Abstract

In contrast to the historical forecast test which is temporally successive with a near-steady forecast skill, the real-time forecast made at any one moment produces a forecast time-series whose skill is rapidly decreasing as the forecast lead time increases, thus only the leading section of the latter is adopted in practical applications. As compared with the intraseasonal filtered historical forecast, the real-time extended-range forecast has a lower skill in the absence of filtering. In addition, it is difficult to estimate the intraseasonal phases near the end of the real-time forecast time-series due to missed information afterwards. The current work developed a simple but useful method to improve the real-time forecast skill from the above two aspects for an empirical extended-range forecast scheme. The scheme is devoted to predict the intraseasonal variabilities of the Indian summer monsoon precipitation, in which the boreal summer intraseasonal oscillation acts as the precursor. The intraseasonal signals in the previous observations, the better forecast skills of shorter lead times, the implicit information regarding the intraseasonal phases in the forecast of longer lead times, as well as the data-adaptive intraseasonal filter are adopted in the improving method, so as to extract the intraseasonal signal as much as possible from the currently available information at each forecast moment. A practical comparison shows that the forecast skills of the real-time forecast improved by this method are close to or even better than the intraseasonal filtered historical forecast. Even at the longest acceptable forecast lead time that the forecast after which is considered to be worthless, it helps extracting useful information regarding the intraseasonal phases.

Highlights

  • Each summer, the Indian summer monsoon (ISM) brings about 80% of annual rainfall over Peninsular India and affects more than one billion people living there

  • All authors contributed to the article and approved the submitted version

Read more

Summary

INTRODUCTION

The Indian summer monsoon (ISM) brings about 80% of annual rainfall over Peninsular India and affects more than one billion people living there. The following facts or assumptions are utilized in achieving this purpose: FIGURE 4 | Anomaly correlations of the observed and forecast precipitation anomalies on the intraseasonal timescale (20- to 80-day band-pass filtered) during 2004–2009 JJA at different forecast lead times (indicated at the top-right corners). Notice that the forecast instantaneous phase is not calculated with the timeseries shown in the figure (red line) but with the constructed and filtered time-series at each point Both the anomaly correlation and ratio of in-phase improved significantly relative to the regular real-time forecast (Figure 7) and are even higher than those in the intraseasonal filtered historical forecast (Figure 5). Even at the longest acceptable forecast lead time, the forecast after which is considered to be worthless, we can still extract information to improve the forecast of intraseasonal phases

SUMMARY
DATA AVAILABILITY STATEMENT
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call