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11.
The variation characteristics of precipitation during the winter (between October and the
following March, to be referred to as just “the winter” hereafter) in Guangdong province during the past 50
years (from 1957 to 2006) and the relationship with Pacific SST are studied using the methods of
Empirical Orthogonal Function (EOF) analysis, wavelet analysis, and correlation analysis. The results
show that The Guangdong precipitation during the winter exhibits quasi-periodic significant oscillations of
40 years and 2 years; rainfall is less from the end of the 1950s to the start of the 1970s and from the end of
the 1990s to the present than from the mid 1970s to the mid 1990s. The frequency of sustained drought is
more than sustained flooding during the winter. The Guangdong precipitation during this time period is in
significantly positive correlation to the equatorial central and eastern Pacific SST, but in a significantly
negative correlation with the western and northern Pacific SST east of the Philippine Sea. 61.5% of the
sustained drought occurred in the phase of negative anomalies of the Ni?o3.4 index and 38.5% in the
phase of positive ones. A composite analysis of atmospheric circulation is performed for the positive and
negative phases of the Ni?o3.4 region associated with the sustained drought. The results showed that a
weak polar vortex, a strong trough in Europe and a ridge near Balkhash Lake, active cold air and consistent
northerly wind anomalies controlling Guangdong at low levels, an inactive westerly low disturbance in the
low-mid latitude of the Asian continent, and a weak southern branch westerly trough, are all mutual causes
for the sustained drought. 相似文献