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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 3
Clim. Past, 9, 1141–1152, 2013
https://doi.org/10.5194/cp-9-1141-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 9, 1141–1152, 2013
https://doi.org/10.5194/cp-9-1141-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 May 2013

Research article | 17 May 2013

An assessment of particle filtering methods and nudging for climate state reconstructions

S. Dubinkina and H. Goosse S. Dubinkina and H. Goosse
  • Earth and Life Institute, Georges Lemaître Centre for Earth and Climate Research, Université catholique de Louvain, P.O. Box L4.03.07, 1348 Louvain-la-Neuve, Belgium

Abstract. Using the climate model of intermediate complexity LOVECLIM in an idealised framework, we assess three data-assimilation methods for reconstructing the climate state. The methods are a nudging, a particle filter with sequential importance resampling, and a nudging proposal particle filter and the test case corresponds to the climate of the high latitudes of the Southern Hemisphere during the past 150 yr. The data-assimilation methods constrain the model by pseudo-observations of surface air temperature anomalies obtained from the same model, but different initial conditions. All three data-assimilation methods provide with good estimations of surface air temperature and of sea ice concentration, with the nudging proposal particle filter obtaining the highest correlations with the pseudo-observations. When reconstructing variables that are not directly linked to the pseudo-observations such as atmospheric circulation and sea surface salinity, the particle filters have equivalent performance and their correlations are smaller than for surface air temperature reconstructions but still satisfactory for many applications. The nudging, on the contrary, obtains sea surface salinity patterns that are opposite to the pseudo-observations, which is due to a spurious impact of the nudging on vertical exchanges in the ocean.

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