怒江下游气象干旱的统计模型预测

Wenhua Chen, Juan Xu, Shuangcheng Li
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引用次数: 1

摘要

全球气候变化、气温上升以及干旱等极端气象灾害威胁着自然生态系统和人类社会的发展。干旱预报是发展减灾系统的重要一步。基于标准化降水指数(SPI)和标准化降水蒸散指数(SPEI),利用统计自回归综合移动平均(ARIMA)模型对怒江下游某主要支流的干旱状况进行了预测。我们使用2001 - 2010年的数据来拟合模型,并使用2011 - 2013年的数据进行模型验证。结果表明,各指标序列的决定系数(R2)均在0.85以上,均方根误差和平均绝对误差均较低,表明ARIMA模型对该地区是有效和适宜的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Prediction of Meteorological Drought in the Lower Nu River by Statistical Model
Global climate change, temperature rise and some kinds of extreme meteorological disaster, such as the drought, threaten the development of the natural ecosystem and human society. Forecasting in drought is an important step toward developing a disaster mitigation system. In this study, we utilized the statistical, autoregressive integrated moving average (ARIMA) model to predict drought conditions based on the standardized precipitation index (SPI) and standardized precipitation evapotranspiration index (SPEI) in a major tributary in the lower reaches of Nu River. We employed data from 2001 to 2010 to fit the model and data from 2011 to 2013 for model validation. The results showed that the coefficients of determination (R2) was over 0.85 in each index series, and the root-mean-square error and mean absolute error were low, implying that the ARIMA model is effective and adequate for this region.
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