Abstract

With the development of high-performance computer systems and data assimilation techniques, storm-scale numerical weather prediction (NWP) models are gradually used for short-term deterministic forecasts. The primary objective of this study is to evaluate and correct precipitation forecasts of a storm-scale NWP model called the advanced regional prediction system (ARPS). The evaluation and correction consider five heavy precipitation events that occurred in the summer of 2015 in Jiangsu, China. The performances of the original and corrected ARPS precipitation forecasts are evaluated as a function of lead time using standard measurements and a spatial verification method called Structure-Amplitude-Location (SAL). In general, the ARPS could not produce optimal forecasts for very short lead times, and the forecast accuracy improves with increasing lead time. The ARPS overestimates precipitation for all lead times, which is confirmed by large bias in many forecasts in the first and second quadrant of the diagram of SAL, especially at the 1 h lead time. The amplitude correction is performed by matching percentile values of the ARPS precipitation forecasts and observations for each lead time. Amplitude correction significantly improved the ARPS precipitation forecasts in terms of the considered performance indices of standard measures and A-component and S-component of SAL.

Highlights

  • Heavy rain is one of the most severe weather events in China, causing floods and other geological and hydrological disasters

  • This paper quantitatively evaluated the original advanced regional prediction system (ARPS) precipitation forecasts and addressed and corrected the forecast error in Jiangsu

  • The ARPS model yields overestimated and widespread precipitation at a lead time of 1 h, which was confirmed by the significantly large bias and that most forecasts were concentrated in the top hand corner of Figure 6(a)

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Summary

Introduction

Heavy rain is one of the most severe weather events in China, causing floods and other geological and hydrological disasters. High-resolution quantitative precipitation forecasts (QPFs) play an important role in flash flood warning and emergency response. NWP models with atmospheric dynamic constraints have been used to operate for middle and long term weather forecast. The accuracy of NWP model forecasts during the first few hours is always influenced by the “spinup” problem [1]. Precipitation forecasts of NWP models are less accurate than predictions of extrapolationbased techniques at short-term lead times [2]. With the development of high-performance computers and the use of rapid-update-cycle (RUC) approach, the “spin-up” problem of NWP models has been significantly reduced

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