Past and future wave climate in the Baltic Sea produced by the SWAN model with forcing from the regional climate model RCA of the Rossby Centre

E. Kriezi, B. Broman
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引用次数: 21

Abstract

A hindcast wave database and a wave database based on future climate scenarios for the Baltic Sea, Kattegat and Skagerrak is under development. The wind force used for the wave simulation is coming form the RCA model and the future wind from RCA is based on global climate model ECHAM4 for one emission scenario (IPCC SRES A2). The phase averaged spectral model SWAN (Simulated WAves Nearshore) model is used for simulating the wave field. The model is driven by atmospheric forcing and it simulates waves generated by the wind and their propagation both in deep water and near shore areas. When realistic winds are provided the model has an outstanding performance. Winds from the Mesan reanalysis and the RCA model were used as forcing for the SWAN model simulating short hindcast storms for the validation of the wave model in connection with the winds. RCA results appeared to underestimate extreme winds. A correction was introduced which used an empirical relation between 3-second gust and the wind velocity. The model data were compared with observational data. Statistical parameters like scatter index, bias and symmetric slope were used to judge the quality of the data. The performance of the wave model with Mesan is very good. Model and observed data appear to have a good correlation. The performance with RCA is worse and it underestimates the wave height during extreme wind events. The performance when using corrected RCA winds is improved and data give better statistical values when they are compared with observations. The reason for using RCA forcing was the length of RCA data, 40 years of hindcast, and the 50 years of future winds based on global climate scenarios. The corrected coefficient was applied to the RCA and used to force SWAN. Only one year of hindcast has been performed initially while the 40 year run is planned to be performed in the near future. Moreover, a run based on future scenario has been performed. Six month is 1970 were run as control period and 6 months in 2020 as a future projection, giving insight to some of the possible changes in the future wave climate. Thirty years of control run and thirty years of future projection are in progress.
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在罗斯比中心区域气候模式RCA的强迫下,SWAN模式产生的波罗的海过去和未来的波浪气候
一个后向海浪数据库和一个基于波罗的海、卡特加特和斯卡格拉克未来气候情景的海浪数据库正在开发中。用于波浪模拟的风力来自RCA模式,RCA的未来风基于全球气候模式ECHAM4的一种排放情景(IPCC SRES A2)。采用相位平均谱模型SWAN (simulation WAves Nearshore)模型模拟波浪场。该模式是由大气强迫驱动的,它模拟了由风产生的波浪及其在深水和近岸地区的传播。当提供真实风时,模型具有出色的性能。来自Mesan再分析和RCA模式的风被用作模拟短后抛风暴的SWAN模式的强迫,以验证与风有关的波浪模式。RCA的结果似乎低估了极端风。利用3秒阵风与风速之间的经验关系进行了修正。将模型资料与观测资料进行比较。利用散点指数、偏置和对称斜率等统计参数来判断数据的质量。采用介子模型的波动模型具有很好的性能。模型和观测数据似乎有很好的相关性。RCA的性能较差,并且在极端风事件中低估了波高。当使用校正后的RCA风时,性能得到了改善,数据与观测值相比具有更好的统计值。使用RCA强迫的原因是RCA数据的长度、40年的后验和50年基于全球气候情景的未来风。将修正后的系数应用于RCA,并用于强制SWAN。最初只进行了一年的预测,而计划在不久的将来进行40年的预测。此外,还执行了基于未来场景的运行。1970年的6个月作为对照期,2020年的6个月作为未来的预测,从而对未来波浪气候的一些可能变化有所了解。三十年的控制运行和三十年的未来预测正在进行中。
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