The Southern Oscillation Index (SOI) is a standardized index based on the observed sea level pressure differences between Tahiti and Darwin, Australia. The SOI is one measure of the large-scale fluctuations in air pressure occurring between the western and eastern tropical Pacific (i.e., the state of the Southern Oscillation) during El Niño and La Niña episodes. In general, smoothed time series of the SOI correspond very well with changes in ocean temperatures across the eastern tropical Pacific. The negative phase of the SOI represents below-normal air pressure at Tahiti and above-normal air pressure at Darwin. Prolonged periods of negative (positive) SOI values coincide with abnormally warm (cold) ocean waters across the eastern tropical Pacific typical of El Niño (La Niña) episodes. The methodology used to calculate SOI is available below. More information can be found at the Climate Prediction Center SOI page.
| Dec 2012 | Jan 2013 | Feb 2013 | Mar 2013 | Apr 2013 |
|---|---|---|---|---|
Note the anomalies are departures from the 1951-1980 base period.
| SOI | = | (Standardized Tahiti - Standardized Darwin) |
|---|---|---|
| MSD |
where
| Standardized Tahiti | = | (Actual Tahiti SLP - Mean Tahiti SLP) |
|---|---|---|
| Standard Deviation Tahiti |
where
| Standard Deviation Tahiti | = SQRT | ∑ (actual Tahiti SLP - mean Tahiti SLP)2 | ||
|---|---|---|---|---|
| N |
where
N = number of months
and
| Standardized Darwin | = | (Actual Darwin SLP - Mean Darwin SLP) |
|---|---|---|
| Standard Deviation Darwin |
where
| Standard Deviation Darwin | = SQRT | ∑ (actual Darwin SLP - mean Darwin SLP)2 | ||
|---|---|---|---|---|
| N |
where
N = number of months
and
| MSD | = Monthly Standard Deviation = SQRT | ∑ (Standardized Tahiti - Standardized Darwin)2 | ||
|---|---|---|---|---|
| N |
where
N = number of summed months
For more information about content specific to this page, please Contact Us.
http://www.ncdc.noaa.gov/teleconnections/enso/indicators/soi.php
