TY - JOUR
T1 - Sensitivity of Hail Precipitation to Ensembles of Uncertainties of Representative Initial Environmental Conditions From ECMWF
AU - Li, Xiaofei
AU - Zhang, Fuqing
AU - Zhang, Qinghong
AU - Kumjian, Matthew R.
N1 - Funding Information:
This study was supported by the National Natural Science Foundation of China (Grants 41330421 and 41875052). We thank Yue (Michael) Ying for pro viding some of the necessary perturba tion data and for making suggestions regarding the figures. We thank the ECMWF for supplying the ensemble initial perturbation data. The work was carried out at National Supercomputer Center in Tianjin in China, and the calculations were performed on TianHe‐1 (A). The authors thank the editor and anonymous reviewers, whose valuable comments and sugges tions significantly improved this article. The data used in this manuscript are available on the website https://pan. baidu.com/s/19Pl5BztO_ nLB5F7XHYKqjw.
Funding Information:
This study was supported by the National Natural Science Foundation of China (Grants 41330421 and 41875052). We thank Yue (Michael) Ying for providing some of the necessary perturbation data and for making suggestions regarding the figures. We thank the ECMWF for supplying the ensemble initial perturbation data. The work was carried out at National Supercomputer Center in Tianjin in China, and the calculations were performed on TianHe-1 (A). The authors thank the editor and anonymous reviewers, whose valuable comments and suggestions significantly improved this article. The data used in this manuscript are available on the website https://pan.baidu.com/s/19Pl5BztO_nLB5F7XHYKqjw.
Publisher Copyright:
©2019. American Geophysical Union. All Rights Reserved.
PY - 2019/7/16
Y1 - 2019/7/16
N2 - The sensitivity of hail precipitation from an idealized hailstorm to realistic environmental uncertainties was investigated through ensembles of cloud-resolving simulations using the Weather Research and Forecasting model, with initial condition perturbations derived from the European Centre for Medium-Range Weather Forecasting (ECMWF) operational ensemble. The analyses revealed that hail precipitation rate was very sensitive to small initial environmental perturbations, particularly in thermodynamic variables. The hail precipitation rate was significantly positively correlated with perturbations to the initial potential temperature below 750 hPa and to water vapor mixing ratio above 750 hPa. These small initial perturbations led to subsequent substantial differences in hail precipitation as well as in characteristics of the parent storm (e.g., updraft velocity, diabatic heating, and microphysical processes), all of which play a key role in hail growth. The larger sensitivity of hail precipitation to thermodynamic rather than kinematic environmental initial condition perturbations persisted even when the magnitude of the perturbations was reduced to 10% of the realistic uncertainties derived from the ECMWF ensemble. In the ensemble with reduced-amplitude initial perturbations, there was still a moderately strong positive correlation between hail precipitation rate and the initial perturbations of the thermodynamic variables. However, these sensitivities were nonlinear, suggesting that the intrinsic predictability of hail precipitation rate may be limited, even when environmental uncertainties are reduced to 10%, 1.0 × 10−3, and 1.0 × 10−5 of the currently realistic magnitude of initial condition uncertainty.
AB - The sensitivity of hail precipitation from an idealized hailstorm to realistic environmental uncertainties was investigated through ensembles of cloud-resolving simulations using the Weather Research and Forecasting model, with initial condition perturbations derived from the European Centre for Medium-Range Weather Forecasting (ECMWF) operational ensemble. The analyses revealed that hail precipitation rate was very sensitive to small initial environmental perturbations, particularly in thermodynamic variables. The hail precipitation rate was significantly positively correlated with perturbations to the initial potential temperature below 750 hPa and to water vapor mixing ratio above 750 hPa. These small initial perturbations led to subsequent substantial differences in hail precipitation as well as in characteristics of the parent storm (e.g., updraft velocity, diabatic heating, and microphysical processes), all of which play a key role in hail growth. The larger sensitivity of hail precipitation to thermodynamic rather than kinematic environmental initial condition perturbations persisted even when the magnitude of the perturbations was reduced to 10% of the realistic uncertainties derived from the ECMWF ensemble. In the ensemble with reduced-amplitude initial perturbations, there was still a moderately strong positive correlation between hail precipitation rate and the initial perturbations of the thermodynamic variables. However, these sensitivities were nonlinear, suggesting that the intrinsic predictability of hail precipitation rate may be limited, even when environmental uncertainties are reduced to 10%, 1.0 × 10−3, and 1.0 × 10−5 of the currently realistic magnitude of initial condition uncertainty.
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U2 - 10.1029/2018JD029899
DO - 10.1029/2018JD029899
M3 - Article
AN - SCOPUS:85068609580
SN - 2169-897X
VL - 124
SP - 6929
EP - 6948
JO - Journal of Geophysical Research: Atmospheres
JF - Journal of Geophysical Research: Atmospheres
IS - 13
ER -