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Temporal and Spatial Features of the First Soaking Rain in Spring in Shijiazhuang
BIAN Tao, LI Guo-Cui, SUN Yun, CHE Shao-Jing
J4    2010, 28 (2): 179-183.  
Abstract1400)      PDF(pc) (2673KB)(1838)       Save
Based on daily precipitation data of 17 stations in Shijiazhuang during 1972-2006, the spatial and temporal variation features of the first soaking rain in spring were analyzed by using the methods of EOF, REOF and linear trend, and the relations between the first soaking rain date and spring, summer rainfall using the method of correlation analysis, as well as the typical circulation features of the first soaking rain were also analyzed. Results show that the dates of the first soaking rain in spring delayed generally from southeast and northwest to the centre of the area. The unusual weather  occurs much easily in the place where the first soaking rain date is earlier or later. In recent 35 years, the first soaking rain dates were becoming earlier with a trend of 4-5 days per decade. The precipitation was generally larger (smaller) in spring and smaller (larger) in summer when the first soaking rain was earlier (later) than normal. The dominant circulation characteristics for the first soaking rain in Shijiazhuang are westerly trough and mid-troposphere vortex.
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Clima tic Character istics and Change Rule of Rain storm in Sh ijiazhuang of Hebe i Prov ince
BIAN  Tao, WANG Li-Rong, LI Guo-Cui, GAO  Qi
J4    2009, 27 (1): 18-23.  
Abstract1566)      PDF(pc) (1012KB)(3120)       Save

Based on the daily p recip itation data from 17 meteorological stations in Shijiazhuang area during 1972 - 2007, the climatic
characteristics and change rule of rainstorm occurred in Shijiazhuang were analyzed using the linear trend, the statistical method, the
power spectrum method aswell as theMann - Kendall test, and the relation between rainstorm days and high temperature dayswas ana
lyzed in light of the Pearson correlation coefficient. Results indicated that less rainstorm years are obviouslymore in the recent 36 years
in Shijiazhuang area. In seasonal distribution, rainstorm appeared in Ap ril to November butmainly concentrated in July and August; The
increase ( decrease) trend of rainstorm ismost remarkable in June (July) ; The rainstorm started to increase slowly from the second - ten
- day ofMay, and sharp increased in early July, then achieved the peak in earlyAugust; Rainstorm number increase ( decrease) trend
ismost obvious in late June ( late July). In spatial distribution, rainstorm days decreased gradually from northwest, southeast to interior
area in Shijiazhuang, and yearly mean rainstorm days in each station is above one day. Annual rainstorm days p resented increasing
trend in the west, north and northeast of Shijiazhuang area, but decreasing trend in the east, south and northwest aswell as urban dis
trict. There is four and three years periodical change in the number of rainstorm, and negative correlation between rainstorm days and
high temperature days in Shijiazhuang area.

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