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作 者:Rong ZHANG Wenjuan ZHANG Yijun ZHANG Jianing FENG Liangtao XU
机构地区:[1]State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,China Meteorological Administration(CMA),Beijing 100081 [2]Key Laboratory for Cloud Physics of CMA,Chinese Academy of Meteorological Sciences,CMA,Beijing 100081 [3]Department of Atmospheric and Oceanic Sciences&Institute of Atmospheric Sciences,Fudan University,Shanghai 200438
出 处:《Journal of Meteorological Research》2020年第5期1052-1067,共16页气象学报(英文版)
基 金:Supported by the National Key Research and Development Program of China(2019YFC1510103);Basic Research Fund of the Chinese Academy of Meteorological Sciences(2019Y003)。
摘 要:Previous observations from World Wide Lightning Location Network(WWLLN) and satellites have shown that typhoon-related lightning data have a potential to improve the forecast of typhoon intensity. The current study was aimed at investigating whether assimilating TC lightning data in numerical models can play such a role. For the case of Super Typhoon Haiyan in 2013, the lightning data assimilation(LDA) was realized in the Weather Research and Forecasting(WRF) model, and the impact of LDA on numerical prediction of Haiyan’s intensity was evaluated.Lightning data from WWLLN were used to adjust the model’s relative humidity(RH) based on the method developed by Dixon et al.(2016). The adjusted RH was output as a pseudo sounding observation, which was then assimilated into the WRF system by using the three-dimensional variational(3DVAR) method in the cycling mode at 1-h intervals. Sensitivity experiments showed that, for Super Typhoon Haiyan(2013), which was characterized by a high proportion of the inner-core(within 100 km from the typhoon center) lightning, assimilation of the inner-core lightning data significantly improved its intensity forecast, while assimilation of the lightning data in the rainbands(100–500 km from the typhoon center) led to no obvious improvement. The improvement became more evident with the increase in LDA cycles, and at least three or four LDA cycles were needed to achieve obvious intensity forecast improvement. Overall, the improvement in the intensity forecast by assimilation of the inner-core lightning data could be maintained for about 48 h. However, it should be noted that the LDA method in this study may have a negative effect when the simulated typhoon is stronger than the observed, since the LDA method cannot suppress the spurious convection.
关 键 词:LIGHTNING three-dimensional variational(3DVAR)data assimilation Typhoon Haiyan typhoon intensity
分 类 号:P456.7[天文地球—大气科学及气象学]
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