Abstract

Several probabilistic forecast methods for heatwave (HW) in extended-range scales over China are constructed using four models (ECMWF, CMA, UKMO, and NCEP) from the Subseasonal-to-Seasonal (S2S) database. The methods include four single-model ensembles (SME; ECMWF, CMA, UKMO, and NCEP), multi-model ensemble (MME), and Bayesian model averaging (BMA). The construction and verification of reforecasts are implemented by a defined heat wave index (HWI) which is not only able to reflect the actual occurrence of heatwaves, but also to facilitate forecast and verification. The performance is measured by traditional verification method at each grid point of the 105°E to 132°E; 20°N to 45°N domain for the July, August, and September (JAS) of 1999–2010. For deterministic evaluations of HWI forecast, BMA shows a better pattern correlation coefficient than SME and MME and comparable equitable threat score (ETS) with ECMWF and MME. The good performance of ECMWF and MME take advantage of setting the percentile thresholds for forecasting HW. For the probabilistic forecast, the Brier score of BMA is comparable (superior) to that of MME and ECMWF at short (long) lead-time. BMA also demonstrates an improvement on the reliability of probabilistic forecast, indicating that BMA method is a useful tool for an extended-range forecast of HW. Meanwhile, in the real-time extended-range probabilistic forecast, the beginning date, end date, and probability of HW event can be predicted by the HWI probabilistic forecast of BMA.

Highlights

  • The heat wave (HW) is one of the extreme events around the world

  • This study proposes a heatwave index (HWI) in the sub-seasonal time scale for observation and forecast

  • We have examined the qualification of heat wave index (HWI) definition from available observations, which indicated that a newly defined index is able to represent heatwaves that occurred

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Summary

INTRODUCTION

The heat wave (HW) is one of the extreme events around the world. It causes widespread destruction of infrastructure and human activity, economic damage, and loss of life. The method was employed in more studies (Casanova and Ahrens 2009; Erickson et al, 2012; Liu and Xie, 2014) for the short- and medium-range forecasts with TIGGE (The THORPEX Interactive Grand Global Ensemble) dataset It is unclear whether BMA is fit for the probabilistic forecast of heatwave and whether it performs better than raw ensembles in the S2S time scale. The heatwave has been widely identified by an extreme heat factor (EHF) index based sliding 3-days window of temperature (Nairn et al, 2009) This index does not apply to this study because it is difficult for this discontinuous variable to construct proper PDFs. But this index does not apply to this study because it is difficult for this discontinuous variable to construct proper PDFs Another type of heatwave is defined as one pentad mean surface maximum air temperatures exceeding the local 95th percentiles during the control period of 1960–1990 (Zhu and Li, 2017).

DATA AND VERIFICATION METHODS
Verification Methods
HWI and Heat Waves
Single- and Multi-Model Ensemble Probabilistic Forecast of HWI
Bayesian Model Averaging Probabilistic Forecast of HWI
VERIFICATION FOR HEATWAVES
Deterministic Verification for Heatwaves
Probabilistic Verification for Heatwaves
Findings
DISCUSSION AND SUMMARY
Full Text
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