請用此 Handle URI 來引用此文件：
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/2335完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 楊穎堅 | |
| dc.contributor.author | Chia-Ying Hsieh | en |
| dc.contributor.author | 謝佳穎 | zh_TW |
| dc.date.accessioned | 2021-05-13T06:39:15Z | - |
| dc.date.available | 2019-08-25 | |
| dc.date.available | 2021-05-13T06:39:15Z | - |
| dc.date.copyright | 2017-08-25 | |
| dc.date.issued | 2017 | |
| dc.date.submitted | 2017-08-15 | |
| dc.identifier.citation | Archiving, Validation and Interpretation of Satellite Oceanographic data (AVISO), 2017: https://www.aviso.altimetry.fr/en/data/products/ sea-surface-height-products/global/msla-h.html
Advanced Very High Resolution Radiometer (AVHRR), 2017: https://www.ncdc.noaa. gov/ oisst/data-access Anthes, R. A., 1982: Tropical cyclones: Their evolution, structure and effects, Amer. Meteor. Soc., 41(19), 1982 – 208. Berliand, M. E., and T. G. Berliand, 1952: Measurement of the effective radiation of the earth with varying cloud amounts (in Russian). IZV. Akad. Nauk SSSR, Ser. Geofiz., 1, 64-78. Blanc, T. V., 1987: Accuracy of bulk-method-determined flux, stability, and sea surface roughness. J. Geophys. Res., 92, 3867-3876. Bradley, F., P. A. Coppin and J. S. Godfrey, 1991: Measurements of sensible and latent heat flux in the western equatorial Pacific ocean. J. Geophys. Res., 96, 3375-3389. Chang, H.-I, Y.-F. Ma, W.-H. Her, Y. J. Yang, M.-H. Chang, S. Jan, and C.-L. Wei (2017, Jun). The NTU Buoy for Typhoon Observation, Part 1: System. Oceans 2017, Aberdeen, UK. Chang, S.W. and R.A Anthes, 1978: Numerical simulations of the ocean’s nonlinear baroclinic response to translating hurricanes, J. Phys. Oceanogr., 8, 468–480. Chia, H. -H. and C.-C. Wu, 2006: Air-sea turbulent fluxes of the western equatorial Pacific, Atmos. Sci., 34(2), 127-141. Chiu, P. -G. and J.-Y. Yu, 2006: Examining typhoon activity in the western North Pacific: Difference between active and non-active years, Atmos. Sci., 34(3), 201-215. D’Asaro, E. A., C. C. Eriksen, M. D. Levine, P. Niiler, C. A. Paulson, and P. van Meurs , 1995: Upper-ocean inertial currents forced by a strong storm. Part I: Data and comparisons with linear theory, J. Phys. Oceanogr., 25, 2909–2936. Day, C. G., and F. Webster, 1965: Some current measurements in the Sargasso sea. Deep-Sea Res., 12, 805-814. Fairall, C., W. and S. E. Larsen, 1986: Inertial dissipation method and turbulent fluxes at the air ocean interface, Bound. Layer Meteorol., 34, 287-301. Fairall, C., C. W., E. F. Bradley, J. E. Hare, A. A. Grachev and J. B. Edson, 2003: Bulk parameterization of air-sea fluxes: Updates and verification for the COARE algorithm, J. Climate, 16, 571-591. Fung, I. Y., D. E. Harrison, and A. A. Lacis, 1984: On the variability of the net longwave radiation at the ocean surface. Rev. Geophys, Space Phys., 22, 177-193. Gao, S., and L. S. Chiu, 2010: Surface latent heat flux and rainfall associated with rapidly intensifying tropical cyclones over the western North Pacific. Int. J. Remote Sens., 31, 4699-4710. Geisler, J.E., 1970: Linear theory of the response of a two-layer ocean to a moving hurricane, Geophys. Fluid Dyn., 1, 249-272. Gray, W. M., 1968: Global view of the origin of tropical disturbances and storms. Mon. Wea. Rev., 96(10), 669-700. Hayes, S. P., L. J. Mangum, J. Picaut, A. Sumi, and K. Takeuchi, 1991: TOGA TAO: A moored array for real-time measurements in the tropical Pacific Ocean. Bull. Am. Meteorol. Soc., 72, 339–347. Hormann, V., L. R. Centurioni, L. Rainville, C. M. Lee, and L. J. Braasch, 2014: Response of upper ocean currents to Typhoon Fanapi, Geophys. Res. Lett., 3995-4003. Huang, P., I-I Lin, C. Chou, and R.-H. Huang, 2015: Change in ocean subsurface environment to suppress tropical cyclone intensification under global warming. Nat. Commun., 6(7188), 1-9. Hwang, C., C.-R. Wu, and R. Kao, 2004: TOPEX/Poseidon observations of mesoscale eddies over the Subtropical Countercurrent: Kinematic characteristics of an anticyclonic eddy and a cyclonic eddy. J. Geophys. Res., 109(C08013), 1-17. Kunze, E., 1985: Near-Inertial wave propagation in geostrophic shear. J. Phys. Oceanogr., 15, 544–565. Leipper, D., and D. Volgenau, 1972: Hurricane heat potential in the Gulf of Mexico. J. Phys. Oceanogr., 2, 218–224. Lin, I-I, C.-C. Wu, K., A. Emanuel, I-H. Lee, C.-R. Wu and I.-F. Pun, 2005: The interaction of supertyphoon Maemi (2003) with a warm ocean eddy. Mon. Wea. Rev., 133, 2635-2649. Liu, W. T., K. B. Katsaros, and J. A. Businger, 1979: Bulk parameterization of air-sea exchanges of heat and water vapor including the molecular constraints at the interface. J. Atoms. Sci., 36, 1722-1735. Ma, Z., J. Fei, X. Huang, and X. Cheng, 2014: Contributions of surface sensible heat fluxes to tropical cyclone. Part I: Evolution of tropical cyclone intensity and structure. J. Atmos. Sci.,72, 120-140. National Centers for Environmental Prediction (NCEP) ,2017: https://www.esrl.noaa. gov/psd/data/ gridded/data.ncep.html Objectively Analyzed air-sea Fluxes (OAFlux) ,2017: http://oaflux.whoi.edu/index.html Pawlowicz, R., B. Beardsley, and S. Lentz, 2002: Classical tidal harmonic analysis including error estimates in MATLAB using T_TIDE., Computers and Geosciences, 28, 929-937. Payne, R. E., 1972: Albedo of the sea surface. J. Atmos. Sci., 29, 959-970. Pollard, R. T., 1970: Surface waves with rotation: An exact solution. J. Geophys. Res., 75, 5895-5898. Price, J. F., 1981: Upper ocean response to a hurricane. J. Phys. Oceanogr., 11, 153–175. Price, J. F., R. A. Weller, and R. Pinkel, 1986: Diurnal cycling: observations and models of the upper ocean response to diurnal heating, cooling, and wind mixing. J. Geophys. Res., 91, 8411-8427. Pun, I.F., Y.-T. Chang, I.-I. Lin, T.Y. Tang, and R.-C. Lien, 2011: Typhoon-ocean interaction in the western North Pacific: Part 2. Oceanography, 24(4), 32–41. Qiu, B, 1999: Seasonal eddy field modulation of the North Pacific subtropical countercurrent: TOPEX/Poseidon observation and theory. J. Physi. Oceanogr., 29, 2471-2486. Reed, R., 1977: On estimating insolation over the ocean. J. Phys. Oceanogr., 7, 82-485. Rohde, R. A., (2006, November 2): Historic tropical cyclone tracks. Retrieved June 28, 2017, from https://earthobservatory.nasa.gov/IOTD/view.php?id=7079 Schlesinger, M. E., and J. F. B. Mitchell, 1987: Climate model simulations of the equilibrium climate response to increased carbon dioxide. Rev. Geophys., 25, 760-798. Shay, L. K., A. J. Mariano, S. D. Jacob, and E. H. Ryan, 1998: Mean and near-inertial current response to Hurricane Gilbert, J. Phys. Oceanogr., 28, 858–889. Zeng, X., M. Zhao, and R. E. Dickinson, 1998: Intercomparison of bulk aerodynamic algorithms for the computation of sea surface fluxes using TOGA COARE and TAO data. J. Climate, 11, 2628-2644. 楊穎堅, 張宏毅, 何文華, 馬玉芳, 邱協棟, 謝佳穎, 李文慧, 謝祥志, 連政佳, 鄭欣雅, 魏慶琳（2016a）。海氣象即時傳輸浮標之精進與海上測試。105年天氣分析與預報研討會，臺北。 楊穎堅, 張宏毅, 何文華, 邱協棟, 謝佳穎, 李文慧, 馬玉芳, 謝祥志, 連政佳, 洪瑋廷（2016b）。新一代海氣象即時傳輸浮標對颱風觀測之應用。第十八屆水下技術研討會暨國科會成果發表會，台南。 楊穎堅, 張宏毅, 張明輝, 詹森, 邱銘達, 何文華, 邱協棟, 李文慧, 馬玉芳, 謝祥志, 連政佳, 洪瑋廷, 魏慶琳（2015）。海氣象即時傳輸浮標發展及其對颱風觀測之應用。104年天氣分析與預報研討會，臺北。 | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/2335 | - |
| dc.description.abstract | 西北太平洋為颱風生成的熱區，此海域的颱風較其他海域多且強。颱風生命週期中，大多時間滯留於海面上，因此除了當時的大氣環境會影響其生長，海洋狀態亦非常重要，若能即時掌握上層海洋的改變，將有助於改善對颱風強度的預報。本研究利用國立臺灣大學海洋研究所的海氣象即時傳輸浮標，在2015和2016夏天於鵝鑾鼻東南方海域約375與175公里處，進行測試實驗時所收集到的資料，搭配衛星遙測資料與數值模式資料討論颱風造成的海洋變化。在觀測期間內，計有2015年的蓮花、昌鴻、蘇迪勒與天鵝；及2016年的尼伯特、莫蘭蒂、馬勒卡、梅姬與艾利，等9個颱風經過附近海域，其中NTU1和NTU2站分別進到馬勒卡與尼伯特颱風的颱風眼範圍內。在分析後得到以下結論：慣性運動在颱風逐漸靠近即開始形成，且颱風的到達時間點會影響慣性流之大小。此外，近慣性運動週期除了可能受到背景場或渦旋影響外，亦可能受到颱風尚在南邊時的影響，致使觀測所得之慣性週期略大於當地慣性週期。在強烈颱風靠近時，會因強風造成的流切不穩定使混合層之厚度可以在5小時內增加100公尺，且可能為了維持位渦守恆，使颱風來時所造成之厚的混合層，在颱風中心離開後隨即快速變薄。此外，在颱風中心通過之後，因水平平流帶來颱風左側之較暖的海水，使表層海洋有回溫現象。 | zh_TW |
| dc.description.abstract | Western North Pacific is the most active area for typhoons in the world. To understand the changes of upper ocean is necessary for optimizing the typhoon intensity forecasts. In summer of 2015 and 2016, the Institute of Oceanography, National Taiwan University (IONTU) deployed two air/sea-observing buoys at distances of approximately 375 km (station NTU1) and 175 km (station NTU2) from the southernmost tip of Taiwan. During the trails, buoys survived nine typhoons (Linfa, Chanhom, Soudelor, Goni, Nepartak, Meranti, Malakas, Megi, and Aere). Among them, the stations NTU2 and NTU1 almost coincided with the paths of typhoon Nepartak and Malakas, respectively. In this research, buoy data, satellite and numerical model products were used to figure out the ocean responses resulting from typhoon. Observation data shows two major conclusions. First, the near inertial motion started when typhoon approached, and the arrival time could be related with magnitude of inertial current speed. Furthermore, the observed inertial period was larger than local inertial period. It is probably related to interactions between near- and sub-inertial currents or the inertial motion generated at the southern side of buoy. Second, the thickness of mixed layer increased 100m in 5 hours by current shear instability. Besides, the thickness of mixed layer rapidly decreased after typhoon’s center has passed. It could be related to potential vorticity conservation. Moreover, the temperature of sea surface increased is due to the horizontal advection. | en |
| dc.description.provenance | Made available in DSpace on 2021-05-13T06:39:15Z (GMT). No. of bitstreams: 1 ntu-106-R04241101-1.pdf: 9805495 bytes, checksum: 718c03313e3a8f07eab7a0a8cfe1c702 (MD5) Previous issue date: 2017 | en |
| dc.description.tableofcontents | 口試委員會審定書 I
誌謝 II 中文摘要 III 英文摘要 IV 目錄 V 圖目錄 VII 表目錄 XI 符號表 XII 第一章 緒論 1 1.1研究背景回顧 1 1.2研究動機與目的 3 第二章 海氣象即時傳輸浮標介紹 5 第三章 實驗與資料介紹 15 3.1實驗設計 15 3.1.1 2015年 15 3.1.2 2016年 16 3.2資料介紹 17 3.2.1 浮標資料 17 3.2.2 表面高度異常資料 17 3.2.3 大氣模式資料 17 3.2.4 海表溫資料 18 3.2.5 熱含量資料 18 第四章 資料分析 24 4.1資料初步分析 24 4.1.1 觀測資料簡述 24 4.1.2 資料比對 26 4.2上層海洋熱含量與海氣熱通量之分析 39 4.2.1 上層海洋熱含量 39 4.2.2 海氣熱通量 39 4.3颱風造成之慣性運動 47 4.4上層海洋變化過程 66 第五章 討論與結論 71 5.1討論 71 5.1.1 近慣性運動 71 5.1.2 上層海水混合後之恢復過程 72 5.1.3 熱通量之年際變化 73 5.2結論 80 參考文獻 81 | |
| dc.language.iso | zh-TW | |
| dc.subject | 混合過程 | zh_TW |
| dc.subject | 海氣象浮標 | zh_TW |
| dc.subject | 颱風 | zh_TW |
| dc.subject | 熱通量 | zh_TW |
| dc.subject | 近慣性運動 | zh_TW |
| dc.subject | Mixing process | en |
| dc.subject | Air/sea-observing buoy | en |
| dc.subject | Typhoon | en |
| dc.subject | Heat flux | en |
| dc.subject | Near inertial motion | en |
| dc.title | 浮標觀測颱風中心附近海域的海氣象變化之研究 | zh_TW |
| dc.title | Investigation of data buoys observed sea surface atmosphere and upper ocean variations during typhoons | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 105-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 張明輝 | |
| dc.contributor.oralexamcommittee | 詹森,張宏毅,曾若玄 | |
| dc.subject.keyword | 海氣象浮標,颱風,熱通量,近慣性運動,混合過程, | zh_TW |
| dc.subject.keyword | Air/sea-observing buoy,Typhoon,Heat flux,Near inertial motion,Mixing process, | en |
| dc.relation.page | 85 | |
| dc.identifier.doi | 10.6342/NTU201703398 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2017-08-15 | |
| 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 | |
文件中的檔案：
| 檔案 | 大小 | 格式 | |
|---|---|---|---|
| ntu-106-1.pdf | 9.58 MB | Adobe PDF | 檢視/開啟 |
系統中的文件，除了特別指名其著作權條款之外，均受到著作權保護，並且保留所有的權利。