EU Index
24 November, 2023
Yoshihiro Tachibana (Mie University)
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The definition of EU index
1) EOF was applied to a temporal covariance matrix of geopotential height fields for individual calendar months using a monthly geopotential height field at 500 hPa for the Eurasia region (20W-160E, 30-67.5N).
2) The daily time series of the EU index is obtained by projecting daily geopotential height anomalies onto the EOF of each month.
Details are shown in Tachibana et al. (2007).
References
Tachibana. Y., T. Nakamura, and N. Tazou (2007) Interannual variation in snow-accumulation events in Tokyo and its relationship to the Eurasian pattern.SOLA, 3, 129-132. doi: 10.2151/sola.2007‒033. (Link)