在本文中，本研究探討觀點在於說明在高度小於十公里（對流層）之水蒸氣與二氧化碳對溫度和熱傳遞可能會造成之變化以及影響。並且證明解釋現實的溫度、壓力以及氣體濃度...等等輻射影響因子對輻射特性之影響。
本文將對大氣中可能遭遇之熱傳問題進行系統地評估以及假設。為了簡化問題，本模擬程式將熱傳方程式假定為一維，並且只純粹探討傳導以及輻射的模式。太陽光可穿過大氣層之波長範圍介於短波長範圍接近可見光（波長約在0.4至0.7μm ）的區間，然後其穿過之太陽光部分被空氣吸收、反射以及被地表吸收。地表吸收太陽光造成地表溫度上升，然後以黑體方式發散長波長輻射。探討水蒸氣與二氧化碳之吸收與穿透方面，水蒸氣在長波範圍(8至12μm )部分穿透、吸收（穿透為主）；二氧化碳具有三個長波範圍吸收波段分別以15μm、10.4μm、9.4 μm為中心尖峰。
根據數值分析出來之結果，本研究可以證明水蒸氣以及二氧化碳為造成溫度差異高達攝氏2至5度最重要的影響因子。

The effects of water vapor and carbon dioxide on temperature and heat transfer in the troposphere layer, which is less than the altitude of 10 km, in the atmosphere are presented in this work. Accounting for realistic temperature- and pressure- or concentration-dependent radiative properties, this work systematically evaluates heat transfer encountered in atmosphere. For simplicity, the heat transfer is assumed to be one-dimensional and pure conduction and radiation modes. The solar irradiation penetrates through the atmosphere within its short wavelength range near around visible range between 0.4-0.7 μm , and absorbed and reflected by the earth ground with a black body property. The ground emits radiation in longwave range. Water vapor is transparent to longwave range 8-12 μm , whereas carbon dioxide is absorbed in three long wavelength bands centered at 15, 10.4 and 9.4 μm , respectively. The computed results quantitatively show that water vapor and carbon dioxide are the most important factors affecting temperature difference around 2 and 5 Celsius degrees.

目錄
頁次
謝誌 Ⅰ
目錄 Ⅱ
圖目錄 Ⅳ
符號說明 Ⅵ
中文摘要 Ⅷ
英文摘要 Ⅸ
第一章　緒論 1
1.1 前言與文獻回顧 1
1.2 研究動機 4
1.3 研究目的 6
1.4 本文架構 7
第二章　系統模型之假設與理論分析 8
2.1 理論模型與假設 8
2.2 在空氣中之熱方程式 10
2.3 在地殼表面的熱方程式 14
2.4 邊界條件 15
第三章　結果與討論 19
3.1 印證實驗以及模擬數據 20
3.2 現實大氣模擬結果 24
第四章　結論 38
參考文獻 39

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