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  • 學位論文

以自組特徵映射網路推估蒸發量

Estimation of Evaporation using a Self-Organizing Map Network

指導教授 : 張斐章

摘要


蒸發現象為影響水氣於水文循環分佈中重要之因素,在農業水資源管理上扮演重要角色。傳統經驗式利用氣象變數推估蒸發量,而忽略蒸發在自然界中呈高度非線性現象,故本研究利用具有分類特性的自組特徵映射網路架構一蒸發量推估模式。 本研究利用恆春氣象站的氣象變數作為模式輸入,透過自組特徵映射網路(SOM)學習,將相似特性的輸入資料聚為一類,並探討拓樸網路架構的潛在特性。自組特徵映射網路可快速有效將輸入的氣象變數分類,形成網路拓樸層,再將各聚類之中心點以線性迴歸方式與輸出層連結,可準確的推估蒸發量。另外建立強制型自組特徵映射網路(ESOM)以加強映射較為極端的案例空間,並與Modified Penman(FAO,1984)、Penman-Monteith(ICID,1994)等傳統經驗式進行比較。結果顯示,拓樸層架構能詳細說明輸入與輸出間映射的關係,且用SOM與ESOM可根據氣象變數作良好的推估;四種模式中以ESOM推估表現最好(RMSE=1.15mm/day,MAE=0.87 mm/day),對於長期蒸發量的推估表現中,也是以ESOM表現最佳。研究再針對已建立的模式進行穩定性與適用性討論,結果顯示直接將網路用於其他地區會因區域蒸發量的差異造成模式推估值與實際觀測值有較為明顯的差異。

並列摘要


The phenomenon of evaporation is an important factor that affects the distribution of water in hydrological cycle and plays a key role in agriculture and water resource management. The tranditional evaporation formulas usally neglect the non-linear characteristics in the nature. In this study we propose the self-organizing map(SOM) network to estimate daily evaporation. First, the daily meteorological data from climate gauges were collected as inputs of the SOM and then classified into topology map based on their similarities to investigate their potential property. To effectively and accurately estimate the daily evaporation, the connected weights between the cluster in topology layer with output layer were trained by using the linear regression method. In addition, we bulit enforced Self-Organizing Map (ESOM) to strength mapping spaces for these extremely data and compared with Modified Penman (FAO,1984) and Penman-Monteith (ICID,1994). The results demonstrated that the topology structures of SOM and ESOM could give a meaningful map to present the clusters of meteorological variables and the networks could well estimate the daily evaporation based on the input meteorological variables used in this study. In comparing the performances of these four models, the ESOM provides the best performance (RMSE=1.15mm/day,MAE=0.87 mm/day). The ESOM performance is also well in estimating long term evaporation. We have the suitability of using these models in other areas where their evaporations are different widely from the original station, the estimation, however, are not well as the one we use in the built station. This result suggests that the network must be adequately trained before it is used to estimate the local evaporation.

參考文獻


13. 黃振昌,2003,「Penman-Monteith方程式日射-日照關係地域性參數之建立與評估」,中國農業工程學報,49(3):79-91。
14. 黃振昌、張德鑫、宋易倫,2005,「Penman-Monteith方程式蒸汽壓力差最佳計算式適用性評估:頻率分析法」,中央氣象局氣象學報,46(1):13-30。
1. 丁裕峰,2004,「併聯式類神經網路於水文事件分析與應用」,台灣大學生物環境工程研究所碩士論文。
5. 杜榮鴻,2005,「應用MODIS影像估算潛勢蒸發散量之研究」,成功大學水利及海洋工程生研究所碩士論文。
9. 陳姜琦,2002,「應用衛星搖測於區域蒸發散量之估算」,成功大學水利及海洋工程生研究所碩士論文。

被引用紀錄


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黃健維(2016)。自組特徵映射網路結合非線性自回歸模式預測屏東平原地下水位〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU201601833
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黃俊霖(2014)。建置智慧型地下水位推估模式-以濁水溪水系為案例〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU.2014.01310

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