The relationship between the meridional profile of zonal-mean geostrophic wind and station wave at 500 hPa

The sea-level pressure (SLP), 500 hPa height, zonal-mean 500 hPa height ([Z (500)]), stationary wave eddy component of the 500 hPa height (Z(500)*) and zonal-mean 500 hPa geostrophic wind [U-g] fields poleward of 20 degreesN a re examined for the period 1958-1997, with emphasis on the winter season. T he relationships between the Arctic Oscillation (AO)index and algebraic dif ference of the zonal-mean wind in 55 degreesN and 35 degreesN (Ut) index we re investigated, making use the Monte Carlo procedure, Singular Value Decom position (SVD), Empirical orthogonal function (EOF) and regression method. The leading modes of empirical orthogonal function (EOF's) of SLP are more robust than the 500 hPa height EOF's. not only in the ratio of the two larg est eigenvalues, but in more zonally symmetric. Comparing the meridional pr ofiles of zonal-mean wind amplitude associated with the AO and Ut index, th e profiles for the two indexes are very similar, both with respect to ampli tude and the placement of the maximum and minimum. Comparing the station wa ve component of 500 hPa height field regressed upon the AO and Ut index. th ere is one-to-one correspondence between all the major centers of action in the two maps, especially in the North Atlantic and Eurasian continent. The pattern is unlike the prominent teleconnection patterns, they have hemisph eric extent and cannot be interpreted in term of the individual wavetrains.