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1、全球主要非地带性气候的分布及原因气候大类气候类型分布地区形成原因热带气候热带雨林气候马达加斯加岛东侧1、处于来自海洋的信风（北半球为东北信风，南半球为东南信风）的迎风坡，多地形雨。2、附近海域有暖流流经，对沿岸地区有增温增湿作用。3、再加上地形的抬升加强了地形雨。澳大利亚的东北部巴西高原东南部沿海中美洲的东北部几内亚湾沿岸热带雨林气候纬度位置偏高几内亚湾暖流对沿岸的增温增湿作用再加上地形的抬升加强了地形雨。热带草原气候东非高原圭亚那高原地势较高，气温随之下降，降水也减少（改变了大气环流状况），形成了终年高温、有明显干湿两季的热带草原气候。热带沙漠气候非洲西南部沿岸 本格拉寒流的影响澳大利亚西海
2、岸西澳大利亚寒流的影响、地形平坦、大分水岭对东南信风的阻挡。（地理纵横）秘鲁沿岸秘鲁寒流的影响、安第斯山的阻挡。索马里沿岸索马里寒流的影响，该地区呈现类似于荒漠化景观。塔尔沙漠西南季风影响小，气候干旱降水少人为原因：古代对植被的破坏。亚热带气候亚热带季风气候北美大陆东部季风气候不显著海陆热力差异：北美大陆东部的海陆热力差异不如东亚地区那样明显。气团和锋：北美大陆上南北属性不同的气团交绥，气旋活动频繁，季风环流遭到抑制而减弱。地中海气候澳大利亚东南部地处西风带的迎风坡，冬季受西风带的影响。温带 温带海洋 欧洲西部温带海洋流和海陆轮廓因素：由于欧洲西部文档编码:CT3D10U2R5P7 HY9C5
3、I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C
4、5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9
5、C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY
6、9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 H
7、Y9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7
8、HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7
9、 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9气候气候洋性气候一直延伸到北极圈附近的海陆轮廓更有利于沿岸强大的北大西洋暖流深入。澳大利亚东南部及新西兰南北二岛（大陆
10、东岸的温带海洋性气候）温带海洋性气候分布在南北纬4060之间的地区。主要分布在西欧、北美及南美大陆西岸狭长地带，许多人误以为温带海洋性气候只分布于南北纬 4060大陆西岸。事实上，只要是温带地区，又能受到西风的影响，终年有暖湿空气从海洋面上吹来，就可以形成温和多雨的温带海洋性气候。北美洲西部温带海洋性气候比欧洲西部温带海洋性气候范围狭小且南北延伸地形因素：由于南北延伸的高大的科迪勒拉山系的阻挡作用，把西风和暖流的影响仅限制在沿海一带。温带季风气候俄罗斯远东地区东西伯利亚山地的阻挡作用（迎风坡）文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3
11、D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT
12、3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:C
13、T3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:
14、CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码
15、:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编
16、码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档
17、编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9温带大陆气候巴塔哥尼亚高原尽管这里东西距海较近，且处于西风带范围内，但该地处于南美洲南部安第斯山脉的东侧山脉东侧背风坡地带，受山地的阻挡，雨水稀少。亚寒带气候亚寒带针叶林气候
18、亚欧大陆北部亚寒带针叶林气候在大陆东岸比大陆西岸纬度位置偏低洋流因素：西岸受北大西洋暖流的影响，东岸受千岛寒流的影响。南半球缺失海陆分布：南半球同纬度地区为海洋（地理纵横）极地气候苔原气候南半球缺失海陆分布：南半球同纬度地区为海洋冰原气候 北冰洋沿岸缺失海陆分布：北半球同纬度地区为北冰洋（但在格陵兰岛内陆地区有分布）。南北美洲西海岸的各种气候这些气候的分布范围仅局限在沿岸地带，形成南北延伸、东西更替更替的分布特点。是因为受高大的南北文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10
19、N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U1
20、0N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U
21、10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7
22、U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O
23、7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10
24、O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH1
25、0O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9南北延伸、东西更替更替的分布走向的科迪勒拉山系阻挡，各气候带不能向东深入，而仅局限与沿海一带。文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J
26、5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4
27、J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C
28、4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2
29、C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I
30、2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5
31、I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9文档编码:CT3D10U2R5P7 HY9C5I2C4J5 ZH10O7U10N6L9