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Modeling bulk density and snow water equivalent using daily snow depth observations

机译:使用每日雪深观测值对堆密度和雪水当量进行建模

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Bulk density is a fundamental property of snow relating its depth and mass.Previously, two simple models of bulk density (depending on snow depth,date, and location) have been developed to convert snow depth observationsto snow water equivalent (SWE) estimates. However, these models were notintended for application at the daily time step. We develop a new model ofbulk density for the daily time step and demonstrate its improved skill overthe existing models.Snow depth and density are negatively correlated at short (10 days)timescales while positively correlated at longer (90 days) timescales. Weseparate these scales of variability by modeling smoothed, daily snow depth(long timescales) and the observed positive and negative anomalies from thesmoothed time series (short timescales) as separate terms. A climatology offit is also included as a predictor variable.Over half a million daily observations of depth and SWE at 345 snowpack telemetry (SNOTEL) sitesare used to fit models and evaluate their performance. For each location, wetrain the three models to the neighboring stations within 70 km, transfer theparameters to the location to be modeled, and evaluate modeled time seriesagainst the observations at that site. Our model exhibits improvedstatistics and qualitatively more-realistic behavior at the daily time stepwhen sufficient local training data are available. We reduce density root mean square error (RMSE) by9.9 and 4.5% compared to previous models while increasing R2from 0.46 to 0.52 to 0.56 across models. Focusing on the 21-day window aroundpeak SWE in each water year, our model reduces density RMSE by 24 and17.4% relative to the previous models, with R2 increasing from 0.55to 0.58 to 0.71 across models. Removing the challenge of parameter transferover the full observational record increases R2 scores for both theexisting and new models, but the gain is greatest for the new model (R2 = 0.75). Our model shows general improvement over existing models when dataare more frequent than once every 5 days and at least 3 stations areavailable for training.
机译:堆积密度是积雪与深度和质量相关的基本属性。以前,已经开发了两个简单的堆积密度模型(取决于积雪深度,日期和位置),以将积雪深度观测值转换为雪水当量(SWE)估计值。但是,这些模型并非打算在每天的时间步骤中应用。我们为每天的时间步长开发了一个新的体积密度模型,并证明了其在现有模型上的改进技巧。 雪深和密度在短(10天)时间尺度上呈负相关,而在更长(90天)时间尺度上呈正相关。时间尺度。通过将平滑的每日降雪深度(较长的时间尺度)和从平滑的时间序列(较短的时间尺度)中观察到的正负异常建模为单独的术语,将这些可变性尺度分开。还包括适合的气候学作为预测变量。 每天在345个雪堆遥测(SNOTEL)站点上对深度和SWE进行每天超过一百万次的观测,以拟合模型并评估其性能。对于每个位置,我们将这三个模型训练到70公里以内的相邻站点,将参数转移到要建模的位置,然后针对该站点的观测值评估建模的时间序列。当有足够的本地训练数据可用时,我们的模型将在每天的时间步上显示出改进的统计量和定性更真实的行为。与以前的模型相比,我们将密度的均方根误差(RMSE)降低了9.9%和4.5%,而整个模型中的 R 2 从0.46增至0.52到0.56。着眼于每个水年峰值SWE的21天窗,我们的模型相对于以前的模型将密度RMSE降低了24和17.4%,其中 R 2 从跨模型介于0.55至0.58至0.71之间。消除参数转移对整个观测记录的挑战,现有模型和新模型均会增加 R 2 得分,但新模型的收益最大( R < / i> 2 = 0.75)。当数据每5天超过一次且至少有3个站点可供训练时,我们的模型显示出对现有模型的总体改进。

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