Uncertainty in 100 and 10,000 Year Ice Loads on Offshore Structures

R. McKenna, Mark Fuglem, G. Crocker
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Abstract

The ISO 19906 arctic structures standard specifies that ice loads be calculated at the extreme level (100 year return period) for verifying ultimate limit states and at the abnormal level (10,000 years) for accidental/abnormal limit states. Since ice load measurements on structures have only been made over much shorter time periods, concerns are often expressed about the accuracy to which 10,000 year values can be estimated. In this paper, the uncertainties in 100 and 10,000 year loads are considered through examples based on experience with calculations of loads on structures in different iceberg and sea ice environments. For icebergs, it is necessary to consider the size distribution of icebergs (including the potential presence of extremely large icebergs and ice islands) as well as drift velocities and shapes that can govern high return- period loads for fixed structures. With sea ice, abnormal-level loads can be governed either by the presence and geometrical properties of large discrete features (e.g. first-year ridges and stamukhi, or in the arctic, multi-year floes with thick ridges), or by very thick ice as a result of thermal growth. It is demonstrated how errors in key contributing ice parameters can influence extreme-level loads, and the relationship between level/rafted ice loads at the abnormal level and the factored (1.35) extreme-level values, and how these uncertainties might be considered in the design process.
海洋结构上100年和10000年冰荷载的不确定性
ISO 19906北极结构标准规定,在极端水平(100年回复期)计算冰荷载,以验证最终极限状态,在异常水平(10,000年)计算意外/异常极限状态。由于对结构的冰荷载的测量只在较短的时间内进行,因此人们经常对一万年值的估计精度表示关注。本文根据不同冰山和海冰环境下结构的荷载计算经验,通过实例考虑了100年和10000年荷载的不确定性。对于冰山,有必要考虑冰山的大小分布(包括可能存在的极大的冰山和冰岛)以及漂移速度和形状,它们可以控制固定结构的高返回周期载荷。对于海冰,异常水平的负荷可以由大型离散特征的存在和几何特性来控制(例如,第一年的脊和stamukhi,或者在北极,具有厚脊的多年浮冰),或者由于热生长而产生的非常厚的冰。演示了关键贡献冰参数的误差如何影响极端水平荷载,以及异常水平/漂流冰荷载与因子(1.35)极端水平值之间的关系,以及如何在设计过程中考虑这些不确定性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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