温度预报作为减缓气候变化的手段及其影响——以马里为例

Utibe Billy
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引用次数: 0

摘要

在马里的几个地点进行了温度预报和趋势分析,作为警告潜在威胁天气事件的重要工具,如严重的热浪、风暴、干旱和洪水,这些天气事件可能对人类及其环境构成巨大风险。马里(1700n - 4000w)的五个地点(Segou, Sikasso, Kayes, Gao和Taoudenni)被选为这项研究工作。这项工作使用了从欧洲中期天气预报中心(ECMWF)数据库获得的35年(1985-2019)年温度卫星数据。对不同地点进行Mann-Kendall趋势检验,观察和研究趋势。采用自回归和综合移动平均(ARIMA)、指数平滑(ETS)、TBATS(三角季节性、Box-Cox变换、ARMA误差、趋势和季节成分)和线性模型对各地区10年平均气温进行了预测。在95%置信水平下产生最佳预测的模型预计具有最低的均方根误差(RMSE)值。结果显示,在考虑的地点没有记录到明显的趋势。线性模型对Segou、Kayes和Taoudenni的预测效果最好,而TBATS模型对Gao的预测效果最好,ARIMA模型对Sikasso的预测效果最好。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Temperature Forecasting as a Means of Mitigating Climate Change and Its Effects: A Case Study of Mali
Temperature forecasts and trend analyzes were carried out for several locations in Mali as an important tool for warning of potentially threatening weather events such as severe heat waves, storms, droughts and floods, which could pose a great risk to humans and their environment. Five locations (Segou, Sikasso, Kayes, Gao and Taoudenni) across Mali (170 00’N – 40 00’W) were chosen for this research work. Satellite data of annual temperature obtained from the European Centre for Medium-Range Weather Forecast (ECMWF) database for 35 years (1985-2019) was used for this work. The Mann-Kendall trend test was carried out for various locations to observe and study the trend. Four Models including Auto Regressive and Integrated Moving Average (ARIMA), Exponential smoothening (ETS), TBATS (Trigonometric seasonality, Box-Cox transformation, ARMA errors, Trend and Seasonal components) and the linear model were employed to forecast average temperature for 10 years for all the locations. The model that produces the best forecast at the 95% confidence level is expected to have the lowest Root Mean Square Error (RMSE) value. The results showed that no significant trends were recorded at the considered locations. The linear model produced the best forecast for Segou, Kayes and Taoudenni, while the TBATS model produced the best forecast for Gao and the ARIMA model produced the best forecast for Sikasso.
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