2022年常见的天气系统高三一轮复习导学案 .pdf

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1、常见的天气系统一、自主复习1大气中经常发生的阴、晴、风、雨、雪等天气现象，都与天气系统的活动有密切的关系。、和是常见的天气系统。2气团是指在方向上，、等物理性质分布比较均一的大范围空气。在单一气团控制下的天气比较。3冷、暖两种性质不同的气团在移动过程中相遇时，它们之间的倾斜的交界面叫做_ _。锋面与地面相交的线叫做_ _。一般把锋面和锋线统称为。锋面自地面向高空一侧倾斜。4锋面两侧空气的的_ _、_、_、_、等有明显的差别，所以在锋面附近常伴有一系列的_、_、_等天气。4由于冷空气密度_，暖空气密度_，当冷暖气团相遇时，一般是冷气团在锋面_，暖气团在锋面的_。6、在锋面的移动过程中，根据冷暖气

2、团所占的不同，可将锋面分为_、_ _和_ 。7、冷锋是指 _主动向 _移动的锋。冷锋过境时，常出现 _、_、_等天气，过境后，气压_，气温 _，天气 _。冷锋在我国四季皆有，但在半年更常见。符号表示为。8、暖锋是指 _主动向 _ _ 移动的锋。暖锋通常伴有和天气，多为 _性降水。暖锋过境后气温_ _，气压 _ _，天气 _。暖锋在我国的和地区活动频繁。符号表示为。9准静止锋是冷暖气团相当，使锋面来回摆动的锋。初夏，我国地区的“梅雨”就是由它造成的。符号表示为。读图回答问题1锋面特征(1)锋面自地面向高空b_一侧倾斜，其上侧一定是a _。(2)锋面两侧 _、湿度、_差异很大。(3)锋面附近 _变

3、化剧烈。2冷锋、暖锋、准静止锋与天气(1)冷锋过境前：暖气团控制，气温较_，气压较 _。过境时：常出现阴天、_、_、降温等天气现象。过境后：冷气团控制，气温_，气压?_，天气转好。(2)暖锋过境前：?_控制，气温较低，气压较高。过境时：多云和降雨天气，连续性降水或雾。过境后：暖气团控制，气温?_，气压?_，天气?_。(3)准静止锋：冷暖气团势力相当，使锋面来回摆动的锋。二、低压(气旋)、高压(反气旋)与天气1气旋、反气旋与天气天气系统(北半球)低压(气旋)高压(反气旋)气压中心气压低于四周中心气压高于四周水平气流(低空)由四周流向中心由中心流向四周垂直气流?_ 下沉天气状况多阴雨天气多?_天气

4、我国典型的天气夏秋季节影响我国东南沿海地区的?_ 长江流域7、8月份的“?_”；冬季的寒潮；北方文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7

5、文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:C

6、N3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1

7、K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 H

8、Z7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X

9、8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8

10、ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7秋高气爽的天气2.高压脊：从?_延伸出来的狭长区域，好比地形上的山脊。高

11、压或高压脊控制之下，多21_天气。3低压槽：从22_延伸出来的狭长区域，好比地形上的峡谷。低压或低压槽控制之下，多23_天气。二精讲精练考点 1 天气系统特征下图是“我国某地气象站某月18 21 日气温和气压变化图”，读图回答 1 2 题。1此期间过境的天气系统是A冷锋 B反气旋C暖锋 D气旋2图中所示时期，我省大部分地区A低温少雨 B温和多雨 C 炎热干燥 D 炎热多雨读我国某地时段气温变化示意图，回答34 题3.经过该地该时段的天气系统可能是（）A冷锋 B.暖锋C.台风 D.寒潮4.该地太阳能热水器使用效果最差的日期是（）A.12 日 B.4-5日 C.6-7日 D.7-8日考点 2 等压

12、线图的判读读某日 08 时地面天气图和文字信息，回答下题。1058512514530501005 1015 1015 1010 1020 1015 1020 1000 1010 1015 1010 a b 某气象小组学生探讨天气图中ab 天气的空间变化。5.在学生绘制的图中，接近ab 天气实际状况的是（）气温气压风速云量a b A a b B a b C a b D 图 6 的四幅天气图反映了一次寒潮的天气过程。结合图文材料，回答下题文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B

13、5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编

14、码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H

15、4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X

16、3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V

17、10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9

18、H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1

19、F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D76.按照此次寒潮天气发生的过程，四幅天气图由先到后的排序应为（）A.acbd B.b cda C.c bda D.d acb 7据图 6 的四幅天气判断，下列城市的天气状况接近实际的是（）A a-武汉地区晴朗温暖 B b-天津地区大风降温 C c-北京地区雷雨交加 D d-杭州地区阴雨连绵巩固提高1.下列关于锋面与天气的叙述，正

20、确的是（）冷锋过境时，一般出现晴朗天气我国北方夏季暴雨与冷锋活动有关我国冬季寒潮的爆发是冷锋南下时形成的灾害性天气暖锋过境后，气温、气压上升，天气转好A.B.C.D.2、冷锋与暖锋的共同点是（）A都形成连续性降水 B 降水都降在锋前C都是冷气团在下，暖气团在上 D 过境时气温变化明显3.下列四幅冷、暖锋示意图中，A、B、C、D 四地大致位于同一纬度，此时气温最低、气压最高的地点是（不考虑地形和海陆因素）（）4.上海某年3 月 8 日的最高气温比3 月 9 日的最高气温高出8，其原因可能是（）A.9 日有寒潮到达B.9 日有一高压系统控制上海，云量多，大气反射作用增强，近地面气温低C.9 日受江

21、淮准静止锋的影响，阴雨连绵D.9 日受一台风系统的影响，出现阴雨天气右图中的虚线为北半球中纬地区的低压槽线，完成56 题。5.如果槽线东北端的气压低于西南端，则槽线西北和东南的风向分别为()A.西北、东南 B.西北、西南C.东北、东南 D.东北、西南6.如果槽线东北端的气压高于西南端，该类槽线夏天出现在我国华北地区时，最可能出现()A.暴雨和冰雹天气 B.扬沙或者沙尘暴天气C.连绵的阴雨天气 D.晴朗天气文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1

22、K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 H

23、Z7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X

24、8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8

25、ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R

26、10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7

27、文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:C

28、N3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D77.读“锋面天气示意图”回答下列问题：（1）甲城此时天气特征，乙城此时天气特征。(2)假设甲城、乙城之间各相距480 千米，锋面移动速度为20 千米/小时，24 小时后，乙城天气特征。丙城天气特征，此时锋面是锋面。8.读“北半球某地等压线分布图”（图 1）和“锋面示意图”（图 2）及表 1 内容，完成下列问题。图 1 图 2 表 1 日期日均温（）气压（百帕

29、）天气现象1 月 1 日15 1000.3 晴，12 级偏北风1 月 3 日2 1 000.5 中雪，6 8 级偏北风1 月 5 日-2 1028.0 晴，23 级偏北风（1）图 1 中 A、B、C、D四处所绘箭头能正确表示当地风向的是_。（2）图 1 中 A、B两处相比，风力较大的是，原因是_。（3）图 1 中 M、N 两条线附近，将可能出现锋面的是_，该锋面与图2 甲、乙两图中的哪一幅图相符？_。该锋面过境时，一般出现_天气。文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D

30、7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:

31、CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P

32、1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3

33、HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10

34、X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8

35、 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7文档编码:CN3H4P1K9X3 HZ7V10X8V9H8 ZZ1F2R10B5D7