风暴潮增水长期模拟结果的订正方法研究  

Study of the correction method on long-term simulations of storm surge elevation

作　　者：马永锋[1,2] 祖子清 李涛[1,2] 吴少华[1,2] 凌铁军[1,2] 

机构地区：[1]国家海洋局海洋灾害预报技术研究重点实验室,北京100081 [2]国家海洋环境预报中心,北京100081

出　　处：《海洋预报》2015年第5期35-44,共10页Marine Forecasts

基　　金："十二五"国家科技支撑计划项目(2012BAC19B08);国家海洋局海洋公益性行业科研专项(201105018)

摘　　要：利用7个验潮站逐时观测数据与国家海洋环境预报中心业务化风暴潮模式结果进行对比分析,分别采用趋势订正(TSC法)和统计偏差订正(SBC法)两种方法对模拟的风暴潮增水长时间序列进行订正,以提高模拟结果的可靠性。研究结果表明:模拟的风暴潮较观测频次明显偏多且强度偏强,2008—2011年期间模拟的7个站点发生50 cm以上风暴潮的年平均总频次较观测高估238%,且年最大增水值的年平均较观测偏高28.7—104.7 cm。经过TSC和SBC两种方法订正后,其误差显著性减小,年平均总频次分别较观测(226.5次)偏少2%和47%,年最大增水值的年平均偏差分别在-9.8—17.3 cm和-23.7—4.3 cm之间。另外,TSC方法订正后的风暴潮频次和最大增水在数值上较SBC方法更接近于观测,而SBC方法订正后的风暴潮频次、最大增水的季节变化趋势与观测更为一致,其与观测的相关系数在一些站点由订正前的0.2左右提升到0.8以上。Based on the hourly observations at the 7 tidal gauges, the modeled results from National Marine Environmental Forecasting Center operational storm surge model is analyzed, and the simulated longtime series storm surge elevation is corrected by using trend correction（TSC） and statistical bias correction（SBC） method in order to improve the reliability of simulations. The results show that the frequency/intensity of simulated storm surge is obviously more/stronger than observations. The number of annual mean storm surge occurrence of the total 7 sites derived from simulations is 238 % more than observations, with the annual mean maximum storm surge elevation about 28.7-104.7 cm higher than observations. After TSC and SBC correction, the annual mean total frequency at the 7 sites are 2% and 47% less than observations（226.5 times）, respectively, and the mean biases of annual maximum storm surge elevation are range in-9.8-17.3 cm and-23.7-4.3 cm. It shows that the biases between simulation and observation have significantly reduced. Numerically, the frequencies and maximum values of storm surge derived from TSC correction are more matched with the observations than that derived from SBC correction. The seasonal variation of frequencies and maximum surges derived from SBC correction are more consistent with observations, its relative coefficients increased to 〉0.8 from ~0.2 before correction at some sites.

关 键 词：风暴潮 数值模拟 趋势订正 统计偏差订正 

分 类 号：P731.23[天文地球—海洋科学]