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POTENTIAL CHANGES IN THE JOINT PROBABILISTIC DESCRIPTION OF THE NORTH ATLANTIC WAVE CLIMATE

机译:北大西洋波状气候联合概率描述中的可能变化

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Climate changes include natural climate variability and anthropogenic climate change. The latter is leading to global warming and causes changes in metocean conditions. For most marine structures waves represent the dominant environmental load. Therefore, projections of changes of wave characteristics in the 21st century are crucial with respect to design and marine operations. The study investigates potential changes in simultaneous occurrence of significant wave height and spectral wave period in twelve North Atlantic locations by comparing the past and future wave climate. Two IPCC emission scenarios, with radiative forcing of 4.5 and 8.5 W/m~2 by the end of the 21st century, have been selected to project future wave conditions. The third generation (3G) wave model WAM with a resolution of 50 km is used to simulate waves. The model has been forced with winds obtained from six CMIP5 climate models for the historical period 1971-2000 and the future period 2071-2100 for the two emissions scenarios. Wave climate projections obtained from one climate model and one ensemble member are presented herein to indicate potential changes in extreme wave characteristics derived from the long-term joint probabilistic model of significant wave height and spectral wave period. Deviations between the past and future wave climate are shown, given attention to the shape of the joint distribution and wave steepness. Uncertainties associated with the presented results are discussed.
机译:气候变化包括自然气候变化和人为气候变化。后者导致全球变暖,并导致海洋状况发生变化。对于大多数海洋结构而言,波浪代表了主要的环境负荷。因此,对于21世纪的波浪特征变化的预测对于设计和海上作业至关重要。该研究通过比较过去和未来的海浪气候,调查了北大西洋十二个地点同时发生的重要波高和频谱波周期的潜在变化。选择了两种IPCC排放情景,以预测21世纪末辐射强迫为4.5和8.5 W / m〜2的情况。具有50 km分辨率的第三代(3G)波浪模型WAM用于模拟波浪。该模型是根据从1971-2000年历史时期和未来2071-2100年这两种排放情景的六个CMIP5气候模型获得的风强迫的。本文介绍了从一种气候模式和一个集合体获得的海浪气候预测,以指示极端海浪特征的潜在变化,这些极端海浪特征是从具有重要波高和频谱波周期的长期联合概率模型得出的。显示了过去和未来波浪气候之间的差异,并注意了联合分布的形状和波浪陡度。讨论了与提出的结果相关的不确定性。

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