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Validation of a thirty year wave hindcast using the Climate Forecast System Reanalysis winds

机译:使用气候预测系统再分析风验证三十年后浪

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A thirty one year wave hindcast (1979-2009) using NCEP's latest high resolution Climate Forecast System Reanalysis (CFSR) wind and ice database has been developed and is presented here. The hindcast has been generated using the third generation wind wave model WAVEWATCH III? with a mosaic of 16 two-way nested grids. The resolution of the grids ranged from 1/2° to 1/15°. Validation results for bulk significant wave height H s and 10m (above Mean Sea Level) wind speeds U10 have been presented using both altimeter records and NDBC buoys. In general the database does a good job of representing the wave climate. At most buoys there is excellent agreement between model and data out to the 99.9th percentile. The agreement at coastal buoys is not as good as the offshore buoys due to unresolved coastal features (topographic/bathymetric) as well as issues related to interpolating wind fields at the land-sea margins. There are some concerns about the wave climate in the Southern Hemisphere due to the over prediction of winds (early part of the database) as well as the lack of wave blocking due to icebergs (in the model).
机译:利用NCEP最新的高分辨率气候预报系统再分析(CFSR)风冰数据库,开发了一个三十年海浪预报(1979-2009),并在此处进行了介绍。后播是使用第三代风波模型WAVEWATCH III生成的?带有16个双向嵌套网格的马赛克。网格的分辨率范围为1/2°至1/15°。使用高度计记录和NDBC浮标都已经给出了大体有效波高Hs和10m(高于平均海平面)风速U10的验证结果。通常,数据库在表示波浪气候方面做得很好。在大多数浮标上,模型和数据之间的一致性非常好,达到第99.9个百分位。沿海浮标的协议不如海上浮标好,这是因为沿海特征尚未解决(地形/测深)以及与陆海边界处的风场插值有关的问题。由于对风的过度预测(数据库的早期部分)以及由于冰山造成的波浪阻塞(模型中)的缺乏,对南半球的波浪气候存在一些担忧。

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