文學院
Permanent URI for this communityhttp://rportal.lib.ntnu.edu.tw/handle/20.500.12235/2
院成立於民國44年，歷經50餘年的銳意發展，目前設有國文、英文、歷史、地理、臺文等5個學系、翻譯和臺灣史2個獨立所，以及全球華人寫作中心和國際臺灣學研究中心。除臺史所僅設碩士班，其餘6個系所均設有碩、博士班；目前專兼任教師近250人，學生約2500餘人。
本院早期以培養優秀中學國文、英文、歷史和地理教師為鵠的，臺灣中學語文和史地教育的實踐與成功，本院提供不可磨滅的貢獻。近年來，本院隨師範體系轉型而調整發展方向，除維持中學師資培育的優勢外，也積極朝理論研究和實務操作等面向前進。目前，本院各系所師培生的教師檢定通過率平均在95%以上；非師培生在文化、傳播、文學、應用史學及環境災害、地理資訊系統等領域發展，也已卓然有成。
本院各系所教師的研究能量極為豐富，參與國內外學術活動相當活躍。根據論文數量、引用次數等指標所作的學術力評比，本院居人文領域全國第2名。各系所之間，無論是教師的教學與研究，或學生的生活與學習，都能相輔相成、榮辱與共，彼此渾然一體，足堪「為師、為範」而無愧。
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Item 臺灣東部河口地區之地形學研究(地理學系, 1995-10-??) 石再添; 張瑞津; 林雪美; 張政亮; 劉明錡; 陳政典The vincinity of the estuaries is one of the most populated area in the world. In order to ultilize the resources of this area more reasonably, the understanding of its geomorphological, hydrological and sedimentary characteristics becomes a main and basic task. Since estuary is located on the interface of river and sea, the morphology of estuary is influenced by the factors coming from both environments. The drainage basin area, shoreline length, shape factor, channel gradient, runoff, sediments and monthly discharge, etc. are factors coming from land, while the wind, current, wave and tide etc. coming from the sea. This study focuses on eleven estuaries of the eastern coast of Taiwan. Based on the stream slope, number of channels, discharge, etc., these estuaries can be divided into straight and braided pattern. The former has sandbars or spurs, such as Hualien Hsi, Hsiukuluan Hsi and Kangkou Hsi, while the latter have braided channels, sandy-gravel sediments and changeable sandbars, such as Hoping Hsi, Liwu Hsi and the estuaries in Taitung coastal area. The eastern coast is classified as wave-dominated type according to average wave height and tidal range. The wave impacting upon the area between Hoping Hsi and Hsiukuluan Hsi is severer. The forms of the estuaries in eastern Taiwan have significant seasonal change due to the seasonal differences of discharge, monsoon and typhoon. In the summer, the channels usually become wider and the sandbars are gentler and extended seaward for most estuaries. In the winter, however, these sandbars become narrower, steeper and extend toward right bank. The mouth of channels will be narrowed or even closed when typhoon coming. The forms of estuaries are stable in the long-term scale. Eleven estuaries have only slight change during the period from 1904 to 1989, moving back and forth within the distance of 250m. The channel migration of most estuaries, however, is obvious.Item 臺灣西南部河口地區之地形學研究(地理學系, 1995-03-??) 石再添; 張瑞津; 林雪美; 張政亮; 劉明錡; 陳政典The vincinity of the estuaries is one of the most populated area in the world. In order to ultilize the resource of this area more reasonably, the understanding of geomorphogical, hydrological and sedimentary characteristics becomes a main and basic task. Since estuary is located on the interface of river and sea, the morphology of estuary is influenced by the factors coming from both environments. The drainage basin area, shoreline length, shape factor, channel gradient, opening form, runoff, sediments, and monthly discharge etc. coming from the land. While the wind current, wave and tide etc. coming from the sea. This study area focuses on 20 estuaries of the south-western coast of Taiwan. The five of them are gravel estuaries and the rest are sandy. By correlation grain size of sandy estuaries has relationship with channel gradient below 100m, width of opening and shape factor. The forms of sand bar on estuaries are changed seasonly. Most of them has a tendency migrating southward due to northern moonsoon. The 20 estuaries can be classified into the wave dominated type, the tide dominated type and the runoff dominated type according average wave height, specific discharge and tidal range. Comparing the location of 20 estuaries during the period from 1904 to 1990(85 years). Most estuaries tend to migrate westward. The changes of estuaries are controlled by the intensity of wave and precipitation, the influence of reservior and hydraulic engineering and the changes of land use.Item 颱風事件對臺灣河口地形的影響分析(地理學系, 2002-11-??) 林雪美; 彭佳偉; 張喬盛河口地形的形成多依賴長期穩靜變動的河海營力，其平均能量對河口的形成與破壞是緩慢累積的，但是颱風、豪雨等突發事件所帶來的最大能量，其對河口塑形的重要性卻常遠較平均能量為大，往往造成河口地形在短時間內顯而易見的變動。本研究以中港溪口與水璉溪口為對象，利用野外沙洲剖線實測、粒度分析、數值地形等方法，探討研究期間颱風事件對河口沙洲的改變情形。主要目的在於了解河口在颱風事件的強烈能量下的反應情形，並比較不同規模與性質河口的差異性。期能藉由河口地形變動特性的認識，提供下游地區環境災害的預防及開發利用之參考。 研究得知水璉溪口經歷啟德和碧利斯兩個颱風後，河口沙洲被沖刷後退，兩岸沙洲壩變窄而陡；中港溪口在桃芝颱風後，河口沙洲形態變動幅度不大，但納莉颱風後，右岸河口沙洲幾乎全遭沖毀，殘餘的沙洲略有外海偏移的現象，河口沙洲坡度皆變得陡峭，顯示納利颱風對河口地形產生莫大的影響。比較中港溪與水璉溪河口地形對於颱風事件的反映差異，可以得知河口主導營力是重要因素。以潮汐為主控營力的中港溪口，受颱風事件的影響，「逕流+滿潮」的沖刷作用遠超過風浪增強來得重要；而水璉溪口在特殊事件下以風浪為主導營力，受颱風事件的影響，「風浪」的沖刷營力則遠超過逕流增加等作用。再者，水璉溪流域面積小，颱風事件後三個月已大致回復颱風前沙洲形態。而河口粒徑與水璉溪口相近的中港溪口，流域面積為其16倍，在納利颱風過後一年，河口沙洲形態仍未回復。則又說明河川規模是河口地形變動的重要因素；也說明不同事件所造成的河海營力規模，亦是河口地形變動的關鍵因子。