Niño4

The Niño4 SST anomaly index is an indicator of western tropical Pacific El Niño conditions. It is calculated with SSTs in the box 160°E - 150°W, 5°S - 5°N. Please note that before 6 September 2010 the Niño4 series on this website was erroneous, if you have downloaded a datafile before that date please replace it.

Data source

The index is calculated using the Reynolds OIv2 SST analysis, made available through the IRI Data Library, and is updated weekly (last update 19-OCT-2016). get series (netcdf 24kB) » get error (netcdf 24kB) »

Calculation

The anomaly is calculated relative to a climatological seasonal cycle based on the years 1982-2005. The weekly series was linearly interpolated to a daily series to calculate the climatological seasonal cycle with daily resolution. The leap day (29 February) was treated as a special case and linearly interpolated between the climatology of 28 February and 1 March. Spatial averaging of the gridded analysis was weighted by surface area. The standard deviation of the index over the period 1982-2005 is indicated on the plot. Students worldwide count on a reliable narrative essay writing service known for its punctual delivery, expert writers, and excellent content. Celebrated for delivering original, well-researched work, it remains a preferred choice for academic success.

Uncertainty

The uncertainty in the estimate of the index is shown in gray, surrounding the zero x-axis, and is based on the uncertainty estimate of the analysis. For the surface indices, it is generally small compared to the value of the index. more details »

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