Responsive image
博碩士論文 etd-0716117-165448 詳細資訊
Title page for etd-0716117-165448
論文名稱
Title
溫室氣體對大氣近地表溫度之影響
The Effect of Greenhouse Gases on Atmospheric Temperature near the Earth Surface
系所名稱
Department
畢業學年期
Year, semester
語文別
Language
學位類別
Degree
頁數
Number of pages
43
研究生
Author
指導教授
Advisor
召集委員
Convenor
口試委員
Advisory Committee
口試日期
Date of Exam
2017-07-21
繳交日期
Date of Submission
2017-08-16
關鍵字
Keywords
水蒸氣、二氧化碳、吸收係數、對流層、溫室效應
greenhouse effects, water vapor, carbon dioxide, absorption coefficient, troposphere
統計
Statistics
本論文已被瀏覽 5645 次,被下載 0
The thesis/dissertation has been browsed 5645 times, has been downloaded 0 times.
中文摘要
本研究探討對流層(小於10公里高度)二氧化碳與水蒸氣之吸收係數對溫度之影響。可見光範圍附近與短波長範圍內的太陽輻射可穿過大氣層被地面吸收及反射。地面會發射長波長範圍內的輻射。大氣層存在二氧化碳和水蒸氣如同一層溫室玻璃會使大氣溫度增加。二氧化碳和水蒸氣是導致大氣溫室效應的氣體。雖然全球暖化對人類的生活產生了強烈的影響,全球暖化的原因仍然存在爭議。本研究因此有系統地定量計算了對流層中二氧化碳與水蒸氣之吸收係數。吸收係數為波長、溫度和濃度的函數。二氧化碳的主要吸收波段之中心波長為15μm、4.3μm、2.7μm及2μm,而水蒸氣以71μm、6.3μm、2.7μm、1.87μm、1.38μm為波段之中心波長吸收。本研究理論模型與實驗數據的結果一致。計算結果證明了二氧化碳與水蒸氣對對流層溫度之影響。
Abstract
Absorption coefficient of carbon dioxide and water vapor responsible for temperature in the troposphere layer, which is less than the altitude of 10 km in the atmosphere, is presented in this study. It has been well known that the solar irradiation can penetrates through the troposphere layer within short wavelength range near the visible range, and it can then be absorbed, scattered by the atmosphere, and absorbed and reflected by the earth ground. The ground emits radiation in the ranges of long wavelengths. In the presence of carbon dioxide and water vapor, the atmosphere acting as the glass of a greenhouse increases temperature of the atmosphere. Greenhouse gas is the gas component that contributes to the greenhouse effect in the atmosphere. Even though global warming strongly affects the life of the human being, the cause of global warming is still controversial. This study thus establishes a fundamental, systematical and quantitative analysis of absorption coefficient of carbon dioxide and water vapor in the troposphere layer. Absorption coefficient is a function of wavelength, temperature and concentration. Absorptions of carbon dioxide are absorbed in bands centered at 15μm, 4.3μm, 2.7μm, and 2μm and water vapor is absorbed in long wavelength bands centered at 71μm, 6.3μm, 2.7μm, 1.87μm and 1.38μm, respectively. The predict absorptions agree with experimental and theoretical results in exponential wide band model. The computed results show the effects of carbon dioxide and water vapor on temperatures in the troposphere.
目次 Table of Contents
論文審定書 i
摘要 ii
Abstract iii
圖次 v
表次 vii
符號說明 viii
第一章 緒論 1
1.1前言 1
1.2文獻回顧 3
1.3研究目的 4
第二章 分析模型與方程式 5
2.1系統模型 5
2.2空氣統御方程式 6
2.3四季模型 7
2.4 擴散方程式與吸收係數計算 9
第三章 驗證與模擬結果分析 19
3.1 網格驗證 19
3.2 二氧化碳與水蒸氣之吸收係數驗證 25
3.2.1 波段總吸收量 25
3.2.2 波段平均吸收係數 28
3.3 實際溫度驗證 30
第四章 結論 31
參考文獻 32
參考文獻 References
[1] D.P.Martin, 1995. " Demonstrating the Greenhouse Effect : Illustrating Variations on an Atmospheric Phenomenon ," from Google Books: http://books.google.com.tw/books?id=L4jtv2mX0iQC&pg=PA57&redir_esc=y#v=onepage&q&f=false
[2] J. F. R. A. Rohde, 2007.Image:Atmospheric Absorption Bands. June 21,2008, fom the World Wide Web:
http://wattsupwiththat.com/2008/06/21/a-window-on-water-vapor-and-planetary-temperature-part-2/
[3] Oklahoma Climatological Survey,2005. Image:Vertical Structure of the Atmosphere, from Oklahoma Climatological Survey:
http://okfirst.mesonet.org/train/meteorology/VertStructure2.html
[4] http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/prs/hght.rxml
[5] J. B. Fourier, 1827 "Mémoire Sur Les Températures Du Globe Terrestre Et Des Espaces Planétaires,". Mémoires de l'Académie Royale des Sciences 7: pp. 569–604.
[6] H.B.De Saussure,Journal de Paris (no. 108) (1874), pp. 475-478.
[7] J. Tyndall, 1861, "On the Absorption and Radiation of Heat by Gases and Vapours and on the Physical Connexion of Radiation, Absorption and Conduction-the Bakerian Lecture, " Phil. Mag., 22, pp. 169-194.
[8] G.Yamamoto, G.Onishi, 2009. "大気中の水蒸気による太陽輻射の吸收," Journal of the Meteorological Society of Japan. Ser. II, Vol. 29 (1951) No. 4, pp. 103-119.
[9] S. Arrhenius, 1896, "On the Influence of Carbonic Acid in the Air Upon the Temperature of the Ground," Philosophical Magazine ,41, pp. 237-76.
[10] G. P. Callendar, 1938, “The Artificial Production of Carbon Dioxide and It’s Influence Climate,” Quarterly J. Royal Meteorological Soc., 64, pp. 223-240.
[11] S. Joseph, 1970, “Numerical Simulation of the Global Circulation,”Global Circulation of the Atmosphere, pp. 24-41.
[12] G. Plass, 1959, " Carbon Dioxide and the Climate," American Scientist, 98(1) , pp. 58-62.
[13] M. F. Modest, " Radiation Heat Transfer, " McGraw-Hill, 1993, New York.
[14] D. K. Edwards, A.Balakrishnan, 1972, “Thermal radiation by combustion gases, " International Journal of Heat and Mass Transfer, Vol. 16, no. 1, pp. 25–40.
[15] J. N. Howard, D.E.Burch, D. Williams 1955, " Infrared Transmission of Synthetic Atmospheres. II. Absorption by Carbon Dioxide, " JOSA, Vol. 46, Issue 4, pp. 237-241.
[16] D. K. EDWARDSt, University of California, Berkeley, California,
Absorption by Infrared Bands of Carbon Dioxide Gas at Elevated Pressures and Temperatures*
[17] G.Yamamoto, G.Onishi, 1949. "近赤外域に於ける水蒸氣の吸収係數," Journal of the Meteorological Society of Japan. Ser. II, Vol. 2, No. 9 P 269-276.
[18] G.Yamamoto, G.Onishi, 1949. "遠赤外域に於る水蒸氣の吸收係數," Journal of the Meteorological Society of Japan. Ser. II, Vol. 27, No. 2, P 52-64.
[19] http://weather.uwyo.edu/upperair/sounding.html
電子全文 Fulltext
本電子全文僅授權使用者為學術研究之目的,進行個人非營利性質之檢索、閱讀、列印。請遵守中華民國著作權法之相關規定,切勿任意重製、散佈、改作、轉貼、播送,以免觸法。
論文使用權限 Thesis access permission:自定論文開放時間 user define
開放時間 Available:
校內 Campus:永不公開 not available
校外 Off-campus:永不公開 not available

您的 IP(校外) 位址是 18.216.251.37
論文開放下載的時間是 校外不公開

Your IP address is 18.216.251.37
This thesis will be available to you on Indicate off-campus access is not available.

紙本論文 Printed copies
紙本論文的公開資訊在102學年度以後相對較為完整。如果需要查詢101學年度以前的紙本論文公開資訊,請聯繫圖資處紙本論文服務櫃台。如有不便之處敬請見諒。
開放時間 available 永不公開 not available

QR Code