::::::::::::::::::::::::::::::::::::: ::::::: Last Update: 24 Aug 2019 ::::::: :::::::::::::::::::::::::::::::::::::
Madden-Julian Oscillation - Seasonal Index
MJO Resonance Intensity Index - Equatorial Kelvin Wave
Zonal Wind Burst Phenomenon
Analysis By: Principal Coordinate Analysis [PCoA] Correlation Bi-variate Linear Regression [Residuals] + Finite impulse response (FIR) High Pass [0.001] Variable: Zonal Winds (u-m/s) Zonal Wind Burst Index at 1000hPa, 925hpa, 850hpa, 700hPa Equatorial - In Indian Ocean Index: Lat -15 To 15 &Long: 40 To 100 Equatorial - Western Pacific Index: Lat -15 To 15 & Long: 150 To 210
Summary ZWB Theory Zonal Wind Burst Phenomenon Phase
:::::: 1- ZWB Atmospheric variables :::::::
1- Zonal Wind Burst Phenomenon - Multi-Index
Analysis Date: 21 Aug 2017 To 21 Aug 2019
A - ZWB Sub-Seasonal Index
In Indian Ocean: Equatorial - Lat -15 To 15 -Long: 40 To 100 + In Western Pacific:Equatorial - Lat -15 To 15 = - Long: 150 To 210
B - ZWB Seasonal Index
In Indian Ocean: Equatorial - Lat -15 To 15 - Long: 40 To 100 + In Western Pacific: Equatorial - Lat -15 To 15 = - Long: 150 To 210
C - ZWB [Differences] Seasonal Index
In Indian Ocean: Equatorial - Lat -15 To 15 - Long: 40 To 100 + In Western Pacific: Equatorial - Lat -15 To 15 = - Long: 150 To 210