On the parallelization of atmospheric inversions of CO 2 surface fluxes within a variational framework

Abstract. The variational formulation of Bayes' theorem allows inferring CO2 sources and sinks from atmospheric concentrations at much higher time–space resolution than the ensemble or analytical approaches. However, it usually exhibits limited scalable parallelism. This limitation hinders global atmospheric inversions operated on decadal time scales and regional ones with kilometric spatial scales because of the computational cost of the underlying transport model that has to be run at each iteration of the variational minimization. Here, we introduce a physical parallelization (PP) of variational atmospheric inversions. In the PP, the inversion still manages a single physically and statistically consistent window, but the transport model is run in parallel overlapping sub-segments in order to massively reduce the computation wall-clock time of the inversion. For global inversions, a simplification of transport modelling is described to connect the output of all segments. We demonstrate the performance of the approach on a global inversion for CO2 with a 32 yr inversion window (1979–2010) with atmospheric measurements from 81 sites of the NOAA global cooperative air sampling network. In this case, we show that the duration of the inversion is reduced by a seven-fold factor (from months to days), while still processing the three decades consistently and with improved numerical stability.

[1]  J. Randerson,et al.  An atmospheric perspective on North American carbon dioxide exchange: CarbonTracker , 2007, Proceedings of the National Academy of Sciences.

[2]  P. Ciais,et al.  A European summertime CO2 biogenic flux inversion at mesoscale from continuous in situ mixing ratio measurements , 2011 .

[3]  Philippe Bousquet,et al.  Inferring CO2 sources and sinks from satellite observations: Method and application to TOVS data , 2005 .

[4]  Philippe Ciais,et al.  Towards robust regional estimates of CO2 sources and sinks using atmospheric transport models , 2002, Nature.

[5]  R. Giering,et al.  Two decades of terrestrial carbon fluxes from a carbon cycle data assimilation system (CCDAS) , 2005 .

[6]  Thomas Kaminski,et al.  On aggregation errors in atmospheric transport inversions , 2001 .

[7]  A. Denning,et al.  Carbon flux bias estimation employing Maximum Likelihood Ensemble Filter (MLEF) , 2007 .

[8]  Kevin R. Gurney,et al.  Regional trends in terrestrial carbon exchange and their seasonal signatures , 2011 .

[9]  François-Marie Bréon,et al.  Contribution of the Orbiting Carbon Observatory to the estimation of CO2 sources and sinks: Theoretical study in a variational data assimilation framework , 2007 .

[10]  S. Dance,et al.  Estimating surface CO2 fluxes from space-borne CO2 dry air mole fraction observations using an ensemble Kalman Filter , 2009 .

[11]  Marc Bocquet,et al.  Grid resolution dependence in the reconstruction of an atmospheric tracer source , 2005 .

[12]  I. C. Prentice,et al.  A dynamic global vegetation model for studies of the coupled atmosphere‐biosphere system , 2005 .

[13]  Sarah L. Dance,et al.  Estimating surface CO 2 fluxes from space-borne CO 2 dry air mole fraction observations using an ensemble Kalman Filter , 2008 .

[14]  Shamil Maksyutov,et al.  TransCom model simulations of CH4 and related species: linking transport, surface flux and chemical loss with CH4 variability in the troposphere and lower stratosphere , 2011 .

[15]  Philippe Ciais,et al.  What eddy‐covariance measurements tell us about prior land flux errors in CO2‐flux inversion schemes , 2012 .

[16]  Markus Reichstein,et al.  On the assignment of prior errors in Bayesian inversions of CO2 surface fluxes , 2006 .

[17]  J. Randerson,et al.  Global fire emissions and the contribution of deforestation, savanna, forest, agricultural, and peat fires (1997-2009) , 2010 .

[18]  Beniamino Gioli,et al.  Bridging the gap between atmospheric concentrations and local ecosystem measurements , 2009 .

[19]  Wouter Peters,et al.  An improved Kalman Smoother for atmospheric inversions , 2005 .

[20]  S. Bony,et al.  The LMDZ4 general circulation model: climate performance and sensitivity to parametrized physics with emphasis on tropical convection , 2006 .

[21]  Christoph Gerbig,et al.  A Bayesian inversion estimate of N2O emissions for western and central Europe and the assessment of aggregation errors , 2010 .

[22]  Gérald Desroziers,et al.  Accelerating and parallelizing minimizations in ensemble and deterministic variational assimilations , 2012 .

[23]  Dusanka Zupanski,et al.  An ensemble data assimilation system to estimate CO2 surface fluxes from atmospheric trace gas observations , 2005 .

[24]  Andrew J. Watson,et al.  Climatological Mean and Decadal Change in Surface Ocean Pco(2), and Net Sea-Air Co2 Flux Over the Global Oceans (Vol 56, Pg 554, 2009) , 2009 .

[25]  Fabienne Maignan,et al.  CO2 surface fluxes at grid point scale estimated from a global 21 year reanalysis of atmospheric measurements , 2010 .