Abstract

The Madden Julian Oscillation (MJO), the dominant subseasonal variability in the tropics, is widely represented using the Real-time Multivariate MJO (RMM) index. The index is limited to the satellite era (post-1974) as its calculation relies on satellite-based observations. Oliver and Thompson (J Clim 25:1996–2019, 2012) extended the RMM index for the twentieth century, employing a multilinear regression on the sea level pressure (SLP) from the NOAA twentieth century reanalysis. They obtained an 82.5% correspondence with the index in the satellite era. In this study, we show that the historical MJO index can be successfully reconstructed using machine learning techniques and improved upon. We obtain a significant improvement of up to 4%, using the support vector regressor (SVR) and convolutional neural network (CNN) methods on the same set of predictors used by Oliver and Thompson. Based on the improved RMM indices, we explore the long-term changes in the intensity, phase occurrences, and frequency of the winter MJO events during 1905–2015. We show an increasing trend in MJO intensity (22–27%) during this period. We also find a multidecadal change in MJO phase occurrence and periodicity corresponding to the Pacific Decadal Oscillation (PDO), while the role of anthropogenic warming cannot be ignored.

Highlights

  • The Madden Julian Oscillation (MJO), the dominant subseasonal variability in the tropics, is widely represented using the Real-time Multivariate MJO (RMM) index

  • The MJO index derived from our multivariate linear regression (MLR) is very similar to the OT12 index which is computed based on 54 ensembles of 20CRV3 reanalyses

  • We explore the possibility of historical reconstruction of the MJO using machine learning algorithms, thereby improving the existing historical MJO index (OT12)

Read more

Summary

Introduction

The Madden Julian Oscillation (MJO), the dominant subseasonal variability in the tropics, is widely represented using the Real-time Multivariate MJO (RMM) index. Oliver and Thompson (J Clim 25:1996–2019, 2012) extended the RMM index for the twentieth century, employing a multilinear regression on the sea level pressure (SLP) from the NOAA twentieth century reanalysis They obtained an 82.5% correspondence with the index in the satellite era. The use of satellite OLR along with zonal winds is a crucial factor in the definition of the WH04 RMM index as it explains the amount of convective activity associated with the MJO circulation. This factor distinguishes the WH04 RMM index from other solely dynamical or convection based MJO indices like velocity potential ­index[5] and bimodal ISO i­ndices[6], respectively. Using the zonal winds (a dynamical proxy of MJO) from NCEP-NCAR reanalysis, Jones and ­Carvalho[7] showed that there were significant trends in the intensity of MJO in boreal winter and summer, during the Scientific Reports | (2020) 10:18567

Objectives
Methods
Results
Conclusion
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