Assimilation impact of high‐temporal‐resolution volume scans on quantitative precipitation forecasts in a severe storm: Evidence from nudging data assimilation experiments with a thermodynamic retrieval method
Assimilation impact of high‐temporal‐resolution volume scans on quantitative precipitation forecasts in a severe storm: Evidence from nudging data assimilation experiments with a thermodynamic retrieval method
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高时间分辨率体积扫描对强风暴定量降水预报的同化影响:热力学检索方法推动数据同化实验的证据
DOI:
10.1002/qj.3548
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发表时间:
2019
期刊:
影响因子:
--
通讯作者:
S. Suzuki
中科院分区:
文献类型:
--
作者:
S. Shimizu;K. Iwanami and R. Kato; N. Sakurai; T. Maesaka; K. Kieda; Y. Shusse; S. Suzuki
The assimilation impact of high‐temporal volume scan data (1 min) on very‐short‐range (within 1 h) quantitative precipitation forecasts (QPFs) of a severe storm was investigated using a nudging data assimilation method. This study investigated (a) the assimilation impact of two observational parameters (potential temperature, retrieved using a traditional technique and pseudo‐water vapour, obtained from reflectivity observations), (b) the sensitivity to the temporal resolution of three‐dimensional radar observations, and (c) the assimilation method (re‐initialization at a single time or sequential nudging over 20 min), regarding the predictability of a tornadic storm observed on 2 September 2013 around Koshigaya City, Japan. Our results indicate that (a) data assimilation of both pseudo‐water vapour and potential temperature perturbation demonstrated the highest contribution for up to the first 30 min of the evaluation period (50 min in total), (b) finer temporal resolution provided a better forecast overall, and (c) a nudging scheme provided a better forecast in the first 30 min. Our results showed better predictability than traditional extrapolation‐based nowcasts in the latter 40 min of the evaluation period. The data assimilation with water vapour and potential temperature, determined from a 1 min volume scan, therefore has the potential to extend the cloud‐scale predictability in strong rainfall intensity situations (>20 mm/h) of very‐short‐range QPFs (within 30 min).