Impact of adjusted and non-adjusted surface observations on the cold season performance of the Canadian Precipitation Analysis (CaPA) System

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Pei-Ning Feng, Stéphane Bélair, Dikraa Khedhaouiria, Franck Lespinas, Eva Mekis, Julie M. Thériault
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引用次数: 0

Abstract

Abstract The Canadian Precipitation Analysis System (CaPA) is an operational system that uses a combination of weather gauge and ground-based radar measurements together with short-term forecasts from a numerical weather model to provide near-real-time estimates of 6 and 24-hour precipitation amounts. During the winter season, many gauge measurements are rejected by the CaPA quality control process due to the wind-induced undercatch for solid precipitation. The goal of this study is to improve the precipitation estimates over central Canada during the winter seasons from 2019 to 2022. Two approaches were tested. First, the quality control procedure in CaPA has been relaxed to increase the number of surface observations assimilated. Second, the automatic solid precipitation measurements were adjusted using a universal transfer function to compensate for the undercatch problem. Although increasing the wind speed threshold resulted in lower amounts and worse biases in frequency, the overall precipitation estimates is improved as the equitable threat score is improved due to a substantial decrease in the false alarm ratio, which compensates the degradation of the probability of detection. The increase of solid precipitation amounts using a transfer function improves the biases in both frequency and amounts, and the probability of detection for all precipitation thresholds. However, the false alarm ratio deteriorates for large thresholds. The statistics varies from year to year, but an overall improvement is demonstrated by increasing the number of stations and adjusting the solid precipitation amounts for wind speed undercatch.
调整和非调整的地面观测对加拿大降水分析系统(CaPA)冷季性能的影响
加拿大降水分析系统(CaPA)是一个业务系统,它结合了天气测量仪和地面雷达测量,以及数值天气模式的短期预报,提供近实时的6和24小时降水量估计。在冬季,由于风引起的固体降水捕获不足,许多测量结果在CaPA质量控制过程中被拒绝。本研究的目的是改善2019年至2022年冬季加拿大中部的降水估计。测试了两种方法。首先,放宽了CaPA的质量控制程序,增加了表面观测的同化数量。其次,使用通用传递函数对自动固体降水测量进行调整,以补偿欠捕获问题。虽然增加风速阈值会导致数量减少和频率偏差加剧,但由于虚警率的大幅降低,公平威胁评分得到了提高,从而补偿了检测概率的下降,因此总体降水估计得到了改善。使用传递函数增加固体降水量可以改善频率和数量上的偏差,以及所有降水阈值的检测概率。但是,当阈值较大时,虚警率会下降。每年的统计数据有所不同,但通过增加台站数量和根据风速调整固体降水量,总体上有所改善。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Hydrometeorology
Journal of Hydrometeorology 地学-气象与大气科学
CiteScore
7.40
自引率
5.30%
发文量
116
审稿时长
4-8 weeks
期刊介绍: The Journal of Hydrometeorology (JHM) (ISSN: 1525-755X; eISSN: 1525-7541) publishes research on modeling, observing, and forecasting processes related to fluxes and storage of water and energy, including interactions with the boundary layer and lower atmosphere, and processes related to precipitation, radiation, and other meteorological inputs.
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