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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 柯彥廷(Yen-Ting Ko) | |
| dc.contributor.author | Tsung-Lin Tsai | en |
| dc.contributor.author | 蔡宗霖 | zh_TW |
| dc.date.accessioned | 2022-11-23T09:00:51Z | - |
| dc.date.available | 2022-02-16 | |
| dc.date.available | 2022-11-23T09:00:51Z | - |
| dc.date.copyright | 2022-02-16 | |
| dc.date.issued | 2022 | |
| dc.date.submitted | 2022-02-11 | |
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Dalrymple. Water wave mechanics for engineers and scientists. Vol. 2. world scientific publishing company, 1991. DOI: 10.1142/9789812385512_0001 36. Nooghabi, Aida Hejazi, et al. 'Coda reconstruction from cross-correlation of a diffuse field on thin elastic plates.' Physical Review E 96.3 (2017): 032137. DOI: 10.1103/PhysRevE.96.032137 | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79452 | - |
| dc.description.abstract | 在21世紀因為數個劇烈地震產生的海嘯已經帶來了嚴重的損失。為了減少自然災害帶來的損失，必須發展海嘯預警系統。現今有兩種主要的方法監測海嘯，一個是DART(Deep-ocean Assessment and Reporting of Tsunami)系統另一個是透過COMCOT(Cornell Multi-grid Coupled Tsunami model)軟體進行數值模擬。DART是透過海嘯儀連接浮標可以提供即時偵測的資訊，而COMCOT是主要是透過淺水波方程式模擬海嘯傳遞行為來預估到時。以上的兩種方法都需要很高的成本且沒辦法有效的預測近岸所產生的海嘯。 從噪訊地震學中任意測站對記錄的連續資料互相關結果可以近似於測站間的格林函數得到了啟發。近年來，已經有許多透過噪訊資料進行互相關的研究且得到很好的結果。模擬上，Saito和Kawahara將模擬噪訊源所激發的海洋訊號傳遞至兩側站的結果進行互相關，發現其結果會近似於水體的的格林函數。而本研究將會驗證實際海洋噪訊互相關函數結果可否建立可信的水體特徵函數，如果可行，將可以有效的減少近域海嘯帶來的傷亡及破壞。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2022-11-23T09:00:51Z (GMT). No. of bitstreams: 1 U0001-1002202201231500.pdf: 9098632 bytes, checksum: 636d6a305ddbe6a91279774322c0b8fa (MD5) Previous issue date: 2022 | en |
| dc.description.tableofcontents | 目 錄 口試委員會審定書 I 致謝 II 摘要 III ABSTRACT IV 目 錄 V 圖目錄 VII 表目錄 IX 第一章 緒論 1 1.1海嘯 1 1.1.1 海嘯的成因與發展過程 1 1.1.2臺灣歷史上的海嘯 4 1.1.3 海嘯預警系統 6 1.2 環境噪訊在地球科學上的發展 9 1.3 研究動機與目標 11 第二章 背景理論 12 2.1 環境噪訊 12 2.2 互相關 16 2.3 MSNOISE 18 2.4 海嘯 19 2.4.1 波浪運動 19 2.4.2 海嘯發生時的水體運動以及能量 19 2.5 COMCOT 21 2.5.1 控制方程式 22 2.5.1.1 線性淺水波方程式 22 2.5.1.2非線性淺水波方程式 23 第三章 資料處理 24 3.1 資料來源 24 3.2 資料處理流程 28 3.3 原始資料處理 30 3.4 資料正規化處理 38 3.4.1 時間域正規化處理 38 3.4.2 頻率域正規化處理 40 3.5 堆疊 41 第四章 結果與討論 45 4.1 正規化討論 45 4.2 CCF疊加與時間變化 47 4.3 實際地震、COMCOT模擬及水體噪訊互相關結果 52 4.3.1 2021/08/05外海地震COMCOT模擬結果與實際潮位紀錄 52 4.3.2 EOS2位置COMCOT模擬結果與實際潮位紀錄 55 4.3.3 CCF結果探討 58 4.3.3.1 時間修正 58 4.3.3.2 路徑影響 64 第五章 結論 66 參考文獻 68 | |
| dc.language.iso | zh-TW | |
| dc.title | 從海洋噪訊中重建水體特徵函數 | zh_TW |
| dc.title | Reconstruction of Water Eigenfunction from Oceanic Ambient Noise | en |
| dc.date.schoolyear | 110-1 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 黃信樺(Chen-Chi Wu),洪淑蕙,陳映年 | |
| dc.subject.keyword | 環境噪訊,互相關函數,海嘯預警系統,淺水波理論,海洋噪訊, | zh_TW |
| dc.subject.keyword | Ambient Noise,Cross-correlation Function,Tsunami Warning System,Shallow Water Equation,Oceanic Noise, | en |
| dc.relation.page | 73 | |
| dc.identifier.doi | 10.6342/NTU202200496 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2022-02-13 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位： | 海洋研究所 | |
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