B13C-0190:
Reducing Uncertainty in Terrestrial Biosphere Models with Satellite Observations of Atmospheric CO2: Comparing MsTMIP with GOSAT
Monday, 15 December 2014
Jessica B Swetish1, Deborah N Huntzinger1, Christopher R Schwalm1, Joshua B Fisher2, Junjie Liu3, Anna M Michalak4 and Kevin W Bowman3, (1)Northern Arizona University, Flagstaff, AZ, United States, (2)NASA Jet Propulsion Laboratory, Pasadena, CA, United States, (3)Jet Propulsion Laboratory, Pasadena, CA, United States, (4)Carnegie Institution for Science, Washington, DC, United States
Abstract:
Global-scale terrestrial biosphere models (TBMs) vary in their underlying driving assumptions, inputs, and parameterizations. As a result, TBM estimates of carbon fluxes and pools vary greatly and the lack of direct observations of land-atmosphere carbon exchange at the same spatio-temporal resolution (e.g., 0.5° x 0.5° degree and sub-daily to monthly) of model estimates makes it difficult to assess TBM performance in terms of their ability to represent the terrestrial carbon cycle. Atmospheric CO2 measurements, however, may be a potentially powerful observational constraint for TBMs because they provide an integrated view of surface sources and sinks of carbon. The Greenhouse Gases Observing Satellite (GOSAT) measures atmospheric CO2 from space at spatio-temporal scales relatively consistent with model estimates. Using TBM estimates from the North American Carbon Program Multi-scale synthesis and Terrestrial Model Intercomparison Project (MsTMIP), together with estimates of fossil fuel emissions and air-sea fluxes, we translate surfaces fluxes into atmospheric CO2 concentrations using the GEOS-Chem atmospheric transport model. The performance of MsTMIP TBMs is evaluated by comparing the dry air column-averaged mole fractions of CO2 (ΧCO2) from transported surface fluxes to observations of ΧCO2 from GOSAT. While MsTMIP ΧCO2 signals are generally consistent with GOSAT ΧCO2 in the southern hemisphere, MsTMIP and GOSAT XCO2 show profound differences in the northern hemisphere (NH). In general, MsTMIP XCO2 tends to be higher than GOSAT XCO2 at northern latitudes, especially in the NH summer and fall. Looking specifically at regions in the NH, we compare each MsTMIP ΧCO2 to GOSAT ΧCO2 in terms of its ability to reproduce the spatial distribution, magnitude and timing of the GOSAT ΧCO2 seasonal cycle. We use the information derived from the comparison to link model performance with how certain processes are represented within the models themselves, thus aiding in model development and improvement.