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110年 - 110 國立臺灣大學_碩士班招生考試_大氣科學研究所甲組:氣候學#100334
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3. Consider the physical processes in the Hadley circulation. (total 25 points]
c. Please discuss how convection may change under the global warming scenario (Discuss s one potential mechanism in detail). [5pt]
相關申論題
a. the heating (radiative and latent) and circulation in the tropical atmosphere [10pt]
#419869
b. the SST distribution (equatorial warm pool and cold tongue. coastal water in the eastern and western boundary of Pacific) [10pt]
#419870
c. the thermocline (D20) distribution [5pt]
#419871
d. the upper ocean circulation (Ekman and geostrophic currents) [5pt]
#419872
a. Mark on Fig. 2 where convergence and divergence occurs and describe concisely the Walker and Hadley circulation based on the figure and dynamic arguments. [10pt]
#419873
b. Describe qualitatively the changes in SST. wind. D20. and precipitation from the climatology shown in Fig. 1 [10pt]
#419874
a. Sketch the vertical structure that represents the environment of the deep convection region in terms of moist static energy (h), saturation molst static energy (h"), and dry static energy (s) from the surface to the bottom of the stratosphere. Be careful about the detailed relationship between the state variables and their quantitative values (in terms of temperature [K). [10pt]
#419875
b. Same as a), sketch the vertical structure for the environment of the shallow convection region. [10pt)
#419876
a. Starting from the moist static energy budget and moisture budget, write down all of the energetic terms (c:g. energy luxes) that would affect globally averaged dry static energy. Be clear about the definition of positive and negative signs. [10ptl
#419878
b. Under global warming, deep tropical high clouds tend to risc and maintain a similar temperature. With the help of a.), discussed how raising high clouds with global warming in deep tropics affects global mcan precipitation. [5pt]
#419879
相關試卷
110年 - 110 國立臺灣大學_碩士班招生考試_大氣科學研究所甲組:氣候學#100334
110年 · #100334
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