Detecting regional variability in sources and sinks of carbon dioxide: A synthesis

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Abstract

The current paper reviews the experimental setup of the CarboEurope Experimental Strategy (CERES) campaigns with the aim of providing an overview of the instrumentation used, the data-set and associated modelling. It then assesses progress in the field of regional observation and modelling of carbon fluxes, bringing the papers of this special issue into a somewhat broader context of analysis. Instrumental progress has been obtained in the field of remotely monitoring from tall towers and the experimental planning. Flux measurements from aircraft are now capable, within some constraints, to provide regular regional observations of fluxes of CO2, latent and sensible heat. Considerable effort still needs to be put into calibrating the surface schemes of models, as they have direct impact on the input of energy, moisture and carbon fluxes in the boundary layer. Overall, the mesoscale models appear to be capable of simulating the large scale dynamics of the region, but in the fine detail, like the precise horizontal and vertical CO2 field differences between the models still exist. These errors translate directly into transport uncertainty, when the forward simulations are used in inverse mode. Quantification of this uncertainty, including that of inadequate boundary layer height modelling, still remains a major challenge for state of the art mesoscale models. Progress in inverse models has been slow, but has shown that it is possible to estimate some of the errors involved, and that using the combination of observations. Overall, the capability to produce regional, high-resolution estimates of carbon exchange, exist in potential, but the routine application will require considerable effort, both in the experimental as in the modelling domain. © Author(s) 2009.

Figures

  • Fig. 1. Map of surface vegetation cover over the CERES domain with experimental network (grey squares are flux stations).
  • Table 1. Observations made during the three CERES campaign.
  • Fig. 2. Mean CO2 concentration measured at the Biscarosse tower (blue) and at the Bellegarde-Sainte-Marie tower at different height (green and black), during the April (above) and September (below) 2007 campaigns (data provided by LSCE).
  • Fig. 3. Dimona aircraft trajectory (left) on 19 April 2007 over the croplands, the Landes forest and the ocean, and the vertical cross section of the CO2 concentration measured as the function of the distance flown by the aircraft (right).
  • Fig. 4. Sky Arrow Ibimet measurement of sensible heat flux (a), latent heat flux (b) and CO2 flux (c) (data provided by IBIMET, Beniamino Gioli).
  • Fig. 5. CO2 distribution and wind vectors on the vertical plane along 44◦25′ N, 00◦34′ W for the 27 May case, at (a) 0000, (b) 0600, (c) 1000, and (d) 1400, (from Ahmadov et al., 2007).
  • Figure 6. Schematic diagram showing the variables and process involved in determining the regional carbon balance

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CITATION STYLE

APA

Dolman, A. J., Gerbig, C., Noilhan, J., Sarrat, C., & Miglietta, F. (2009). Detecting regional variability in sources and sinks of carbon dioxide: A synthesis. Biogeosciences, 6(6), 1015–1026. https://doi.org/10.5194/bg-6-1015-2009

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