Articles | Volume 29, issue 1
https://doi.org/10.5194/npg-29-1-2022
https://doi.org/10.5194/npg-29-1-2022
Research article
 | 
10 Jan 2022
Research article |  | 10 Jan 2022

A waveform skewness index for measuring time series nonlinearity and its applications to the ENSO–Indian monsoon relationship

Justin Schulte, Frederick Policelli, and Benjamin Zaitchik

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Justin Schulte on behalf of the Authors (20 Jun 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (05 Jul 2021) by Norbert Marwan
AR by Justin Schulte on behalf of the Authors (24 Jul 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (02 Aug 2021) by Norbert Marwan
AR by Justin Schulte on behalf of the Authors (12 Aug 2021)  Author's response   Manuscript 
Download
Short summary
The skewness of a time series is commonly used to quantify the extent to which positive (negative) deviations from the mean are larger than negative (positive) ones. However, in some cases, traditional skewness may not provide reliable information about time series skewness, motivating the development of a waveform skewness index in this paper. The waveform skewness index is used to show that changes in the relationship strength between climate time series could arise from changes in skewness.