大学地理科学专业气象学与气候学期末考试复习要点及试题.pdf

学习好资料欢迎下载气象学与气候学期末考试要点及试题*教学要点及试题：绪论重点：1.气象学、气候学、天气学的概念及所研究对象2.本学科与其他部门地理、区域地理学的关系一.选择题：1.（）是气象学的研究范围a.风b.雨c.冷却d.台风e.雪f.龙卷g.蒸发2.（）是天气学的研究范围a.霜b.台风c.凝结d.龙卷e.温度3.气象学与气候学的关系是（）a.气候学包含气象学b.气象学是气候学的基础c.气象学和气候学是独立的二、填空题：.气象学是研究发生于（）中的一切（）和（）的科学，以（）为研究对象。用（）表示。2.天气学是研究（）不同的区域内所发生的（）的（）及（）规律，并应用这些规律（）的科学，以（）为研究对象。3.天气是指在某一地区，（）或（）内大气中的（）和天气现象的综合。4.气候学是研究地球上的（）、（）、（）规律的科学，以（）为研究对象。5.气候是指在（）、（）、（）和（）长时间相互作用下，在某一时段内大量（）的综合。6.气象学是气候学的（）基础，天气学是气候学的（）基础，气候学是（）和（）的综合。三.问答题：1.天气与气候的区别和联系？2.本学科在实际中有哪些方面的应用？3.根据以前学过的专业课和日常生活讲述一、二个有关气象或气候应用的小例子。第一章 大气概述学习好资料欢迎下载重点:1.干洁空气的概念、成分及作用2.对流层、平流层的特点及成因#1-1 大气的组成要求:1.熟练掌握干洁空气的概念、成分及作用2.掌握大气中的水汽、固体杂质的来源及分布3.理解固体杂质、液体微粒的作用一.填空题：1.大气中物质的存在有三种形态，即（）、（）、（）2.地面 90km的范围中大气的组成是（）、（）、（）。3.大气是（）的混合物，主要成分是（），此外还有含量不定的（）、（）微粒。4.干空气是指不包含（）、（）、（）的大气。其含量占整个大气的（）%，主要成分是（、），占干空气的（）%；次要成分是（、），占干空气的（）%。5.90km以下大气的分子量是（），90km以上大气主要成分是（、）。6.氧来源于水的离解，其方程式是（）；光合作用的方程式是（）臭氧分解的方程式是（）。7.大气中的氧参与有机物的（）、（）、（）过程。8.CO2在大气中的含量比为（）%，主要集中于（）km 以下，具有（）分布特点。参与植物的（）作用，能吸收（）和（）的长波辐射。9.O3的作用是（），使大气增暖，另一个作用就是（）。10.大气中的水汽量随高度而（），随纬度而（）。11.水汽是大气中唯一具有（）变化的气体，可以吸收来自于地表的（）辐射，可以放出（）辐射。12.大气中的固体杂质主要集中于（）。并具有（）分布特点，其作用是（）和（）。13.液体微粒是指悬浮于大气中的（）、（）和（）等水汽凝结物。二.选择题：文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 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HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8学习好资料欢迎下载1.0-90km范围内，大气是由（）组成的a.干洁空气b.O2 c.CO2 d.水汽e.杂质与微粒f.杂质2.干空气是指不包含（）的大气。a.水汽b.杂质c.惰性气体d.液体微粒3.干空气占整个空气质量的（）%。a.99.97 b.99.96 c.99.98 d.99.99 4.90km以上，大气的主要成分是（）a.臭氧b.氮c.氧d.氩5.()可以产生大气中的氧。a.离子交换b.光合作用c.闪电d.水的电解6.氮的作用是（）a.参与有机物的分解b.缓解氧化c.吸收长波辐射d.肥料7.臭氧在（）km 处量最多a.20-30 b.20-25 c.15-25 8.大气中的固体杂质作用是（）a.破坏能见度b.减弱地面长波辐射c.水汽的凝结核心9.（）可以吸收地面的长波辐射a.臭氧b.水汽c.二氧化碳d.固体杂质e.氮和氧三.判断并改错：1.大气底层臭氧量少，是因为氧原子少。（）2.大气中的气体由于临界温压高，因此都以气体形态存在。（）3.大气中的水汽其容积变化范围是0-4%（）四.简答题：1.二氧化碳的来源及作用2.臭氧在高空中的分布特点及原因、作用3.水汽在大气中的作用五.作图题：臭氧在大气中的分布曲线#1-2 大气的垂直结构要求：文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 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的大气中质量仅占（）%，大气中的（）和（）随高度而逐渐变小。2.气象学规定在大气中有（）出现的最大高度，称为（），其高度为（）km。密度法规定的大气上界高度为（）km。3.在垂直方向上根据大气（）、（）、（）和（）将大气分为（）个层次。4.对流层的上界因纬度而不同，低纬（），高纬（）；又因季节而不同，夏季（），冬季（）。在本层中集中了（）大气，（）水汽。5.对流层中的平均温度递减率为（）/100m。6.在对流层中按（）和（）分为三层。最下层称为（），范围是（）km。7.（）层又称电离层，具有（）的能力。二.选择题：1.物理上界的高度是（）km。a.2000 b.1000 c.1200 d.3000-4000 2.密度法规定的大气上界的电子浓度是（）个/cm3，质点浓度是（）个/cm3，高度是（）km。a.10-102 b.102-10 3 c.103-104a.1 b.2 c.3 a.2000 b.3000 c.2000-3000 3.大气的垂直分层根据（）a.大气温度b.水汽c.大气成分d.垂直运动状况4.对流层在低纬的上界高度是（）km a.13-14 b.15-16 c.17-18 5.在对流层中，因（）而分（）层a.气温b.气流c.天气现象d.水汽分布a.3 b.2 c.4 6.对流层中（）层是天气预报的重要层次a.1 b.2 c.3 d.4 7.平流层中的温度升高是因为（）文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8学习好资料欢迎下载a.臭氧多b.氮、氧分子多c.空气运动快8.中间层温度随高度而（），原因是（）a.降低b.升度c.不变a.臭氧b.氮、氧分子c.太阳辐射9.在中间层的（）km 处，仅白天出现一个电离D 层a.60-70 b.60-80 c.60-90 10.()层具有无线电波的反射能力a.中间层b.平流层c.暖层d.散逸层11.在大气的垂直五层中，有（）个层次温度随高度而升高a.2 b.3 c.4 12.()层中偶尔会出现贝母云a.对流层b.平流层c.中间层d.暖层三.判断并改错：1.对流层上界高度随季节而有变化，夏季低，冬季高。（）2.对流层中温度、湿度分布不均是因为地表性质不同而产生的()3 在对流层和平流层之间大约2km 的层次中有一个温度随高度升高变小或不变的过渡层。（）4平流层中水汽、尘埃含量少，是因为此层远离地表。(）5中间层又称高空对流层，有时能观测到夜光云。（）四.问答题：1.在对流层中温度随高度变化的特点是什么？为什么？2.在对流层中水平方向上温度、湿度有何特点？为什么？3.在对流层中空气运动的特点是什么？为什么？4.平流层中温度随高度有何变化特点？为什么？5.在平流层中空气运动的特点是什么？为什么？6.平流层中为什么水汽、尘埃含量少？7.中间层温度随高度分布的特点是什么？为什么？8.暖层中温度的分布特点是什么？为什么？9.暖层中空气处于什么状态？为什么？10.为什么低纬对流层顶高度高，而高纬对流层顶高度低？文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8学习好资料欢迎下载五.作图题：画出大气垂直结构中温度随高度的变化曲线#1-3大气的基本物理特性要求:1.熟练掌握各主要气象要素的定义、单位及公式2.掌握干空气、湿空气的状态方程3.能利用仪器准确测定主要的气象要素一.填充题：1.表示大气状态的物理量，称为（）2.气压的大小主要决定于（）3.在气象学上，气压的单位是（）、（）、（）4.1mb=（）达因/cm2=()帕5.标准大气压是指在（）的海平面上，温度为（）时，所测到的水银柱的为高度为（）的大气压强。5.1mmhg=（）mb，1mb=（）mmhg 6.气温表示大气（）程度的物理量，单位有（）、（）和（）7.气温高低的实质就是（）8.摄氏温标与华氏温标换算的表达式是（）9.华氏温标与摄氏温标换算的表达式是（）10.摄氏温标与绝对温标换算的表达式是（）11.湿度是指表示大气（）程度的物理量12.绝对湿度的单位是（）和（）13.比湿的表达式是（）14.相对湿度是指空气中的（）和同温度下的（）的百分比，表达式是（）15.饱和差的表达式是（）16.在表示空气湿度的物理量中，其中表示空气中水汽含量的物理量有（），表示空气距离饱和程度的物理量有（）17.气流运动的物理量是（），地面风用（）表示，高空风用（）表示，NNE 表示（）风，SSW（）风18.空气的状态用（、）表示19.理想气体的状态方程是（）20.干空气状态方程的表达式是（）文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 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ZY5T4F8E6Z8学习好资料欢迎下载二.选择题：1.1 个标准大气压=（）mb a.1000 b.1013 c.1013.5 2.水汽的比气体常数（Rw=1.608Rd）比干空气（）a.小b.相等c.大三.是非题：1.相对湿度数值愈小，表示当时空气饱和程度愈远（）2.在气压不变的情况下，Td只与空气中的水汽含水量量有关（）3.露点表示空气中水汽含量的多少，其值愈高水汽量愈多(）4.大气中是产生蒸发，还是凝结，主要取决于空气的含水量（）5.大气中水汽凝结量的多少，主要决定于空气是否饱和（）第二章大气的热能和温度重点:1.太阳辐射及太阳常数2.干绝热直减率和湿绝热直减率3.全球水平气温的分布特点4.如何判别大气稳定度难点：1.大气稳定度能量的判别2.乱流逆温的形成过程#2-1 太阳辐射要求：1 熟练掌握太阳辐射、太阳辐射光谱、太阳常数的概念，大气对太阳辐射吸收的特点，影响直接辐射的因素文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 ZY5T4F8E6Z8文档编码:CV5I4J3B10F5 HH8Y9I10X7T7 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