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Amela Jeričević

Researcher at Croatian Meteorological and Hydrological Service

Publications -  29
Citations -  559

Amela Jeričević is an academic researcher from Croatian Meteorological and Hydrological Service. The author has contributed to research in topics: Air quality index & Numerical weather prediction. The author has an hindex of 10, co-authored 29 publications receiving 493 citations.

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Model evaluation and ensemble modelling of surface-level ozone in Europe and North America in the context of AQMEII

TL;DR: In this paper, the authors investigated the optimal ensemble size and quality of the members based on a clustering methodology to build a skilful ensemble based on model association and data clustering, which makes no use of priori knowledge of model skill.
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The low-level katabatic jet height versus Monin–Obukhov height

TL;DR: The authors showed that for sufficiently stratified flows over moderately sloped surfaces, Monin-Obukhov scaling is inadequate for describing the basic ABL dynamics, which is often governed by katabatic and drainage flows.
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Parameterization of vertical diffusion and the atmospheric boundary layer height determination in the EMEP model

TL;DR: In this article, the authors introduced two changes of the turbulence parameterization for the EMEP (European Monitoring and Evaluation Programme) Eulerian air pollution model: the replacement of the Blackadar in stable and O'Brien in unstable turbulence formulations with an analytical vertical diffusion profile (K(z)) called Grisogono, and a different mixing height determination, based on a bulk Richardson number formulation (RiB), which has been validated in all stability conditions against the observed daily surface nitrogen dioxide (NO2), sulphur dioxide (SO2) and sulphate (SO
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The critical bulk Richardson number in urban areas: verification and application in a numerical weather prediction model

TL;DR: In this article, the impact of urban areas on the choice of critical values of bulk Richardson number (Ri Bc ) was explored, and different values were used for convective boundary layer (CBL) and for stable boundary layer(SBL).