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Characteristic analysis of early spring hail in Chengdu based on S-band polarization radar
ZHOU Cong, ZHANG Tao, XIA Xin, ZHANG Kui
Journal of Arid Meteorology    2024, 42 (1): 95-106.   DOI: 10. 11755/j. issn. 1006-7639(2024)-01-0095
Abstract82)      PDF(pc) (35923KB)(180)    PDF(mobile) (35923KB)(8)    Save
 In order to better carry out the monitoring, forecasting and early warning of hail weather in Chengdu, the characteristics of
dual-polarization parameters of hail in early spring in Chengdu were studied by using the S-band dual-polarization radar detection of Chengdu, combined with the regional automatic weather station and conventional observation data. The fine structure of hail cloud was analyzed and compared with the short-term heavy precipitation in early spring of the same year. The results show that under the dynamic condition of strong ascending motion formed by the coupling of the high and lower-level jets, the high-level cold advection combined with the surface cold air jointly triggered the hail weather of Chengdu “3·16”. At the maturity stage, the central reflectivity factor (ZH) of hail cloud was more than 70 dBZ and there were obvious overhanging strong echo. Besides, the differential reflectivity (ZDR) and correlation coefficient (CC) of hail cloud were concentrated in –2–1 dB and 0.8–0.95, respectively, accompanied by specific differential phase shift rate (KDP) hole and CC valley structure in front of the cloud, and there was a typical ZDR column near strong updraft. With the
weakening of the ascending motion, the ZDR large value area decreases with distance appeares in front of hail cloud, while CC shows increasing trend. Compared to hail cloud, the ZH of heavy precipitation convective cloud was smaller, while the ZDR and CC were significantly larger, and there was no overhanging strong echo and obvious ZDR column in front of the convective cloud.

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Low-level Wind Field Characteristic Observed by Wind Profile Radar During Two Rainstorm Processes in Chengdu#br#
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WANG Jiajin, ZHANG Qi, ZHANG Tao, LONG Keji, SHI Rui,
Journal of Arid Meteorology    2021, 39 (1): 87-95.  
Abstract399)      PDF(pc) (3550KB)(1498)       Save
 Based on the high temporal and spatial resolution data of wind profile radar, the characteristics of the low-altitude wind field during the two rainstorm processes in Chengdu in July 2018 were analyzed. The results are as follows: (1) Before the start of heavy precipitation, the southward wind of 2-4 km strengthened and even reached the strength of jet stream. The peak value of jet index had a certain advance compared with the beginning time of short-term heavy precipitation. (2) When the short-time heavy precipitation started from the invasion of cold air in the middle and lower layer, the disturbance of wind field near the height of 0.5 km occured about 1 h earlier than the start time of heavy precipitation. (3) The two heavy precipitation processes showed that the strong vertical shear generated by strengthening of the south wind was conducive to the occurrence of heavy precipitation, while the strong shear generated by strengthening of the north wind weakened the precipitation.




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Temporal and Spatial Distribution Characteristics of Cold Waves in Eastern Hexi Corridor During 1960-2017
LI Wanrong, ZHANG Tao
Journal of Arid Meteorology    2019, 37 (5): 747-753.   DOI: 10.11755/j.issn.1006-7639(2019)-05-0747
Abstract467)      PDF(pc) (1640KB)(2102)       Save
From the view of single station and region, based on the daily average temperature and minimum temperature data at 5 meteorological stations in eastern Hexi Corridor of Gansu Province from 1960 to 2017, the temporal and spatial variation characteristics of cold waves frequency were analyzed statistically by using linear trend analysis, Mann-Kendall test and Morlet wavelet methods. The results show that the spatial distribution of cold waves frequency and intensity was obviously different at each station of eastern Hexi Corridor. The frequency of cold waves decreased gradually from north to south except for Wuwei station, while the intensity of cold wave was strong in the north and the south and weak in the middle. The single-station cold waves mainly occurred from September to next May, while the regional cold waves distributed from October to next May, and the single-station and regional cold waves tended to happen in spring, while the strongest was easily to occur in autumn. The frequency of cold waves mutated significantly from many to few at Minqin, Yongchang and Wuwei stations of eastern Hexi Corridor from 1960 to 2017, and the mutation occurred in 1973, 1973 and 2014, respectively. The frequency of cold waves existed 41 a periodic change at five stations of eastern Hexi Corridor. The frequency of regional cold waves appeared interdecadal variation in phase, it significantly decreased firstly and then slowly increased, but the mutation wasn’t significant, and there were 42 a, 15 a, 8 a and 4 a periodic changes. The current statistical standard of cold waves can’t fully reflect cold air activity with temperature slowly declining.
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Effects of Different Color Plastic Film Mulching on the Growth and Yield of Spring Wheat in a Semi-arid Region
LEI Jun, ZHAO Funian, ZHANG Hongbing,LI Qiang, NIU Haiyang, TIAN Yu, ZHANG Tao
Journal of Arid Meteorology    DOI: 10.11755/j.issn.1006-7639(2018)-04-0561
Change of Typical Phenological Phases of Spring Wheat and Oil Flax in Semi-arid Region in Northwest China
SUN Run1,2, LEI Jun, SHANG Junlin, GUO Jiping,ZHANG Tao, ZHANG Haiyao, LI Qiang
Journal of Arid Meteorology    DOI: 10.11755/j.issn.1006-7639(2017)-05-0761