地理必修一知识点复习.pdf

北京市知春里中学地理必修一复习提纲地理会考第页共 11 页1 说出天体系统的层次、地球在天体系统中的位置、太阳系概况。说明地球是太阳系中一颗既普通又特殊的行星1、天体系统的层次：2、太阳系概况：组成：八大行星的由里向外的顺序是水星、金星、地球、火星（类地行星）、木星、土星（巨行星）、天王星、海王星（远日行星）；其中小行星带是位于火星 和木星 之间。3、地球的普通性：与其它行星相比，地球在（物理性质）方面和（运动特征“同向性、共面性、近圆性”）方面是一颗普通的行星4、地球是太阳系中既普通又特殊的行星，其特殊性在于有生命存在。其原因是：（1）外部原因（2）内部原因:（温、气、水）.安全 的宇宙环境.日地距离适中适宜的温度.稳定 的光照条件.体积质量适中可供呼吸的大气.自转和公转周期适中温度变化小.地球上有 液态水 的存在说出太阳活动的主要类型；说出太阳活动对地球的影响、太阳辐射对地球的影响5、（1）太阳辐射：太阳源源不断地以电磁波 的形式向四周放射能量。太阳辐射的能量来源：太阳内部的核聚变反应（2）太阳辐射对地球的影响：太阳辐射为地球提供光和热；维持地表温度，为地球上的水循环、大气运动和生物活动提供能量（3）太阳活动的标志是黑子 和耀斑，分别出现在太阳外部圈层的光球层 和色球层，活动周期 约 11 年。（4）太阳活动对地球的影响主要有：黑子：影响地球气候：黑子的数量变化与降水的年际变化有相关性耀斑：扰乱地球电离层，干扰 无线电短波通信耀斑：干扰地球磁场，产生 磁暴 和极光。说出自转、公转的特点；分析说明地球自转和公转的关系；分析说明地球运动的地理意义：昼夜交替、地方时、物体水平运动方向的偏转、正午太阳高度的变化、昼夜长短的变化、四季的更替6、（1）自转和公转的特点方向周期角速度线速度自转自西向东，北逆南顺真正：恒星日日常：太阳日除两极点外，都是 15/小时规律：从赤道向两极递减公转自西向东真正：恒星年日常：回归年规律：近日点（1 月初）快，远日点（7 月初）慢【1 近快；7 远慢】（2）自转和公转的关系-产生 黄赤交角（23?26 ）（地轴和黄道面的夹角：66?34）黄赤交角：地球自转轨道面（赤道面）和地球公转轨道面（黄道面）之间的夹角。北京市知春里中学地理必修一复习提纲地理会考第页共 11 页2 太阳直射点的回归运动原因：黄赤交角（23?26 ）的存在。（直射次数：南北回归线之间一年2 次直射；南北回归线上一年1 次直射，南北回归线以南以北无直射）（3）自转的地理意义1：昼夜更替：晨昏线是 昼夜半球 的分界线。晨昏线的 判断方法：顺着地球自转方向，由夜半球进入昼半球所经过的晨昏线部分为 晨线；由昼半球进入夜半球所经过的晨昏线部分为昏线。与太阳高度的关系：晨昏线上太阳高度是0 度。夜半球太阳高度小于0 度，昼半球太阳高度大于0 度与太阳光线的关系：太阳光线与晨昏线始终垂直，太阳直射光线 垂直平分 晨昏线与纬线的关系：晨昏线把纬线分成昼弧 和夜弧，昼弧中点为12 点，夜弧中点为24 点或 0 点。晨赤交点为6 点，昏赤交点为18 点（4）自转的地理意义2：地方时全球共分为24 个时区。经度每隔15 度，地方时相差1 小时。1 度=4 分钟计算方法：东加西减。北京时间是 东八区 的区时。国际标准时间（世界时）是中时区 的区时。（5）自转的地理意义3：地转偏向力规律：北半球 右偏，南半球 左偏，赤道 不偏。（6）自转和公转共同的地理意义1：正午太阳高度的变化规律：离太阳直射点越近，正午太阳高度角越大，反之亦然。纬度变化（同时间不同纬度）规律：由直射纬度向南北两侧递减。春分（3.21）夏至（6.22）秋分（9.23）冬至（12.22）太阳直射纬度赤道北回归线赤道南回归线纬度变化规律从赤道向南北两侧递减从北回归线向南北两侧递减从赤道向南北两侧递减从南回归线向南北两侧递减季节变化（同纬度不同时间）规律：夏至日：北回归线及其 以北地区，正午太阳高度角达全年最大值；南半球 各地达到最小值。冬至日：南回归线及其 以南地区，正午太阳高度角达全年最大值；北半球 各地达到最小值。春秋分：赤道上正午太阳高度角达最大值，其他地区介于最大值和最小值之间全球各地正午时，物体影子的朝向和长短变化规律：长短：正午太阳高度角越大，影子越短，反之亦然。朝向：位于直射点北侧的地区，影子朝北；位于直射点南侧的地区，影子朝南；直射无影。节气时间（前后）直射点位置移动方向春分3 月 21 日赤道向北夏至6 月 22 日北回归线向南秋分9 月 23 日赤道向南冬至12 月 22 日南回归线向北晨昏线特点文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3北京市知春里中学地理必修一复习提纲地理会考第页共 11 页3（7）自转和公转共同的地理意义2：昼夜长短的变化太阳直射哪个半球哪个半球昼长夜短随季节变化（北半球）（8）天文四季的划分依据：昼夜长短和正午太阳高度角季节变化按气候划分：3、4、5 月为春季、6、7、8 月为夏季、9、10、11 月为秋季、12、1、2 月为冬季。（9）五带的划分：热带（南、北回归线之间）：有太阳直射现象，无极昼极夜现象北温带和南温带（回归线和极圈之间）：无太阳直射现象，无极昼极夜现象北寒带和南寒带（极圈以北、以南）：无太阳直射现象，有极昼极夜现象说出地球的各个圈层名称，地球内部圈层的结构，岩石圈的组成与特点外部圈层：位于地表以上，包括大气圈、水圈、生物圈7、地球圈层结构内部圈层：位于地表以下，包括地壳、地幔、地核（划分依据：地震波传播速度）岩石圈：组成：包括地壳全部、软流层以上的地幔部分（上地幔顶部）特点：岩石圈物质可循环大气圈：文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3北京市知春里中学地理必修一复习提纲地理会考第页共 11 页4 说出大气的热量来源；运用图表说明大气受热过程；分析大气的垂直运动和水平运动的成因；运用大气热力环流原理，分析一些地理现象8、大气受热过程（记住过程、环节）（1）太阳辐射 是地球大气的 最根本 的能量来源，地面辐射 是近地面大气的 最主要、直接 的热源。（2）大气对太阳辐射的削弱作用：作用形式参与作用的大气成分波长范围作用特点吸收臭氧（平流层）紫外线强烈吸收，有选择性，大部分可见光可穿透水汽、二氧化碳（对流层）红外线反射云层、尘埃各种波长同样被反射无选择性，反射光呈白色散射空气分子、微小尘埃蓝色光最易被散射向四面八方散射，有选择性（3）大气对地面 的保温作用：地面辐射几乎全部被大气中的二氧化碳和水汽吸收大气向外放出热量，其中大部分朝向地面，与地面辐射方向相反，被称作大气逆辐射与大气的保温作用有关的现象现象成因夜晚多云时气温比晴天高夜晚多云时大气逆辐射强，地面散失热量少人造烟雾的防冻效果可增强大气逆辐射，提高地面温度晚秋或寒秋，霜冻出现在晴朗夜晚及“十雾九晴”晴朗夜晚，大气逆辐射弱，气温低，易现霜冻及雾等天气现象9、大气运动（空间尺度：小-热力环流；大 大气环流）（1）热力环流：由 地面冷热不均 而形成的空气环流原理：如果某地受热，近地面大气就会膨胀上升，到上空聚集起来，使上空空气密度增大（比同一水平面上其他地区相比），气压增高，形成高压区；某地周围空气冷却收缩下沉，上空空气密度减少，气压降低，形成低压区。（垂直运动）于是，上空的空气便从气压高的地区向气压低的地区扩散。受热地区空气上升后，近地面空气密度减小，气压比周围地区都低，形成低压区；冷却的地区因有下沉气流，近地面的空气密度增大，形成高压区。这样近地面空气从气压高的地区流回气压低的地区（水平运动），以补充受热地上升的空气。（先垂直运动，后水平运动）文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3北京市知春里中学地理必修一复习提纲地理会考第页共 11 页5 示意图利用原理分析地理现象海陆风城市风山谷风（2）风（形成的 直接原因：大气的水平运动。）理想状态下的风：只受水平气压梯度力的影响：风向与等压线垂直高空大气风向是地转偏向力和水平气压剃度力的共同作用的结果，风向最终与等压线平行。近地面大气风向是摩擦力、地转偏向力和水平气压剃度力的共同作用的结果，风向最终与等压线斜交。风向：北半球右偏、南半球左偏（受地转偏向力影响）。风速：等压线密集-水平气压梯度力大-风速大；等压线稀疏-水平气压梯度力小-风速小说出全球气压带与风带的形成和分布，说明气压带、风带的分布、移动规律及对气候的影响说明北半球冬、夏季高、低压中心的分布（3）大气环流：使高低纬度之间、海陆分布之间的水分和热量得到交换，调整了全球的水热分布。大气环流与气压带、风带的形成（根本原因：高低纬度间受热不均）考虑因素：高低纬受热不均-单圈环流考虑因素：高低纬受热不均+地转偏向力-三圈环流三圈环流所对应的地面气压带风带全球共有 7 个气压带，6 个风带，其中有3 个低气压带，4 个高压带，相间分布考虑因素：纬度位置不同+地转偏向力+太阳直射点移动导致 气压带风带随季节而移动（课本39 页）规律：北半球，夏季北移，冬季 南移。考虑因素纬度位置不同+地转偏向力+太阳直射点移动+海陆分布和地形起伏-季风环流文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3北京市知春里中学地理必修一复习提纲地理会考第页共 11 页6（4）季风环流夏季 300N 附近原为副热带高压带，因陆地增温比海洋快所以气温高，空气膨胀上升，形成热低压亚洲大陆：亚洲（印度）低压，切断了副热带高压带，使高压保留在海洋上，太平洋形成夏威夷高压冬季 600 N 附近原为副极地低压带，因陆地降温比海洋快所以气温低，空气收缩下沉，形成冷高压 亚洲大陆：亚洲（蒙古）高压，切断了副极地低气压带，使低压保留在海洋上，太平洋形成阿留申低压。东亚季风：风向：冬季 西北 风，夏季 东南 风。成因：海陆热力性质差异。南亚季风：风向：冬季 东北 风，夏季 西南 风。成因：海陆热力性质差异气压带风带季节移动(东南信风越过赤道变为西南风)（5）大气环流（包括季风环流）对气候的影响气候类型成因分布规律气候特征热带雨林气候受赤道低气压带控制，盛行上升气流赤道附近终年高温多雨热带沙漠气候受副热带高气压带控制，下沉气流南北纬 30 o左右终年炎热干燥温带海洋气候西风带控制纬度 40o60o之间的大陆西岸终年温和湿润地中海气候受副热带高气压带和西风带交替控制南北纬 30o40o大陆西岸夏季炎热少雨冬季温和多雨亚热带季风气候海陆热力性质差异南北纬 25o 35o大陆东岸夏季高温多雨冬季低温少雨温带季风气候海陆热力性质差异南北纬 35o 55o大陆东岸夏季高温多雨冬季寒冷干燥分析锋面、低压中心（气旋）、高压中心（反气旋）等天气系统的特点；判读简易天气系统图；说明影响我国的主要天气系统。10、天气系统（1）锋面系统文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3北京市知春里中学地理必修一复习提纲地理会考第页共 11 页7（2）气旋系统中心气压垂直方向水平运动方向天气状况气旋低气压辐合上升北逆南顺多阴雨天气反气旋高气压辐散下降北顺南逆天气晴朗结合水循环示意图，说出水循环的过程和主要环节；说明水循环的地理意义11、水循环（1）认识水循环的各个环节的名称。海陆间循环的各环节蒸发、水汽输送、降水、下渗、径流（地表、地下）（2）水循环的地理意义联系四大圈层，调节水量平衡，更新陆地淡水调节不同纬度间热量平衡实现物质迁移塑造地表形态运用世界洋流分布示意图，归纳出世界洋流分布规律；说明洋流对地理环境的影响12、洋流（1）分类暖流：低纬向高纬寒流：高纬向低纬（2）分布规律（3）影响气候：调节全球热量平衡；暖流增温增湿、寒流降温减湿生物：寒暖流交汇出现大渔场（北海、北海道、纽芬兰）；上升补偿流也会出现渔场（秘鲁渔场）航行：顺流加速、逆流减速；海雾影响航行（减速）污染：减小污染浓度、扩大污染面积文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5 ZH2N1L8B10H3文档编码:CR10F9W5N3R3 HO9N9S3R8H5