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Climate Change Research ›› 2020, Vol. 16 ›› Issue (2): 203-214.doi: 10.12006/j.issn.1673-1719.2019.051
• Changes in Climate System • Previous Articles Next Articles
Received:
2019-03-08
Revised:
2019-04-12
Online:
2020-03-30
Published:
2020-04-01
Contact:
Ping ZHAO
E-mail:zhaop@cma.gov.cn
LIU Chong,ZHAO Ping. Climatological characteristics of Sichuan Basin vortex during 1979-2016[J]. Climate Change Research, 2020, 16(2): 203-214.
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URL: http://www.climatechange.cn/EN/10.12006/j.issn.1673-1719.2019.051
Fig. 4 The moving tracks of Sichuan Basin vortexes that move out of the target area (a) eastward-migrating type, (b) northeastward-migrating type, (c) southeastward-migrating type, (d) westward-migrating type (blue dot indicates the generation of a vortex, green dot indicates the degeneration of the vortex, while red line connecting the two dots shows the moving track of the vortex)
Fig. 5 South-north cross sections of composite fields for different types of long-lived Sichuan Basin vortexes in summer (vertical velocity has been increased a hundredfold, unit for wind vectors: m/s; blue lines indicate relative humidity, unit: %)
Fig. 8 Composite moving tracks and precipitation in 6 hours for long-lived Sichuan Basin vortexes in summer (the black dot indicates the averaged initial location of the vortex in different developing periods, and the red dot indicates the location of the vortex after 6 h)
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