International audienceWe give here an account on the results of source inversion of the ETEX-II experiment. Inversion has been performed with the maximum entropy method on the basis of non-zero measurements and in conjunction with a transport model Polair3D. The discrepancy scaling factor between the true and the reconstructed mass has been estimated to be equal to 7. The results contrast with the method's performance on the ETEX-I source. In the latter case its mass has been reconstructed with an accuracy exceeding 80%. The large value of the discrepancy factor for ETEX-II could be ascribed to modelling difficulties, possibly linked not to the transport model itself but rather to the quality of the measurements
International audienceA new method of performing the source inversion of a passive tracer at contine...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceWe give here an account on the results of source inversion of the ETEX-II expe...
International audienceWe give here an account on the results of source inversion of the ETEX-II expe...
Abstract. We give here an account on the results of source inversion of the ETEX-II experiment. Inve...
We give here an account on the results of source inversion of the ETEX-II experiment. Inversion has ...
International audienceFor a start, recent techniques devoted to the reconstruction of sources of an ...
International audienceIn a previous two-part paper, new methods for reconstructing the source of an ...
Estimation of the temporal profile of an atmospheric release, also called the source term, is an imp...
An inverse model using atmospheric CO2 observations from a European network of stations to reconstru...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceThe fate and transport of mercury over Europe is studied using a regional Eule...
International audienceThe fate and transport of mercury over Europe is studied using a regional Eule...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceA new method of performing the source inversion of a passive tracer at contine...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceWe give here an account on the results of source inversion of the ETEX-II expe...
International audienceWe give here an account on the results of source inversion of the ETEX-II expe...
Abstract. We give here an account on the results of source inversion of the ETEX-II experiment. Inve...
We give here an account on the results of source inversion of the ETEX-II experiment. Inversion has ...
International audienceFor a start, recent techniques devoted to the reconstruction of sources of an ...
International audienceIn a previous two-part paper, new methods for reconstructing the source of an ...
Estimation of the temporal profile of an atmospheric release, also called the source term, is an imp...
An inverse model using atmospheric CO2 observations from a European network of stations to reconstru...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceThe fate and transport of mercury over Europe is studied using a regional Eule...
International audienceThe fate and transport of mercury over Europe is studied using a regional Eule...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceA new method of performing the source inversion of a passive tracer at contine...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...
International audienceAn inverse model using atmospheric CO 2 observations from a European network o...