省优质课《热力环流》讲课课件

冷熟不均引大气运高中地理实验教科书必修第二章第一节Evaluadononly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL冷熟不均引大气运1冷熟不均引大气运高中地理实验教科书必修第二章第一节侪人:储娟娟单谧:安阳市实验中学Evaluadononly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL冷熟不均引大气运2想为什么暖气片装在教室的下部,而冷空调却安装在教室的上部?Evaluationonly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL想3吧回凹热力环流Evaluauononr.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL吧回凹4气压和等压面气压是单位面积伴么捷忾座的压力,以百帕(hPa)为单位Evaluationonly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL气压和等压面5结论一同一地点海拔越高,气压越低a23000米Pal>Pa2a1ValadononlychAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL结论一同一地点海拔越高,气压越低6气压和等压面(hPa)等压面把空间气压值相同940的各点组合而成的等压面面叫做等压面。960等压面980等压面1000B假设地表性质均一,受热均匀Valadononry.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL气压和等压面7执水冰瑛犭Evaluationonly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL执水8三、热力环流的形成过程AB受热升箭冷却下箭高度播放等压高水低水Evaluadononly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL三、热力环流的形成过程9二、热力环流的形成过程低气质一高气压低气压由于地面冷热不均而形成的空气环流,称为熟力环流。乞是大气运动最简单的形式。高气唐·)低气压一高气压B冷热冷Valadononry.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL二、热力环流的形成过程10省优质课《热力环流》讲课课件11省优质课《热力环流》讲课课件12省优质课《热力环流》讲课课件13省优质课《热力环流》讲课课件14省优质课《热力环流》讲课课件15省优质课《热力环流》讲课课件16省优质课《热力环流》讲课课件17省优质课《热力环流》讲课课件18省优质课《热力环流》讲课课件19省优质课《热力环流》讲课课件20省优质课《热力环流》讲课课件21省优质课《热力环流》讲课课件22省优质课《热力环流》讲课课件23省优质课《热力环流》讲课课件24省优质课《热力环流》讲课课件25冷熟不均引大气运高中地理实验教科书必修第二章第一节Evaluadononly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL冷熟不均引大气运26冷熟不均引大气运高中地理实验教科书必修第二章第一节侪人:储娟娟单谧:安阳市实验中学Evaluadononly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL冷熟不均引大气运27想为什么暖气片装在教室的下部,而冷空调却安装在教室的上部?Evaluationonly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL想28吧回凹热力环流Evaluauononr.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL吧回凹29气压和等压面气压是单位面积伴么捷忾座的压力,以百帕(hPa)为单位Evaluationonly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL气压和等压面30结论一同一地点海拔越高,气压越低a23000米Pal>Pa2a1ValadononlychAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL结论一同一地点海拔越高,气压越低31气压和等压面(hPa)等压面把空间气压值相同940的各点组合而成的等压面面叫做等压面。960等压面980等压面1000B假设地表性质均一,受热均匀Valadononry.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL气压和等压面32执水冰瑛犭Evaluationonly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL执水33三、热力环流的形成过程AB受热升箭冷却下箭高度播放等压高水低水Evaluadononly.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL三、热力环流的形成过程34二、热力环流的形成过程低气质一高气压低气压由于地面冷热不均而形成的空气环流,称为熟力环流。乞是大气运动最简单的形式。高气唐·)低气压一高气压B冷热冷Valadononry.chAsposeslidesforNET4odientPEvaluationonly.CreatedwithAsposeSlidesforNET4.0dientProfilo71Copyright2019-2019AsposePtyL二、热力环流的形成过程35省优质课《热力环流》讲课课件36省优质课《热力环流》讲课课件37