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研究生:李杰
研究生(外文):Chieh Li
論文名稱:大氣對流層內水蒸氣及二氧化碳之輻射吸收及溫度變化之影響
論文名稱(外文):The Effect of the Water Vapor and Carbon Dioxide on the Radiation Absorption and Temperature Profile in Troposphere
指導教授:魏蓬生
指導教授(外文):Peng-Sheng Wei
學位類別:碩士
校院名稱:國立中山大學
系所名稱:機械與機電工程學系研究所
學門:工程學門
學類:機械工程學類
論文種類:學術論文
論文出版年:2013
畢業學年度:101
語文別:中文
論文頁數:96
中文關鍵詞:輻射熱傳導對流層溫室氣體溫室效應二氧化碳水蒸氣全球暖化吸收係數
外文關鍵詞:water vaporradiative heat transferabsorption coefficientcarbon dioxidegreenhouse gasesclimate changegreenhouse effectsglobal warming
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本研究主要探討垂直高度十公里內之對流層中水蒸氣及二氧化碳對大氣溫度及熱傳導之影響,根據真實溫度、壓力及濃度和溫室氣體輻射性質之關係有系統地提出大氣熱流模擬計算。
為了簡化數值運算,本研究將大氣模型假設為單純熱傳導及輻射之一維系統。太陽將能量以紫外線(7%)、可見光(44%)、及紅外線(37%)傳入地球[3],部分短波除了可見光(0.4 μm 至0.7 μm)可穿透至對流層,大部分均在對流層頂(Tropopause)被吸收或反射,而在對流層內自地表所散發的長波熱輻射則多被溫室氣體如水蒸氣及二氧化碳等所吸收。被吸收之能量會上下兩向再次被輻射,而向下的輻射則會被地球表面所吸收,進而導致溫度的上升,故水蒸氣及二氧化碳為氣候暖化一個很重要的因素。其中二氧化碳之濃度更是逐年提升,相對於水蒸氣存在周期八至十天而言,其周期是以百年計算,故影響日益加劇,現今研究多將二氧化碳列為主要溫室氣體。
本研究主要對水蒸氣及二氧化碳作模擬,其結果顯示此兩種氣體可造成大氣溫度差異達2℃~5℃,對於溫室效應而言有著顯著的影響。
The work on this paper focus on the effect of the water vapor and carbon dioxide on the absorption of atmospheric radiation and the temperature within the troposphere (10km above the ground), which is based on the realistic temperature- and pressure- or concentration-dependent radiative properties. And for simplicity, this model is assumed one-dimension and only concerning about the conduction and radiation.
As we know, the earth receives energy from the sun in the form UV, visible light, and near infrared radiation. And virtually all wave below 290 nm is absorbed at tropopause (top of the troposphere), and the wave between 300 nm and 800 nm is weakly absorbed and transmitted into the troposphere. Some of them are absorbed by the land and ocean, about 50%. Then the earth surface radiates the energy back in the form of far infrared thermal radiation, which is mostly absorbed by the atmosphere. Those absorbed far IR thermal radiation is re-radiated both upwards and downwards, and the downwards part is absorbed by the earth surface, which leads to a raising temperature. As a result, the influence of water vapor and carbon dioxide on global warming is growing day by day. Although the water vapor absorbs most of the infrared emitted by the ground, yet it got a shorter period about 8 days. Comparing to that, the concentration of carbon dioxide is increasing gradually since the industry revolution due to the anthropogenic emission like burning fossil fuel and deforestation .That’s why recent surveys of global warming all list Carbon dioxide as the main greenhouse gases.
The computed results in this work quantitatively show that water vapor and carbon dioxide play an important role on affecting the temperature difference about 2 to 5 Celsius degree and therefore remind us of taking notice of the global warming.
目錄
頁次
論文審定書 i
謝誌 ii
中文摘要 iii
Abstract iv
目錄 vi
圖次 viii
符號說明 xi
第一章 緒論 1
1-1前言 1
1-2文獻回顧 4
1-3研究目的 5
第二章 分析模型與假設 6
2-1模型建立 6
2-2空氣統御方程式 8
2-3擴散方程式 11
2-4 Exponential Wide Band Model 之吸收係數驗證 33
第三章 結果與討論 41
3-1 Picket Fence Model溫度模擬 41
3-2 Exponential Wide Band Model溫度模擬 48
3-3 Picket Fence Model 與Exponential Wide Band Model吸收係數比較 51
第四章 結論 57
附錄一 二氧化碳各波段總吸收量驗證數據 58
附錄二 水蒸氣各波段之波數吸收係數驗證數據 66
附錄三 Gauss’ Formula, Arbitrary Interval 77
參考文獻 78
[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] From Encyclopaedia Britannica, 1997.Image:Atmospheric Pressure and
Altitude.April 12, 2008, fom the World Wide Web:
http://fiziknota.blogspot.com/2008/04/atmospheric-pressure-pressure-and-
altitude.html
[5] 24小時太陽輻射量。香港天文台。民國102年6月11號。取自http://www.hko.gov.hk/wxinfo/ts/display_element_solar_c.htm
[6] J. B. Fourier, 1827 "Mémoire Sur Les Températures Du Globe Terrestre Et Des Espaces Planétaires,". Mémoires de l''Académie Royale des Sciences 7: 569–604.
[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, 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 P 103-119
[9] S. Arrhenius, 1896, "On the Influence of Carbonic Acid in the Air Upon the Temperature of the Ground," Philosophical Magazine ,41, 237-76
[10] G. Plass, 1959, " Carbon Dioxide and the Climate," American Scientist, 98(1) 58-62.
[11] Intergovernmental Panel on Climate Change (IPCC), 2007 "Fourth Assessment Report(AR4) Working Group I(WGI) "
[12] 地球氣候系統(無日期)。中央氣象局。民102年6月25日,取自:
http://www.cwb.gov.tw/
[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] 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
[17] 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
[18] Upper air data, university of Wyoming, Aug 15, 2011, http://weather.uwyo.edu/upperair/sounding.html
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