Journal of Arid Meteorology ›› 2023, Vol. 41 ›› Issue (2): 290-300.DOI: 10.11755/j.issn.1006-7639(2023)-02-0290
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Received:
2022-08-24
Revised:
2022-10-24
Online:
2023-04-30
Published:
2023-05-09
通讯作者:
张述文(1966—),男,河南固始人,教授,主要从事陆-气相互作用、资料同化与强对流天气预报研究。E-mail: zhangsw@lzu.edu.cn。
作者简介:
孙明燕(1997—),女,贵州遵义人,硕士生,主要从事中小尺度数值模拟研究。E-mail: sunmy20@lzu.edu.cn。
基金资助:
CLC Number:
SUN Mingyan, ZHANG Shuwen. Cases study of numerical simulation influences of turbulent vertical mixing intensity on local thermal convection in boundary layer[J]. Journal of Arid Meteorology, 2023, 41(2): 290-300.
孙明燕, 张述文. 边界层湍流垂直混合强度对局地热对流模拟影响的个例研究[J]. 干旱气象, 2023, 41(2): 290-300.
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URL: http://www.ghqx.org.cn/EN/10.11755/j.issn.1006-7639(2023)-02-0290
试验名称 | 试验设置 | 试验名称 | 试验设置 |
---|---|---|---|
YSU10 | p=1.00 | ACM10 | p=1.00 |
YSU15 | p=1.50 | ACM15 | p=1.50 |
YSU20 | p=2.00(模式默认值) | ACM20 | p=2.00(模式默认值) |
YSU25 | p=2.50 | ACM25 | p=2.50 |
YSU30 | p=3.00 | ACM30 | p=3.00 |
Tab.1 Experiment settings and naming of two schemes
试验名称 | 试验设置 | 试验名称 | 试验设置 |
---|---|---|---|
YSU10 | p=1.00 | ACM10 | p=1.00 |
YSU15 | p=1.50 | ACM15 | p=1.50 |
YSU20 | p=2.00(模式默认值) | ACM20 | p=2.00(模式默认值) |
YSU25 | p=2.50 | ACM25 | p=2.50 |
YSU30 | p=3.00 | ACM30 | p=3.00 |
试验名称 | 13:00 | 14:00 | 15:00 | 16:00 | 试验名称 | 14:30 | 15:00 | 16:00 | 17:00 |
---|---|---|---|---|---|---|---|---|---|
YSU10 | 0.000 | 0.000 | 0.170 | 0.099 | ACM10 | 0.000 | 0.032 | 0.284 | 0.103 |
YSU15 | 0.000 | 0.072 | 0.176 | 0.006 | ACM15 | 0.000 | 0.135 | 0.196 | 0.118 |
YSU20 | 0.000 | 0.371 | 0.205 | 0.044 | ACM20 | 0.073 | 0.273 | 0.236 | 0.163 |
YSU25 | 0.003 | 0.480 | 0.275 | 0.054 | ACM25 | 0.211 | 0.337 | 0.221 | 0.013 |
YSU30 | 0.144 | 0.336 | 0.175 | 0.056 | ACM30 | 0.303 | 0.403 | 0.307 | 0.007 |
Tab.2 FSS of simulated radar composite reflectivity under different vertical mixing intensities of two schemes
试验名称 | 13:00 | 14:00 | 15:00 | 16:00 | 试验名称 | 14:30 | 15:00 | 16:00 | 17:00 |
---|---|---|---|---|---|---|---|---|---|
YSU10 | 0.000 | 0.000 | 0.170 | 0.099 | ACM10 | 0.000 | 0.032 | 0.284 | 0.103 |
YSU15 | 0.000 | 0.072 | 0.176 | 0.006 | ACM15 | 0.000 | 0.135 | 0.196 | 0.118 |
YSU20 | 0.000 | 0.371 | 0.205 | 0.044 | ACM20 | 0.073 | 0.273 | 0.236 | 0.163 |
YSU25 | 0.003 | 0.480 | 0.275 | 0.054 | ACM25 | 0.211 | 0.337 | 0.221 | 0.013 |
YSU30 | 0.144 | 0.336 | 0.175 | 0.056 | ACM30 | 0.303 | 0.403 | 0.307 | 0.007 |
Fig.6 The vertical profile of simulated regional mean zonal wind (u), meridional wind (v), potential temperature (θ) and water vapor mixing ratio (q) at different time on 29 July 2016 under different vertical mixing intensities of two schemes (The positive and negative on the horizontal axis indicate the wind direction, which are positive to the east and the north, and negative to the west and the south)
Fig.7 The times series of simulated regional mean CAPE (a, c) and CIN (b, d) on 29 July 2016 under different vertical mixing intensities of YSU (a, b) and ACM2 (c, d) schemes
Fig.8 Evolution of observed and simulated radar composite reflectivity at Nanjing on 16 August 2013 under different vertical mixing intensities of two schemes (Unit: dBZ)
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