly sat con

11 Results: Diurnal – Dry season
con

12 Results: Diurnal and seasonal variation of NEE

13 Results: Cumulative NEE
con sat - con

14 Conclusions Control experiment fails to simulate the energy partion (H and LE); Simulation is clearly improved in the dry season when water is available at the bottom layers: energy partition is improved!!! Saturation experiment: available energy becomes the only limiting factor in the Amazon rainforest (consistent with past studies); Model calibration MUST be performed (e.g, diurnal pattern of gorund heat flux); At the end of the 3 years, the saturation simulation uptakes approximately 30% more carbon (0.25 g m-2 s-1) than the control experiment; IMPORTANT: This study is just a QUICK FIX to the issue of Amazon “green- up”; the best approach is actually to incorporate a powerful phenology prognostic model and develop a rooting dynamics formulation to account for water extraction under stress conditions;


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