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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 吳清吉 | |
| dc.contributor.author | Jyh-Huei Tai | en |
| dc.contributor.author | 戴志輝 | zh_TW |
| dc.date.accessioned | 2021-05-20T21:30:58Z | - |
| dc.date.available | 2010-08-20 | |
| dc.date.available | 2021-05-20T21:30:58Z | - |
| dc.date.copyright | 2010-08-20 | |
| dc.date.issued | 2010 | |
| dc.date.submitted | 2010-08-18 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/10456 | - |
| dc.description.abstract | 本文使用台大－普度三維非靜力模式，透過仿黑潮所伴隨之海溫分布狀態，分別在無斜壓性及具斜壓之性大氣環境下的模擬，探討冬季東北季風盛行下，黑潮海域的海氣溫差對海洋大氣對流邊界層發展的影響。
模擬結果顯示，當水平均溫的冷空氣流經海溫梯度時，海溫分布狀態和可感熱通量分布狀態相似；不均勻海溫分布所形成的海氣溫差，透過亂流傳送將可感熱及水氣上傳至大氣。當水氣尚未凝結、或潛熱釋放還不明顯時，可感熱通量分布主導在暖、冷海面上的邊界層發展。基本上，暖海面上邊界層發展較深厚，凝結量較多，邊界層內氣溫也較高。此外，海面可感熱通量梯度對底層大氣加熱不均勻，所引發出的局部氣壓梯度，使得初始均勻的氣流產生局部偏向及合流，位於合流上方的邊界層，較其他區域都更為深厚，凝結量也更多；當合流上方的總液態水及降雨量夠明顯時，凝結的潛熱釋放使得雙胞型態的垂直次環流建立。 當斜壓的冷空氣流經海溫梯度時，由於等氣溫線與等海溫線之間具有夾角，每一條等氣溫線均可與一條最適當的等海溫線搭配，導致最大可感熱通量分布不再依海溫高低而定，而是出現在台灣東北部外海至東海一帶的三角區域內。此情形下，邊界層在黑潮暖軸心附近發展最深厚，但在冷海面和較低緯度的暖海面上，邊界層厚度差異不大，於是形成沿黑潮暖軸心的厚度脊，以及在黑潮暖軸心西北及東南側的厚度槽。此外，在三角區域內，局部的可感熱通量差異，也激發出垂直次環流發展；次環流建立後向東南移動，伴隨的降雨區也離開原本的合流位置，向東南擴及較寬廣的洋面，並在台灣地形阻擋下，沿著地形東側向南發展，其過程及結果是導致氣候上所見冬季台灣陸地與附近洋面上高平均雨量的原因之一。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-05-20T21:30:58Z (GMT). No. of bitstreams: 1 ntu-99-D90229001-1.pdf: 6661390 bytes, checksum: a8b5a2ab74c3d5ac5ab1db6bbb18c68b (MD5) Previous issue date: 2010 | en |
| dc.description.tableofcontents | 摘要 i
致謝 ii 目錄 iii 圖目錄 v 表目錄 xvi 第一章 前言 1 1.1 研究背景 1 1.2 研究目的 7 第二章 相關研究回顧 20 2.1 地形對氣流之影響 20 2.1.1 地形長寬比固定但高度改變的結果 20 2.1.2 地形高度固定但長寬比改變的結果 21 2.1.3 科氏力的影響 22 2.1.4 非線性過程的作用 23 2.2 海氣交互作用對大氣之調節 25 2.2.1 海氣間的熱量交換 25 2.2.2 海洋大氣邊界層雲系的特徵 26 2.2.3 海洋大氣邊界層的熱力結構 27 2.3 海溫梯度與中尺度天氣過程之關係 29 2.4 海氣交互作用與低壓發展 35 第三章 研究工具及方法 52 3.1 預報方程式 52 3.2 座標系統 55 3.3 邊界條件 55 3.4 其他物理過程之計算 56 3.5 有限差分格式 56 第四章 非斜壓大氣下黑潮海域海洋大氣邊界層的發展 58 4.1 東北季風影響下台灣附近的局部環流 58 4.2 黑潮海域海洋大氣邊界層之發展 61 4.2.1 黑潮海溫分布對海洋大氣邊界層熱力結構之影響 61 4.2.2 黑潮海溫分布對海洋大氣邊界層垂直次環流發展之影響 64 第五章 斜壓大氣下冬季台灣近海的海洋邊界層發展 88 5.1 黑潮區域的海氣特性與邊界層特徵 88 5.2 斜壓大氣下黑潮區域邊界層次環流的發展 94 5.3 台灣地形的作用與敏感度測試 100 第六章 結論 123 參考文獻 126 | |
| dc.language.iso | zh-TW | |
| dc.title | 冬季台灣近海對流邊界層發展之數值模擬 | zh_TW |
| dc.title | Numerical Simulation of the Development of the Convective Boundary Layer over the Ocean adjacent of Taiwan in Winter | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 98-2 | |
| dc.description.degree | 博士 | |
| dc.contributor.oralexamcommittee | 柯文雄,郭鴻基,林沛練,李清勝,鄒治華,王重傑 | |
| dc.subject.keyword | 對流邊界層,海溫梯度,垂直次環流, | zh_TW |
| dc.subject.keyword | convective boundary layer,gradient of sea surface temperature,vertical secondary circulation, | en |
| dc.relation.page | 133 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2010-08-18 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 大氣科學研究所 | zh_TW |
| 顯示於系所單位： | 大氣科學系 | |
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