太阳能的概率预测

J. Boland
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引用次数: 0

摘要

本文介绍了美国西雅图地区15分钟水平面太阳辐照量的预报,以及澳大利亚布罗肯希尔地区15分钟太阳风量的预报。目标是在预测上设置误差界限,特别是估计15个分位数,从本质上最小到m最大值。在实际中,计算的分位数为{0。005,0。025,0。05, 0。1,0。2、……, 0。8,0。9,0。95,0。975, 0。[995]。两个变量的预测范围都提前一步(对于时间t + 1时间间隔在时间t执行)。该过程需要首先计算预测点,然后使用分位数回归技术形成结果噪声项的分位数。建模过程是在这两个地点2017年的数据上进行的,然后在2018年的数据上进行测试。按照标准建模方式,将2017年数据的点预测和分位数模型应用于2018年数据,然后将分位数添加到点预测中,初步验证该程序的有效性。点预报包含一个使用傅立叶级数对显著周期的季节性模型。对于GHI,它们是一年一次,一天一次和两次,加上节拍频率来调节每日周期以适应一年中的时间。由于太阳能发电厂有一个超大的场地,因此限制了输出,唯一必要的循环是每天一次和两次。一旦从原始序列中减去季节性模型,残差由ARMA (p, q)预测模型表示。这些模型的组合形成了点预测。该过程中的噪声项使用分位数回归建模。对于响应的分位数水平τ,目标是
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Probabilistic forecasting for solar energy
: This paper describes the forecasting of 15 minute solar irradiation on a horizontal plane (GHI) for Seattle, USA, as well as 15 minute solar f arm output for Broken Hill, Australia. The goal is to set error bounds on the forecast, specifically estimating 15 quantiles, from essentially minimum to m aximum. In practice, the quantiles calculated are { 0 . 005 , 0 . 025 , 0 . 05 , 0 . 1 , 0 . 2 , . . . , 0 . 8 , 0 . 9 , 0 . 95 , 0 . 975 , 0 . 995 } . The forecast horizons for both variables are one step ahead (for time t + 1 time interval performed at time t ). The procedure entails first calculating point f orecasts, and then using quantile regression techniques to form the quantiles of the resulting noise terms. The modelling process is performed on a year’s data for 2017 for both locations, and then tested on data from 2018. In the standard modelling manner, the models developed for both the point forecasts and quantiles on the 2017 data are applied to the 2018 data, whereupon the quantiles are added to the point forecasts for initial verification of the efficacy of the procedure. The point forecast contains a model for the seasonality using Fourier series for the significant cycles. For GHI, they are once a year, once and twice a day, plus beat frequencies to modulate the daily cycle to suit the time of year. Since the solar farm has an oversized field, thus capping the output, the only necessary cycles are once and twice a day. Once the seasonality model is subtracted from the original series, the residuals are represented by an ARMA ( p, q ) forecast model. The combination of the models forms the point forecast. The noise terms from this process are modelled using quantile regression. For quantile level τ of the response, the goal is to
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