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STATISTICAL ANALYSIS OF LOW-LEVEL JET STREAMS IN NANJING AREA BASED ON WIND PROFILER DATA

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doi: 10.16555/j.1006-8775.2016.02.016

  • In order to understand the activity characteristics of low-level jets in the Nanjing area, statistical analysis and comparative study are carried out on their monthly and diurnal variations, characteristics of their cores and accompanying weather conditions using wind profile data in 2005―2008 collected by two wind profilers. The results show that low-level jets have significant monthly and diurnal variations. They occur more frequently in spring and summer than in autumn and winter and are more active in early morning and at night, with the maximum wind speed usually occurring at midnight. The central part of the low-level jet occurs mainly at the height of less than 1400 meters, and the enhancement of central speed is beneficial to the appearance of precipitation. Meanwhile, when the low-level jet appears in summer, it helps cause heavy rain. The statistical results of the boundary wind profiler are well consistent with those of the tropospheric wind profiler. Two kinds of wind profilers also have the capability of continuously detecting the development of low-level jets.

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CHEN Nan, HU Ming-bao, ZHANG Cheng-cheng, et al. STATISTICAL ANALYSIS OF LOW-LEVEL JET STREAMS IN NANJING AREA BASED ON WIND PROFILER DATA [J]. Journal of Tropical Meteorology, 2016, 22(3): 426-432, https://doi.org/10.16555/j.1006-8775.2016.02.016
CHEN Nan, HU Ming-bao, ZHANG Cheng-cheng, et al. STATISTICAL ANALYSIS OF LOW-LEVEL JET STREAMS IN NANJING AREA BASED ON WIND PROFILER DATA [J]. Journal of Tropical Meteorology, 2016, 22(3): 426-432, https://doi.org/10.16555/j.1006-8775.2016.02.016
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Manuscript revised: 14 April 2016
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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STATISTICAL ANALYSIS OF LOW-LEVEL JET STREAMS IN NANJING AREA BASED ON WIND PROFILER DATA

doi: 10.16555/j.1006-8775.2016.02.016

Abstract: In order to understand the activity characteristics of low-level jets in the Nanjing area, statistical analysis and comparative study are carried out on their monthly and diurnal variations, characteristics of their cores and accompanying weather conditions using wind profile data in 2005―2008 collected by two wind profilers. The results show that low-level jets have significant monthly and diurnal variations. They occur more frequently in spring and summer than in autumn and winter and are more active in early morning and at night, with the maximum wind speed usually occurring at midnight. The central part of the low-level jet occurs mainly at the height of less than 1400 meters, and the enhancement of central speed is beneficial to the appearance of precipitation. Meanwhile, when the low-level jet appears in summer, it helps cause heavy rain. The statistical results of the boundary wind profiler are well consistent with those of the tropospheric wind profiler. Two kinds of wind profilers also have the capability of continuously detecting the development of low-level jets.

CHEN Nan, HU Ming-bao, ZHANG Cheng-cheng, et al. STATISTICAL ANALYSIS OF LOW-LEVEL JET STREAMS IN NANJING AREA BASED ON WIND PROFILER DATA [J]. Journal of Tropical Meteorology, 2016, 22(3): 426-432, https://doi.org/10.16555/j.1006-8775.2016.02.016
Citation: CHEN Nan, HU Ming-bao, ZHANG Cheng-cheng, et al. STATISTICAL ANALYSIS OF LOW-LEVEL JET STREAMS IN NANJING AREA BASED ON WIND PROFILER DATA [J]. Journal of Tropical Meteorology, 2016, 22(3): 426-432, https://doi.org/10.16555/j.1006-8775.2016.02.016

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