Effect of the Form of the Error Correlation Functions on Uncertainty in the Estimation of Atmospheric Aerosol Distribution When Using Spatial-Temporal Optimal Interpolation

Spatial-temporal optimal interpolation (STOI) is a data assimilation method based on minimizing the error in an estimate. Error correlations can be modeled with analytical functions. We investigated the effect of the form of the error correlation functions on the uncertainty in an estimate. We applied STOI to the estimation of aerosol distribution over Europe using the results of GEOS-Chem chemical transport model simulations and observations from a ground-based radiometric Aerosol Robotic Network. We used exponential functions to model correlation curves. The results show that a ±15–25% change in the argument of the constructed exponential functions has little effect on the mean square error in the estimate in regions where observations are dense. STOI estimates are sensitive to the form of the correlation curves in regions where observations are sparse.

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Published
2025-09-22
DOI
https://doi.org/10.3390/eesp2025034011
Primary Topic
Atmospheric aerosols and clouds
Type
article
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article

Effect of the Form of the Error Correlation Functions on Uncertainty in the Estimation of Atmospheric Aerosol Distribution When Using Spatial-Temporal Optimal Interpolation

Anatoly Chaikovsky, Natallia Miatselskaya, Аndrey Bril
Atmospheric aerosols and clouds
article

Effect of the Form of the Error Correlation Functions on Uncertainty in the Estimation of Atmospheric Aerosol Distribution When Using Spatial-Temporal Optimal Interpolation

Anatoly Chaikovsky, Natallia Miatselskaya, Аndrey Bril
article en

Abstract

Spatial-temporal optimal interpolation (STOI) is a data assimilation method based on minimizing the error in an estimate. Error correlations can be modeled with analytical functions. We investigated the effect of the form of the error correlation functions on the uncertainty in an estimate. We applied STOI to the estimation of aerosol distribution over Europe using the results of GEOS-Chem chemical transport model simulations and observations from a ground-based radiometric Aerosol Robotic Network. We used exponential functions to model correlation curves. The results show that a ±15–25% change in the argument of the constructed exponential functions has little effect on the mean square error in the estimate in regions where observations are dense. STOI estimates are sensitive to the form of the correlation curves in regions where observations are sparse.

National Academy of Sciences of Belarus (BY)
Openalex Percentile: Top 76%
Atmospheric aerosols and clouds
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