Abstract

Boreal summer intraseasonal oscillation (BSISO) is one of the dominant modes of intraseasonal variability of the tropical climate system, which has fundamental impacts on regional summer monsoons, tropical storms, and extra-tropical climate variations. Due to its distinctive characteristics, a specific metric for characterizing observed BSISO evolution and assessing numerical models’ simulations has previously been proposed (Lee et al. in Clim Dyn 40:493–509, 2013). However, the current dynamical model’s prediction skill and predictability have not been investigated in a multi-model framework. Using six coupled models in the Intraseasonal Variability Hindcast Experiment project, the predictability estimates and prediction skill of BSISO are examined. The BSISO predictability is estimated by the forecast lead day when mean forecast error becomes as large as the mean signal under the perfect model assumption. Applying the signal-to-error ratio method and using ensemble-mean approach, we found that the multi-model mean BSISO predictability estimate and prediction skill with strong initial amplitude (about 10 % higher than the mean initial amplitude) are about 45 and 22 days, respectively, which are comparable with the corresponding counterparts for Madden–Julian Oscillation during boreal winter (Neena et al. in J Clim 27:4531–4543, 2014a). The significantly lower BSISO prediction skill compared with its predictability indicates considerable room for improvement of the dynamical BSISO prediction. The estimated predictability limit is independent on its initial amplitude, but the models’ prediction skills for strong initial amplitude is 6 days higher than the corresponding skill with the weak initial condition (about 15 % less than mean initial amplitude), suggesting the importance of using accurate initial conditions. The BSISO predictability and prediction skill are phase and season-dependent, but the degree of dependency varies with the models. It is important to note that the estimation of prediction skill depends on the methods that generate initial ensembles. Our analysis indicates that a better dispersion of ensemble members can considerably improve the ensemble mean prediction skills.

Highlights

  • One of the fundamental features of tropical intraseasonal oscillations (ISOs) is the pronounced seasonal variations in their intensity (Madden 1986), movement (Wang and Rui 1990), and periodicity (Hartmann et al 1992)

  • We examined the Boreal summer intraseasonal oscillation (BSISO) prediction skill and estimated its predictability in order to better understand the way to narrow down the gap between the present day prediction capabilities and the predictability limit

  • Using the daily hindcast data from six coupled climate models that participated in Intraseasonal Variability Hindcast Experiment (ISVHE) project, the hindcast BSISO index was obtained by projecting the combined outgoing longwave radiation (OLR) and U850 anomalous fields onto observed BSISO EOF modes

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Summary

Introduction

One of the fundamental features of tropical intraseasonal oscillations (ISOs) is the pronounced seasonal variations in their intensity (Madden 1986), movement (Wang and Rui 1990), and periodicity (Hartmann et al 1992). Summer ISO (BSISO) exhibits several fundamental characteristics that distinguish it from the eastward propagating Madden–Julian Oscillation (MJO) prevailing during boreal winter (Waliser 2006; Goswami 2011): It exhibits prominent northward propagation in the monsoon regions (Yasunari 1979; Krishnamurti and Subrahmanyam 1982; Chen and Murakami 1988) and a significant standing oscillation component between the equatorial Indian Ocean and the tropical western North Pacific (Zhu and Wang 1993). For the BSISO predictability, it is found that the mean predictability of the monsoon ISO-related rainfall over the Asian–western Pacific region (10°S–30°N, 60°–160°E) reaches about 24 days in the coupled model and this is 1 week higher than in the atmosphere-only model (Fu et al 2007)

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