Abstract
Abstract. A four-dimensional variational (4D-Var) data assimilation system for inverse modelling of atmospheric methane emissions is presented. The system is based on the TM5 atmospheric transport model. It can be used for assimilating large volumes of measurements, in particular satellite observations and quasi-continuous in-situ observations, and at the same time it enables the optimization of a large number of model parameters, specifically grid-scale emission rates. Furthermore, the variational method allows to estimate uncertainties in posterior emissions. Here, the system is applied to optimize monthly methane emissions over a 1-year time window on the basis of surface observations from the NOAA-ESRL network. The results are rigorously compared with an analogous inversion by Bergamaschi et al. (2007), which was based on the traditional synthesis approach. The posterior emissions as well as their uncertainties obtained in both inversions show a high degree of consistency. At the same time we illustrate the advantage of 4D-Var in reducing aggregation errors by optimizing emissions at the grid scale of the transport model. The full potential of the assimilation system is exploited in Meirink et al. (2008), who use satellite observations of column-averaged methane mixing ratios to optimize emissions at high spatial resolution, taking advantage of the zooming capability of the TM5 model.
Highlights
Inverse modelling has been widely used as a tool to improve our knowledge on sources and sinks of atmospheric trace gases based on measurements of concentrations in the atmosphere (Enting, 2002)
Satellite observations of column-averaged methane mixing ratio became available from the Scanning Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY) instrument on board ESA’s environmental satellite ENVISAT (Buchwitz et al, 2005; Frankenberg et al, 2005, 2006; Buchwitz et al, 2006)
The purpose of this paper is to present and evaluate a new 4D-Var system for inverse modelling of methane emissions
Summary
Inverse modelling has been widely used as a tool to improve our knowledge on sources and sinks of atmospheric trace gases based on measurements of concentrations in the atmosphere (Enting, 2002). Since such inversions of atmospheric transport are often ill-conditioned, a priori information on the spatial and temporal distribution of sources and sinks derived from emission inventories is normally used to regularize the problem. Bergamaschi et al (2007) (hereafter B07) used these observations – along with the conventional surface measurements – for the first time to optimize continental-scale emission rates
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