Impact of Assimilating Radar Solid Precipitation Data in the Canadian Precipitation Analysis System

Author:

Beaudry Florence L.1,Bélair Stéphane2,Thériault Julie M.1,Khedhaouiria Dikra2,Lespinas Franck3,Michelson Daniel4,Feng Pei-Ning1,Aubry Catherine1

Affiliation:

1. a Centre ESCR, Department of Earth and Atmospheric Sciences, Université du Québec À Montréal, Montréal, Québec, Canada

2. b Atmospheric Science and Technology, Environment and Climate Change Canada, Dorval, Québec, Canada

3. c Canadian Centre for Meteorological and Environmental Prediction, Environment and Climate Change Canada, Dorval, Québec, Canada

4. d Meteorological Research Division, Environment and Climate Change Canada, Toronto, Ontario, Canada

Abstract

Abstract The Canadian Precipitation Analysis (CaPA) system provides near-real-time precipitation analyses over Canada by combining observations with short-term numerical weather prediction forecasts. CaPA’s snowfall estimates suffer from the lack of accurate solid precipitation measurements to correct the first-guess estimate. Weather radars have the potential to add precipitation measurements to CaPA in all seasons but are not assimilated in winter due to radar snowfall estimate imprecision and lack of precipitation gauges for calibration. The main objective of this study is to assess the impact of assimilating Canadian dual-polarized radar-based snowfall data in CaPA to improve precipitation estimates. Two sets of experiments were conducted to evaluate the impact of including radar snowfall retrievals, one set using the high-resolution CaPA (HRDPA) with the currently operational quality control configuration and another increasing the number of assimilated surface observations by relaxing quality control. Experiments spanned two winter seasons (2021 and 2022) in central Canada, covering part of the entire CaPA domain. The results showed that the assimilation of radar-based snowfall data improved CaPA’s precipitation estimates 81.75% of the time for 0.5-mm precipitation thresholds. An increase in the probability of detection together with a decrease in the false alarm ratio suggested an improvement of the precipitation spatial distribution and estimation accuracy. Additionally, the results showed improvements for both precipitation mass and frequency biases for low precipitation amounts. For larger thresholds, the frequency bias was degraded. The results also indicated that the assimilation of dual-polarization radar data is beneficial for the two CaPA configurations tested in this study.

Funder

Manitoba Hydro

Mitacs

Publisher

American Meteorological Society

Reference67 articles.

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