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Wetting and Drying of Soil: From Data to Understandable Models for Prediction

机译:土壤的湿润和干燥:从数据到可理解的预测模型

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摘要

Soil moisture is critical to agriculture, ecology, and certain natural disasters. Existing soil moisture models often fail to predict soil moisture accurately for time periods greater than a few hours. To tackle this problem, we introduce in this paper two novel models, the Naive Accumulative Representation (NAR) and the Additive Exponential Accumulative Representation (AEAR). The parameters in these models reflect hydrological redistribution processes of gravity and suction. We validate our models using soil moisture and rainfall time series data collected from a steep gradient post-wildfire site in Southern California. Data analysis is challenging, since rapid landscape change in steep, burned hillslopes is typically observed in response to even small to moderate rain events. We found that the AEAR model fits the data well for three distinct soil textures at different depths below the ground surface (at 5cm, 15cm, and 30cm). Similar strong results are demonstrated in controlled soil moisture experiments. Our recommended AEAR model has been validated as effective and useful by earth scientists, giving better forecasts than existing models for time horizons of 10 to 24 hours.
机译:土壤水分对于农业,生态和某些自然灾害至关重要。现有的土壤水分模型通常无法在数小时以上的时间内准确预测土壤水分。为了解决这个问题,我们在本文中介绍了两个新颖的模型,即朴素的累积表示(NAR)和加性指数累积表示(AEAR)。这些模型中的参数反映了重力和吸力的水文重新分配过程。我们使用从南加州的陡坡野火场采集的土壤水分和降雨时间序列数据来验证我们的模型。数据分析具有挑战性,因为通常观察到陡峭,燃烧的山坡上的景观快速变化,以响应甚至小到中度的降雨事件。我们发现,AEAR模型在地面以下不同深度(分别为5cm,15cm和30cm)的三个不同土壤质地的数据非常吻合。在受控的土壤水分实验中也证明了类似的结果。我们推荐的AEAR模型已被地球科学家验证为有效和有用,对于10到24小时的时间范围,比现有模型可提供更好的预测。

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