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首页> 外文期刊>Journal of Advances in Modeling Earth Systems >The impact of radiosonde data on forecasting sea?¢????ice distribution along the Northern Sea Route during an extremely developed cyclone
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The impact of radiosonde data on forecasting sea?¢????ice distribution along the Northern Sea Route during an extremely developed cyclone

机译:在极度发达的气旋中,探空仪数据对预测北冰洋沿线海冰分布的影响

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To investigate the impact of radiosonde data on the sea?¢????ice forecast in the Northern Sea Route during an extremely developed cyclone on 6 August 2012, a series of numerical experiments were conducted using an ice?¢????ocean coupled model with fine horizontal resolution (approximately 2.5 km). The atmospheric forcing data used for the model were forecast data with (CTL) and without (OSE) initialization by radiosonde data over the Fram Strait, obtained by the German R/V Polarstern , and the European Centre for Medium?¢????Range Weather Forecasts Interim reanalysis data. All numerical experiments were run from 06:00 UTC on 3 August 2012 to 00:00 UTC on 8 August 2012 with an initial sea?¢????ice concentration and thickness derived from the Advanced Microwave Scanning Radiometer 2 satellite data. The root?¢????mean?¢????square error and correlation coefficient for the sea?¢????ice distribution showed that the CTL simulation predicted better the sea?¢????ice distribution in the Northern Sea Route than the OSE simulation. This occurred in particular from 6 to 7 August when the cyclone became strong. The thermodynamic processes resulted in the difference in the sea?¢????ice thickness due to changes in the vertical energy fluxes. However, the differences in the sea?¢????ice concentration and velocity were caused mainly by the dynamics, particularly the difference in wind fields, rather than the thermodynamics. These results suggest that radiosonde data are effective in improving the forecast accuracy of the sea?¢????ice distribution. Therefore, errors in the weather forecast data would have a substantial impact on the safety of ship navigation and the sea?¢????ice distribution.
机译:为了调查无线电探空仪数据对2012年8月6日极度发达的气旋期间北海航线冰预报的影响,我们使用了冰海进行了一系列数值实验。精细水平分辨率(约2.5 km)的耦合模型。用于该模型的大气强迫数据是由德国R / V Polarstern和欧洲中型中心获得的Fram海峡上的探空仪数据,带(CTL)且没有(OSE)初始化的天气预报数据。范围天气预报中期再分析数据。所有数值实验都是从2012年8月3日世界标准时间06:00到2012年8月8日世界标准时间00:00进行的,初始冰浓度和厚度是从高级微波扫描辐射计2卫星数据中得出的。根冰分布的均方根和相关系数的平方根和均方根表明,CTL模拟能更好地预测海中冰的分布。北海航线比OSE模拟。这尤其是在8月6日至7日旋风变强时发生。由于垂直能量通量的变化,热力学过程导致海冰厚度的差异。但是,海冰浓度和速度的差异主要是由动力学引起的,尤其是风场的差异,而不是由热力学引起的。这些结果表明,探空仪数据在提高海冰分布预测准确性方面是有效的。因此,天气预报数据中的错误将对船舶航行和海上冰的安全性产生重大影响。

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