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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 吳健銘(Chien-Ming Wu) | |
| dc.contributor.author | Min-Lin Tsai | en |
| dc.contributor.author | 蔡旻霖 | zh_TW |
| dc.date.accessioned | 2022-11-23T09:24:01Z | - |
| dc.date.available | 2021-08-13 | |
| dc.date.available | 2022-11-23T09:24:01Z | - |
| dc.date.copyright | 2021-08-13 | |
| dc.date.issued | 2021 | |
| dc.date.submitted | 2021-07-21 | |
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Yen, 2007: Enhancement of Afternoon Thunderstorm Activity by Urbanization in a Valley: Taipei. Journal of Applied Meteorology and Climatology, 46(9), P1324-1340 Chen, T.-C., M.-C. Yen, J.-D. Tsay, C.-C. Liao, and E. S. Takle, 2014: Impact of Afternoon Thunderstorms on the Land–Sea Breeze in the Taipei Basin during Summer: An Experiment. Journal of Applied Meteorology and Climatology, 53(7), P1714-1738 Cheng, F.-Y., Y.-C. Hsu, P.-L. Lin, and T.-H. Lin, 2013: Investigation of the Effects of Different Land Use and Land Cover Patterns on Mesoscale Meteorological Simulations in the Taiwan Area. Journal of Applied Meteorology and Climatology, 52(3), P570-587 Crosman, E. T. and J. D. Horel, 2010: Sea and Lake Breezes: A Review of Numerical Studies. Boundary-Layer Meteorology, 137, P1-29 Fovell, R. G., 2005: Convective Initiation ahead of the Sea-Breeze Front. Monthly Weather Review, 133(1), P264-278 Jung, J.-H. and A. Arakawa, 2008: A Three-Dimensional Anelastic Model Based on the Vorticity Equation. Monthly Weather Review, 136(1), P276-294 Huang, J.-D., C.-M. Wu, 2020: Effects of Microphysical Processes on the Precipitation Spectrum in a Strongly Forced Environment. Earth and Space Sciences, 7(6), e2020EA001190 Kirshbaum, D. J. and D. R. Durran, 2004: Factors Governing Cellular Convection in Orographic Precipitation. Journal of the Atmospheric Sciences, 61(6), P682-698 Kirshbaum, D. J., 2011: Cloud-Resolving Simulations of Deep Convection over a Heated Mountain. Journal of the Atmospheric Sciences, 68(2), P361-378 Krueger, S. K., G. T. McLean, and Q. Fu, 1995: Numerical Simulation of the Stratus-to-Cumulus Transition in the Subtropical Marine Boundary Layer. Part II: Boundary-Layer Circulation. Journal of the Atmospheric Sciences, 52(16), P2851-2868 Kuo, K.-T., and C.-M. Wu, 2019: The precipitation hotspots of afternoon thunderstorms over the Taipei Basin: Idealized numerical simulations. Journal of the Meteorological Society of Japan, 97(2), P501– 517 Lin, P.-F., P.-L. Chang, B. J.-D. Jou, J. W. Wilson, and R. D. Roberts, 2011: Warm Season Afternoon Thunderstorm Characteristics under Weak Synoptic-Scale Forcing over Taiwan Island. Weather and Forecasting, 26(1), P 44-60 Lin, P.-F., P.-L. Chang, B. J.-D. Jou, J. W. Wilson, and R. D. Roberts, 2012: Objective Prediction of Warm Season Afternoon Thunderstorms in Northern Taiwan Using a Fuzzy Logic Approach. Weather and Forecasting, 27(5), P1178-1197 Porson, A., D. G. Steyn and G. Schayes, 2007: Sea-breeze scaling from numerical model simulations, Part I: Pure sea breezes. Boundary-Layer Meteorology, 122, P17-29 Porson, A., D. G. Steyn and G. Schayes, 2007: Sea-breeze scaling from numerical model simulations, part II: Interaction between the sea breeze and slope flows. Boundary-Layer Meteorology, 122, P31-41 Wu, C.-M. and A. Arakawa, 2011: Inclusion of Surface Topography into the Vector Vorticity Equation Model (VVM). Journal of Advances in Modeling Earth Systems, 3(2) Wu, C.-M. and A. Arakawa, 2014: A Unified Representation of Deep Moist Convection in Numerical Modeling of the Atmosphere. Part II. Journal of the Atmospheric Sciences, 71(6), P2089-2103 Wu, C.-M., B. Stevens, and A. Arakawa, 2009: What controls the transition from shallow to deep convection? Journal of the Atmospheric Sciences, 66(6), P1793-1806 Wu, C.-M., H.-C. Lin, F.-Y. Cheng and M.-H. Chien, 2019: Implementation of the Land Surface Processes into a Vector Vorticity Equation Model (VVM) to Study its Impact on Afternoon Thunderstorms over Complex Topography in Taiwan. Asia-Pacific Journal of Atmospheric Sciences volume, 55, P701-717 Wu, C.-M., M.-H. Lo, W.-T. Chen and C.-T. Lu, 2015: The impacts of heterogeneous land surface fluxes on the diurnal cycle precipitation: A framework for improving the GCM representation of land-atmosphere interactions. Journal of Geophysical Research: Atmospheres, 120(9), P3714-3727 | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/80064 | - |
| dc.description.abstract | 台北盆地是研究午後雷雨如何與背景風場、地形效應和海風相互作用的有趣地點。過去研究指出，在弱綜觀環境下，來自淡水和基隆河谷的海風通常會穿過台北盆地，先在南邊山坡上輻合引發降水，之後才盆地內的後續對流。然而亦有不少觀測案例，區域環流會在台北盆地輻合並長出雷雨胞，而不是由山區對流所引發。本研究使用中央氣象局(CWB)的地表測站觀測數據，風花圖統計結果顯示，有70%以上的台北雷雨案例在台灣海峽北側會是吹西南背景風。進一步使用Vector Vorticity Equation cloud-resolving Model (VVM)進行理想實驗探討台北午後雷雨和西南背景風之間的關係，分別測試風速、林口台地山高、桃園土地利用之影響。固定林口山高為500m，背景風速為3m/s之實驗起始降雨在盆地內部，平均降雨率可到達3mm/hr，相對於1m/s與5m/s時起始降雨在山區，盆地內平均降雨率皆不超過1.5mm/hr。若固定背景風速在3m/s，改變林口台地高度為1000m時盆地內降水為全實驗最少，而高度為250m時盆地內平均降水率最大可達到2.5m/s。分析各實驗之區域環流，顯示西南背景風使桃園城鄉邊界的熱力環流進入盆地內，因此當風速適中約介於2m/s到4m/s之間，且林口台地的高度不會太高時，桃園邊界層環流可以進入台北盆地與兩河谷的海風輻合，直接在盆地中心產生強烈對流。而改變桃園土地利用，對盆地內累積降雨量影響不大，主要影響為桃園城鄉交界位置會決定初始對流輻合之位置。本研究針對西南季風對於台北午後對流的激發所扮演的角色，或許能在未來改善午後雷雨之預報準確度與極端降水之預警。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2022-11-23T09:24:01Z (GMT). No. of bitstreams: 1 U0001-1307202117220300.pdf: 11994219 bytes, checksum: 7648de821673b1f03ba92d859b559db8 (MD5) Previous issue date: 2021 | en |
| dc.description.tableofcontents | 口試委員會審定 i 誌謝 ii 摘要 iii Abstract iv 目錄 vi 表目錄 vii 圖目錄 viii 第一章 前言 1 第二章 觀測資料與統計結果 3 2.1資料選取 3 2.2統計結果 4 第三章模式介紹與實驗設計 5 3.1VVM模式 5 3.2基本設定 5 3.3理想地形 6 3.4實驗變因 6 第四章理想化模擬結果 8 4.1控制組(CTL) 8 4.2背景風速 9 4.3林口山高 11 4.4桃園都市化 12 第五章結論 14 附錄 15 參考文獻 16 附表 19 附圖 20 | |
| dc.language.iso | zh-TW | |
| dc.subject | 西南季風 | zh_TW |
| dc.subject | 理想化模擬 | zh_TW |
| dc.subject | 地形效應 | zh_TW |
| dc.subject | 海陸風 | zh_TW |
| dc.subject | 午後雷雨 | zh_TW |
| dc.subject | VVM模式 | zh_TW |
| dc.subject | sea breezes | en |
| dc.subject | VVM Model | en |
| dc.subject | topography | en |
| dc.subject | southwesterly flow | en |
| dc.subject | afternoon thunderstorms | en |
| dc.subject | idealized simulation | en |
| dc.title | 台北盆地午後雷雨之理想實驗模擬:西南背景風之角色 | zh_TW |
| dc.title | Idealized Simulations of Afternoon Thunderstorm Initiation Over Taipei Basin: The Roles of Southwesterly Background Wind | en |
| dc.date.schoolyear | 109-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 陳維婷(Hsin-Tsai Liu),蘇世顥(Chih-Yang Tseng) | |
| dc.subject.keyword | 理想化模擬,午後雷雨,海陸風,西南季風,地形效應,VVM模式, | zh_TW |
| dc.subject.keyword | idealized simulation,afternoon thunderstorms,sea breezes,southwesterly flow,topography,VVM Model, | en |
| dc.relation.page | 55 | |
| dc.identifier.doi | 10.6342/NTU202101440 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2021-07-21 | |
| 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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