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A comparison of simulated and measured lake ice thickness using a Shallow Water Ice Profiler

机译:使用浅水冰探究器模拟和测量湖冰厚的比较

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In northern regions where observational data is sparse, lake ice models are ideal tools as they can provide valuable informationon ice cover regimes. The Canadian Lake Ice Model was used to simulate ice cover for a lake near Churchill, Manitoba,Canada throughout the 2008/2009 and 2009/2010 ice covered seasons. To validate and improve the model results, in situmeasurements of the ice cover through both seasons were obtained using an upward-looking sonar device Shallow Water IceProfiler (SWIP) installed on the bottom of the lake. The SWIP identified the ice-on/off dates as well as collected ice thicknessmeasurements. In addition, a digital camera was installed on shore to capture images of the ice cover through the seasonsand field measurements were obtained of snow depth on the ice, and both the thickness of snow ice (if present) and total icecover. Altering the amounts of snow cover on the ice surface to represent potential snow redistribution affected simulatedfreeze-up dates by a maximum of 22 days and break-up dates by a maximum of 12 days, highlighting the importance ofaccurately representing the snowpack for lake ice modelling. The late season ice thickness tended to be under estimated bythe simulations with break-up occurring too early, however, the evolution of the ice cover was simulated to fall between therange of the full snow and no snow scenario, with the thickness being dependant on the amount of snow cover on the icesurface. Copyright  2011 John Wiley & Sons, Ltd.
机译:在观测数据稀疏的北部地区,冰冰型是理想的工具,它们可以提供有价值的信息在冰盖制度。加拿大湖冰型模型用于模拟南部丘吉尔(Manitoba)附近的湖泊的冰盖,加拿大在2008/2009和2009/2010冰盖的季节。验证和改进模型结果,原位通过向上看起来的声纳设备浅水冰获得通过两个季节的冰盖的测量分析器(Swip)安装在湖底。 SWIP确定了冰/关日期以及收集的冰厚度测量。此外,岸上安装了一种数码相机,以通过季节捕获冰盖的图像在冰上获得了雪冰的雪深,雪冰(如果存在)和总冰的厚度覆盖。改变冰面上的雪覆盖量,以表示受影响的潜在雪再分配冻结日期最多22天,分手日期最多12天,突出了重要性准确地代表湖冰造型的积雪。晚期冰厚度趋于估计分解的模拟太早,然而,模拟了冰盖的演变以落在全雪和没有积雪场景的范围,厚度依赖于冰上的雪覆盖量表面。版权所有2011 John Wiley&Sons,Ltd。

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