ECMWF降水相态诊断产品(PTYPE)偏差原因分析及改进

管靓 ,  漆梁波 ,  赵渊明

暴雨灾害 ›› 2026, Vol. 45 ›› Issue (3) : 426 -435.

PDF (1329KB)
暴雨灾害 ›› 2026, Vol. 45 ›› Issue (3) : 426 -435. DOI: 10.12406/byzh.2025-059

ECMWF降水相态诊断产品(PTYPE)偏差原因分析及改进

作者信息 +

The reason analysis and improvement of the deviation of the ECMWF precipitation type diagnostic product (PTYPE)

Author information +
文章历史 +
PDF (1360K)

摘要

为改进数值模式降水相态诊断方案,改善业务降水相态预报结果,基于地面自动站和探空实况资料、ERA5再分析资料的降水相态诊断产品(precipitation type,PTYPE)以及高空和地面的气温、露点温度数据,对比2022年和2023年冬季我国北方、西南和江南3个区域不同降水相态天气的诊断探空和实况探空差异,结合统计概念模型和降水相态物理过程对PTYPE偏差的原因进行了分析,并提出改进方法。结果表明:(1)北方和江南地区如将PTYPE的干湿雪统归为降雪,其与实测降雪数据更为吻合。西南地区PTYPE的降雪较实况偏多,可用性明显低于其他地区。(2)当前PTYPE对冻雨的诊断方案与冻雨形成的基本物理过程不符,未充分考量液滴的“过冷”属性,这可能是PTYPE“空报”冻雨的主要原因。(3)PTYPE诊断冰粒时要求2 m气温低于0 ℃,而实况的2 m气温高于0℃,这是导致PTYPE对冰粒存在较多漏判的主要原因;此外,PTYPE诊断方案中只要求到达地面附近的水成物中,固态比例≥50%,而非绝大部分保持固态甚或完全冻结,这会导致冰粒预报偏多。(4)基于对比分析,得到了对PTYPE产品的改进方法,即采用2 m湿球温度作为雨夹雪和降雪的辅助判据,增加近地面液滴的温度作为冻雨的判据,在冰粒方案中剔除2 m气温的影响,并适当降低“地面液态水含量”的阈值,可望提升降水相态的诊断准确率。

Abstract

To improve the diagnostic scheme and the forecast results of precipitation types in numerical models, the surface observational and sounding data, precipitation type diagnosis products (PTYPE) from ERA5 reanalysis data, and temperature and dew point of different pressure levels and the surface are used in this study. The PTYPE diagnostic and observational sounding data for different precipitation types in the northern, southwestern, and Jiangnan area of China from the winter of 2022 to 2023 are compared to analyze the causes of forecast biases in the PTYPE products from the aspects of statistical conceptual models and physical processes, and then the improvement methods are proposed. The results are as follows. (1) The combination of dry and wet snow incidents recognized by PTYPE is consistent with the observed snow events in the northern and Jiangnan area. However, in the southwestern area, the PTYPE tends to overestimate the number of snowfall events, suggesting significantly lower reliability in this area. (2) The PTYPE diagnostic scheme is not consistent with the fundamental physical process of freezing rain formation, overlooking the droplets' supercooled characteristics, which could be the primary reason for the “false alarm” of the freezing rain in the PTYPE product. (3) For diagnosing ice pellets, the PTYPE scheme requires a 2-m surface temperature below 0 °C, which is usually not the case for observations. This could be the main reason for the missed alarm of ice pellets. Additionally, the diagnostic scheme only requires that the proportion of the solid particles near the surface is no less than 50%, rather than a percentage of most or even all, which leads to “false alarm”. (4) Base on comprehensive analysis, an improved PTYPE scheme is proposed: using the surface wet-bulb temperature as a criterion for sleet and snow; adding near-surface droplet temperature for freezing rain; removing the surface temperature in the ice pellet scheme, and appropriately lowering the threshold of "near-surface liquid water content", which are expected to improve the accuracy of these precipitation types.

关键词

降水相态 / PTYPE 产品 / ERA5 / 偏差原因

Key words

precipitation type / PTYPE / ERA5 / deviation cause

引用本文

引用格式 ▾
管靓,漆梁波,赵渊明. ECMWF降水相态诊断产品(PTYPE)偏差原因分析及改进[J]. 暴雨灾害, 2026, 45(3): 426-435 DOI:10.12406/byzh.2025-059

登录浏览全文

4963

注册一个新账户 忘记密码

参考文献

[1]

陈双,谌芸,何立富,等. 2019.我国中东部平原地区临界气温条件下降水相态判别分析[J].气象,45(8):1037-1051.

[2]

Chen S, Chen Y, He L F, et al. 2019. Discrimination analysis of snow and rain occurring under critical temperature conditions in central and eastern China [J].Meteorological Monthly,45(8):1037-1051 (in Chinese). doi:10.7519/j.issn.1000−0526.2019.08.001

[3]

董全,胡宁,宗志平. 2020a. ECMWF 降水相态预报产品 (PTYPE) 应用和检验[J].气象,46(9):1210-1221.

[4]

Dong Q, Hu N, Zong Z P. 2020a. Application and verification of the ECMWF precipitation type forecast product (PTYPE) [J].Meteorological Monthly,46(9):1210-1221 (in Chinese). doi:10.7519/j.issn.1000−0526.2020.09.008

[5]

董全,张峰,宗志平. 2020b.基于 ECMWF 集合预报产品的降水相态客观预报方法[J].应用气象学报,31(5):527-542.

[6]

Dong Q, Zhang F, Zong Z P. 2020b. Objective precipitation type forecast based on ECMWF ensemble prediction product [J].Journal of Applied Meteorological Science,31(5):527-542 (in Chinese). doi:10.11898/1001−7313.20200502

[7]

韩念霏,杨璐,陈明轩,等. 2022.京津冀站点风温湿要素的机器学习订正方法[J].应用气象学报,33(4):489-500.

[8]

Han N F, Yang L, Chen M X, et al. 2022. Machine learning correction of wind, temperature and humidity elements in Beijing-Tianjin-Hebei Region [J].Journal of Applied Meteorological Science,33(4):489-500 (in Chinese). doi:10.11898/1001−7313.20220409

[9]

胡宁,符娇兰,孙军,等. 2021.北京一次冬季极端降水过程中相态转换预报的误差分析[J].气象学报,79(2):328-339.

[10]

Hu N, Fu J L, Sun J, et al. 2021. Errors in the forecast of precipitation type transition in an extreme winter precipitation event in Beijing [J].Acta Meteorologica Sinica,79(2):328-339 (in Chinese). doi:10.11676/qxxb2021.019

[11]

黄骄文,蔡荣辉,姚蓉,等. 2021.深度学习网络在降水判识和预报中的应用[J].气象,47(3):317-326.

[12]

Huang J W, Cai R H, Yao R, et al. 2021. Application of deep learning method to discrimination and forecasting of precipitation type [J].Meteorological Monthly,47(3):317-326 (in Chinese). doi:10.7519/j.issn.1000−0526.2021.03.005

[13]

蓝俊,韩伟中,张祖熠,等. 2023.福建省 ECMWF 细网格模式 2 m 温度预报误差分析与订正[J].气象与减灾研究,46(3):196-202.

[14]

Lan J, Han W Z, Zhang Z Y, et al. 2023. Analysis and correction of 2 m temperature forecast error of ECMWF fine grid model in Fujian province [J].Meteorology and Disaster Reduction Research,46(3):196-202 (in Chinese). doi:10.12013/qxyjzyj2023−027

[15]

李杰,郭学良,周晓宁,等. 2015. 2011~2013 年中国冻雨、冻毛毛雨和冻雾的特征分析[J].大气科学,39(5):1038-1048.

[16]

Li J, Guo X L, Zhou X N, et al. 2015. Characteristics of freezing rain, freezing drizzle, and freezing fog in China from 2011 to 2013 [J].Chinese Journal of Atmospheric Sciences,39(5):1038-1048 (in Chinese). doi:10.3878/j.issn.1006−9895.1501.14239

[17]

刘婷婷,朱秀芳,郭锐,等. 2022.ERA5 再分析降水数据在中国的适用性分析[J].干旱区地理,45(1):66-79.

[18]

Liu T T, Zhu X F, Guo R, et al. 2022. Applicability of ERA5 reanalysis of precipitation data in China [J].Arid Land Geography,45(1):66-79 (in Chinese). doi:10.12118/j.issn.1000−6060.2021.132

[19]

牛嫣静,徐向军,郭欢,等. 2020.三种全球预报产品中国区近地面气温短期预报效果检验[J].气象与环境学报,36(4):18-27.

[20]

Niu Y J, Xu X J, Guo H, et al. 2020. Verification of the short-term forecast of near-surface temperature using different global forecast products in China [J].Journal of Meteorology and Environment,36(4):18-27 (in Chinese). doi:10.3969/j.issn.1673−503X.2020.04.003

[21]

漆梁波. 2012.我国冬季冻雨和冰粒天气的形成机制及预报着眼点[J].气象,38(7):769-778.

[22]

Qi L B. 2012. Formation mechanism and forecast on freezing rain and ice pellet in winter of China [J].Meteorological Monthly,38(7):769-778 (in Chinese). doi:10.7519/j.issn.1000−0526.2012.07.001

[23]

漆梁波,张瑛. 2012.中国东部地区冬季降水相态的识别判据研究[J].气象,38(1):96-102.

[24]

Qi L B, Zhang Y. 2012. Research on winter precipitation types’discrimination criterion in eastern China [J].Meteorological Monthly,38(1):96-102 (in Chinese). doi:10.7519/j.issn.1000−0526.2012.01.011

[25]

覃皓,农孟松,翟丽萍,等. 2024.广西沿海“23.6”弱热带低压破纪录暴雨过程的诊断分析[J].气象学报,82(3):289-305.

[26]

Qin H, Nong M S, Zhai L P, et al. 2024. Diagnosis of the June 2023 record-breaking rainstorm caused by a weak tropical depression in the coastal area of Guangxi, China [J].Acta Meteorologica Sinica,82(3):289-305 (in Chinese). doi:10.11676/qxxb2024.20230121

[27]

任兆鹏,张苏平,马艳,等. 2018.青岛冬半年降水相态统计分析及判别方法研究[J].海洋气象学报,38(1):27-33.

[28]

Ren Z P, Zhang S P, Ma Y, et al. 2018. Statistical analysis and discrimination criterion on precipitation types of winter half year in Qingdao [J].Journal of Marine Meteorology,38(1):27-33 (in Chinese). doi:10.19513/j.cnki.issn2096−3599.2018.01.004

[29]

佟华,张玉涛. 2019. GRAPES-MESO 模式预报降水相态诊断及应用研究[J].大气科学学报,42(4):502-512.

[30]

Tong H, Zhang Y T. 2019. Diagnosis of precipitation types and its application in the GRAPES-MESO forecasts [J].Transactions of Atmospheric Sciences,42(4):502-512 (in Chinese). doi:10.13878/j.cnki.dqkxxb.20190416001

[31]

熊秋芬. 2011. GRAPES_Meso 模式的降水格点检验和站点检验分析[J].气象,37(2):185-193.

[32]

Xiong Q F. 2011. Verification of GRAPE-Meso precipitation forecasts based on fine mesh and station datasets [J].Meteorological Monthly,37(2):185-193 (in Chinese). doi:10.7519/j.issn.1000−0526.2011.2.008

[33]

杨晓霞,吴炜,万明波,等. 2012.山东省两次暴雪天气的对比分析[J].气象,8(7):868-876.

[34]

Yang X X, Wu W, Wan M B, et al. 2012. A comparative analysis of two snowstorms in Shandong Province [J].Meteorological Monthly,8(7):868-876 (in Chinese). doi:10.7519/j.issn.1000−0526.2012.07.013

[35]

张博,张芳华. 2024. 2024 年 2 月我国中东部两次持续性低温雨雪冰冻过程的环流异常特征分析[J].暴雨灾害,43(4):384-394.

[36]

Zhang B, Zhang F H. 2024. Characteristics of circulation anomalies of two continuous low temperature rain and snow freezing weather processes in eastern China in February 2024 [J].Torrential Rain and Disasters,43(4):384-394 (in Chinese). doi:10.12406/byzh.2024−108

[37]

张俊,于碧馨,李如琦,等. 2024.西天山南麓两次暴雪过程对比分析[J].沙漠与绿洲气象,18(5):120-127.

[38]

Zhang J, Yu B X, Li R Q, et al. 2024. Comparative analysis of two blizzard processes in the south slope of the western Tianshan Mountains [J].Deseret and Oasis Meteorology,18(5):120-127 (in Chinese). doi:10.12057/j.issn.1002−0799.2024.05.016

[39]

赵恩榕,潘筱龙,姚蓉,等. 2023.基于卫星与双极化多普勒天气雷达的湖南中部地区一次极端暴雪应用分析[J].高原山地气象研究,43(4):134-145.

[40]

Zhao E R, Pan X L, Yao R, et al. 2023. Application analysis of an extreme snowstorm in central Hunan based on satellite and dual-polarization Doppler weather radar [J].Plateau and Mountain Meteorology Research,43(4):134-145 (in Chinese). doi:10.3969/j.issn.1674−2184.2023.04.017

[41]

赵琳娜,慕秀香,马翠平,等. 2021.冬季稳定性降水相态预报研究进展[J].应用气象学报,32(1):12-24.

[42]

Zhao L N, Mu X X, Ma C P, et al. 2021. A review on stable precipitation type forecast in winter [J].Journal of Applied Meteorological Science,32(1):12-24 (in Chinese). doi:10.10.11898/1001−7313.20210102

[43]

周悦,吕晶晶,高正旭,等. 2024. 2024 年 2 月湖北省一次大范围冻雨过程的宏微观特征及形成机制初探[J].暴雨灾害,43(4):458-468.

[44]

Zhou Y, LV J J, Gao Z X, et al. 2024. Study on the macro and micro characteristics of a large-scale freezing rain weather event in Hubei Province [J].Torrential Rain and Disasters,43(4):458-468 (in Chinese). doi:10.12406/byzh.2024−131

[45]

Ahrens C D. 2000. Meteorology Today: An Introduction to Weather, Climate and the Environment [M]. America: Brooks/Cole:182-199

[46]

Ding B H, Yang K, Qin J, et al. 2014. The dependence of precipitation types on surface elevation and meteorological conditions and its parameterization [J].Journal of Hydrology,513:154-163. doi:10.1016/j.jhydrol.2014.03.038

[47]

ECMWF. 2016. IFS documentation Cy43R1 Part IV: physical processes[R]. Reading: ECMWF:118-120. doi:10.21957/sqvo5yxja

[48]

Knox J A, David S N, Knox P N. 2017. Two simple and accurate approximations for wet-bulb temperature in moist conditions, with forecasting applications [J].Bulletin of the American Meteorological Society,98(9):1897-1906. doi:10.1175/BAMS−D−16−0246.1

[49]

Poore K D, Wang J H, Rossow W B. 1995. Cloud layer thicknesses from a combination of surface and upper-air observations [J].Journal of Climate,8(3):550-568. doi:10.1175/1520−0442(1995)008<0550:CLTFAC>2.0.CO;2

[50]

Reeves H D, Elmore K L, Ryzhkov A, et al. 2014. Sources of uncertainty in precipitation-type forecasting [J].Weather Forecasting,29:936-953. doi:10.1175/WAF−D−14−00007.1

[51]

Stewart R E. 1992. Precipitation types in the transition region of winter storms [J].Bulletin of the American Meteorological Society,73:287-296. doi:10.1175/1520−0477(1992)073<0287:PTITTR>2.0.CO;2

[52]

Tamang S K, Ebtehaj A M, Prein A F, et al. 2020. Linking global changes of snowfall and wet-bulb temperature [J].Journal of Climate,33:39-59. doi:10.1175/JCLI−D−19−0254.1

[53]

Ye M S, Yao X P, Zhang T, et al. 2021. Intercomparison of CRA-Interim precipitation products with ERA5 and JRA-55 [J].Journal of Tropical Meteorology,27(2):136-147. doi:10.46267/j.1006−8775.2021.013

基金资助

中国气象局复盘总结专项(FPZJ2025-044)

AI Summary AI Mindmap
PDF (1329KB)

0

访问

0

被引

详细

导航
相关文章

AI思维导图

/

〈 〉