地球公转产生的地理意义正午太阳高度角复习教案.pdf
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1、地球公转产生的地理意义昼夜长短的变化;正午太阳高度角的变化;四季和五带的形成回顾:描述四个时间段南北半球昼夜长短变化情况正午太阳高度角1.概念:一日内最大的太阳高度2.公式 H=90?-|-|表示所求地纬度,表示太阳直射点纬度两地纬度差多少正午太阳高度就差多少3.规律:正午太阳高度角自太阳直射点向南北两侧递减。离太阳直射点越近,正午太阳高度角越大。夏至日正午太阳高度夏至日,太阳直射北回归线,北回归线及其以北各纬度,正午太阳高度达到一年中最大值,南半球各纬度,达一年中最小值。冬至日正午太阳高度冬至日,太阳直射南回归线,南回归线及其以南各纬度,正午太阳高度达到一年中最大值,北半球各纬度,达一年中最
2、小值。1)夏至日北极点正午太阳高度为多少?2326 2)冬至日南极点正午太阳高度为多少?2326 3)当太阳直射20N 时,北极点正午太阳高度为多少?204)夏至日,冬至日赤道上正午太阳高度分别为多少?6634 6634 5)当太阳直射20N 时,赤道上正午太阳高度为多少?806)一年中,南北极点正午太阳高度的变化范围?0-2326 7)一年中,赤道上正午太阳高度的变化范围?90-6634 在一天中,南北两极的太阳高度角为恒值。4.知识运用根据正午太阳高度判断地理位置:例 1:下列三图中a、b 为两至日正午太阳高度,判断三地的地理位置南北回归线之间地区北回归线以北地区南回归线以南地区B 例 2
3、.读图回答:(1)甲和乙中分别反映纬度较高的曲线是A.B.C.D.D(2)有关四地的叙述错误的是A.地 一 年 中 只 有 一 次 太 阳 直 射 的 机 会B.以 上 四 个 地 点 都 位 于 北 半 球C.地位于北纬45D.地在夏至的时候正午太阳高度为901.下图中,横坐标为地球自转线速度,纵坐标为不同纬度四点某日正午太阳高度。D(1)图中四个地点纬度由低到高的排列是()A abcd B abdc C dcab D cdba B(2)图中四个地点按昼长时间由长到短依次是()A abcd B adcb C badc D dabc 春分夏至秋分冬至春分90450正午太阳高度春分夏至秋分冬至春
4、分昼长(小时)24 12 0 文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ
5、4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J
6、6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编
7、码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D
8、4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R
9、8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10
10、L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U82.读某地一年中正午太阳高度变化示意图,回答:A(1)该地纬度位置是()A.10 N B.10 S C.13 26 N D.13 26 S
11、 A(2)下列说法正确的是()A.之间的时间间隔至少是三个月.B.两处表示太阳直射在北回归线C.处的正午太阳高度表示太阳直射在赤道D.处北半球各地正午太阳高度达全年最大值3.图中四条线分别表示四个地点在北半球夏半年某日的太阳高度变化过程.读图回答:(1)表示的地点是北极点.判断理由是:地球绕地轴自西向东自转,北半球夏半年北极点每天太阳高度整日几乎不变.地夏半年太阳高度值h的变化范围是CA.6634 h 90B.2326 h66 34C.0 h 2326D.30 h60(2)这一天,太阳直射点的纬度是h.(3)四地中,产生极昼现象的是地.这一天发生极昼现象的地区是北纬(90-h)及其以北地区.(
12、4)表示的地方是赤道.判断理由是终年平分昼夜.(5)该日、两地正午太阳高度值H1 为 2 hH2 为(90-h).(6)四个地点的纬度从高到低的排列依次是.DA.B.C.D.计算:1)夏至日,30N 的正午太阳高度.83 342)太阳直射20S,30S的正午太阳高度.703)冬至日,30N 的正午太阳高度.3634日影问题一.总的原则:太阳在前,影子在后.太阳高度与日影的关系:常识:1.太阳高度角越大,影长越 短文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9
13、D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4
14、R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK1
15、0L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4
16、T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 Z
17、Q4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6
18、J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档
19、编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U82.太阳 直射 某地时,某地影长为 零.3.一天之中,正午 影长最 短思考:北回归线以北地区,影子最短是哪一天?最长是哪一天?夏至日,冬至日二.不同纬度正午影子的朝向日影的朝向与光线方向相反;不同纬度正午影子的朝向规律:北回归线以北(除北极):正午影子全年朝北正午影子全年朝北南回归线以南(除南极):正午影子全年朝南正午影子全年朝南南北回归线之间正午影
20、子:既可朝南也可朝北影子朝正北或正南时当地时间为12点思考:赤道与北回归线之间,正午时影子朝南的日子多还是朝北的日子多?朝北 的日子多三.不同时节全球日出日落方向及日影方向(寒带除外)知识储备:日出日落的方位图结论:太阳直射点在赤道时,地球上日出方位在正东,日落于 正西。太阳直射点在北半球时,地球上(除极昼、极夜地区)日出方位均在东北,日落于 西北。太阳直射点在南半球时,地球上(除极昼、极夜地区)日出方位均在东南,日落于 西南。日出日落的日影方向、影长变化规律:A、直射点在北半球时,日出东北影朝_西南 _,日落西北影朝_东南 _。B、直射点在南半球时,日出东南影朝_西北 _,日落西南影朝_东_
21、北。C、直射点在赤道上,日出正东影朝_正西 _,日落正西影朝_正东 _。想想:当太阳直射北半球时北半球中纬度太阳的视运动路线是怎么的?日出日落文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK
22、10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I
23、4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5
24、ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J
25、6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文档编码:CM9D4P3Y4R8 HK10L10I4T9Z5 ZQ4C6J6J6U8文
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