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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
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1- ZWB Atmospheric variables
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​ 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

2 - Zonal Wind Burst Phenomenon Phase

A- ZWB [Correlation] Seasonal Index

​​Analysis Date: 21 Aug 2017 To 21 Aug 2019

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B- ZWB [Differences] Seasonal Index

​​Analysis Date: 21 Aug 2017 To 21 Aug 2019

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Zonal Wind Burst Phenomenon
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2- ZWB Atmospheric-Oceanic [A-O] variables
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1- ZWP [A-O] Coupling Index