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Modelling the dynamics of snow cover, soil frost and surface\ud ice in Norwegian grasslands

机译:模拟积雪,土壤霜冻和表面的动态 冰在挪威草原

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摘要

Studying the winter survival of forage grasses under a changing climate requires models that can simulate the dynamics of soil conditions at low temperatures. We developed a simple model that simulates depth of snow\udcover, the lower frost boundary of the soil and the freezing of surface puddles. We calibrated the model against independent data from four locations in Norway, capturing climatic variation from south to north (Arctic) and from coastal to inland areas. We parameterized the model by means of Bayesian calibration, and identified the least important model parameters using the sensitivity analysis method of Morris. Verification of the model suggests that the results are reasonable. Because of the simple model structure, some overestimation occurs in snow and frost depth. Both the calibration and the sensitivity analysis suggested that the snow cover module could be simplified with respect to snowmelt and liquid water content. The soil frost module should be kept unchanged, whereas the surface ice module should be changed when more detailed topographical data become available, such as better estimates of the fraction of the land area where puddles may form.
机译:在气候变化的情况下研究草料的冬季生存期需要能够模拟低温土壤状况动态的模型。我们开发了一个简单的模型,该模型可以模拟积雪\覆盖层的深度,土壤的较低霜冻边界以及表面水坑的冻结。我们根据来自挪威四个地点的独立数据对模型进行了校准,捕获了从南到北(北极)以及从沿海到内陆地区的气候变化。我们通过贝叶斯校准对模型进行参数化,并使用Morris的灵敏度分析方法确定了最不重要的模型参数。模型的验证表明结果是合理的。由于模型结构简单,因此在雪和霜冻深度中有些高估。校准和灵敏度分析均表明,就融雪和液态水含量而言,可以简化积雪模块。土壤霜冻模块应保持不变,而当可获得更详细的地形数据(例如,更好地估计可能形成水坑的土地面积的比例)时,应更改地表冰模块。

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