Barbara Casati
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Addressing the Effects of Station Network Geographical Inhomogeneity on Spatially Aggregated Verification Scores
1 Introduction Operational verification performed in National Weather Services produces routinely large amounts of verification statistics, to monitor the quality of their forecast products. Verification scores of Numerical Weather Prediction (NWP) systems against station observations are often aggregated over different geographical domains and plotted as a function of the forecast lead-time.
On the Reliability of Surface Observations and the Pitfalls of Verification Against Own Analyses
1 Introduction Numerical Weather Prediction (NWP) is mainly an initial value problem: given the current atmospheric conditions (initial conditions), we integrate a set of partial differential equations that govern atmospheric motion and evolution to obtain future atmospheric states (Pu and Kalnay 2018).
On the Reliability of Surface Observations and the Pitfalls of Verification Against Own Analyses
1 Introduction Numerical Weather Prediction (NWP) is mainly an initial value problem: given the current atmospheric conditions (initial conditions), we integrate a set of partial differential equations that govern atmospheric motion and evolution to obtain future atmospheric states (Pu and Kalnay 2018).
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