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Please use this identifier to cite or link to this item: http://scholars.ntou.edu.tw/handle/123456789/26443
標題: Application of Empirical Mode Decomposition to Land Surface Temperature Projection Under a Changing Climate
作者: Chang, Che-Wei
Huang, Wen-Cheng 
關鍵字: Empirical Mode Decomposition;non-stationary sequences;temperature;Taipei City
公開日期: 2025
出版社: MDPI
卷: 17
期: 15
來源出版物: WATER
摘要: 
This study takes the daily temperature series of Taipei City as an example and proposes a data projection method based on Empirical Mode Decomposition (EMD), which effectively resolves the challenge of modeling non-stationary sequences. According to the daily mean temperature records from 1971 to 2023, Taipei has experienced an average warming rate of 0.02 degrees C per year. After applying EMD, the data were decomposed into 12 intrinsic mode functions (IMFs) and one residual trend. Among them, IMF5, with a period of 352 days (approximately one year), contributes 78% of the total energy, representing the dominant climatic cycle component. In this study, daily temperatures were categorized into five thermal levels: Cold (<12 degrees C), Cool (12-18 degrees C), Moderate (18-27 degrees C), Warm (27-32 degrees C), and Hot (>32 degrees C). In addition, using a 5-year moving process based on the annual EMD results, the IMFs and residuals were recombined to generate 390,625 synthetic sequences per year. Results show that the monthly mean temperatures of each year's simulations closely match the observations, capturing the non-stationary characteristics of temperature variations. The overall classification accuracy of simulated versus observed daily temperature categories ranges from 60% to 71%, with an average of 65.1%. In summary, the EMD combined with the 5-year moving process developed in this study demonstrates a helpful data projection approach with effective reconstruction of periodic structures and stable simulation accuracy. It offers practical value for reconstructing urban climate variability, conducting risk assessments, and analyzing long-term warming trends. Moreover, it serves as a vital tool for modeling non-stationary climate data and supporting future projections.
URI: http://scholars.ntou.edu.tw/handle/123456789/26443
DOI: 10.3390/w17152204
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