Journal of Meteorology and Environment ›› 2022, Vol. 38 ›› Issue (5): 25-33.doi: 10.3969/j.issn.1673-503X.2022.05.003
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Jing LIU1,2(),Chuan-lei CHEN2,Ying WANG2,Kui-zhi CAI2,*(
),Chuan REN3,Wei DONG4
Received:
2021-01-05
Online:
2022-10-28
Published:
2022-11-04
Contact:
Kui-zhi CAI
E-mail:liujing-syau@163.com;ckz_ivan@163.com
CLC Number:
Jing LIU, Chuan-lei CHEN, Ying WANG, Kui-zhi CAI, Chuan REN, Wei DONG. Comparison of neighborhood verification of radar echo forecast in Liaoning province using four high-resolution models[J]. Journal of Meteorology and Environment, 2022, 38(5): 25-33.
Table 2
Occurrence date of selected convective weather processes in Liaoning province in 2017 and 2018"
序号 | 区域性降水时间 | 局地性降水时间 |
1 | 2017-07-22 | 2017-06-19 |
2 | 2017-08-27 | 2017-07-09 |
3 | 2017-08-15 | 2017-07-13 |
4 | 2017-08-24 | 2017-07-14 |
5 | 2017-09-07 | 2017-09-10 |
6 | 2018-07-08 | 2018-06-17 |
7 | 2018-08-14 | 2018-07-09 |
8 | 2018-08-18 | 2018-08-13 |
9 | 2018-08-23 | 2018-08-20 |
10 | 2018-09-15 | 2018-09-02 |
Table 3
Setting parameters of the four high-resolution models"
模式名称 | 区域 | 空间分辨率 | 时间分辨率 | 范围 | 调整后范围 |
华东模式 | 华东区域 | 0.03°×0.03° | 逐小时 | 5°~60°N 50°~160°E | 37°~46°N 115°~127°E |
华北模式 | 华北区域 | 0.03°×0.03° | 逐小时 | 33°~48°N 104°~124°E | 37°~46°N 115°~127°E |
GRAPES_3km | 全国重点区域 | 0.03°×0.03° | 逐小时 | 10°~60°N 70°~145°E | 37°~46°N 115°~127°E |
睿图东北 | 东北地区 | 0.03°×0.03° | 逐小时 | 37°~54°N 112°~135°E | 37°~46°N 115°~127°E |
Fig.1
Radar echo forecasts for regional precipitation processes in Northeast China from June to September in 2017 and 2018 using the East China Model (a), the North China Model (b), the GRAPES Model (c), and the Northeast China WRF Model (d), and the results for local precipitation processes (e-h)"
Fig.3
Comparison of forecast skills of radar echo using four high-resolution models with the neighborhood radius of 3 km (a1), 5 km (b1), 7 km (c1), 9 km (d1), and 11 km for regional precipitation and local precipitation (a2, b2, c2, d2) in Northeast China from June to September in 2017 and 2018"
Fig.4
Variation of FSS of radar echo forecasts for regional precipitation processes in Northeast China from June to September in 2017 and 2018 using the East China Model (a), the North China Model (b), the GRAPES Model (c), and the Northeast China WRF Model (d), and the results for local precipitation processes (e-h)"
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