未命名1

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vortex）是极地高空冷性大型涡旋系统，是极区大气环流的组成部分。当偏离极地向南移动时，常导致寒潮活动增多增强。南极极地涡旋比北极极地涡旋更显著，持续时间也更长。\n近期因北极涡旋相对活跃，且位置更靠近我国北方和西伯利亚这一侧，因此不断分裂出冷空气南下影响我国，再加上乌拉尔山和鄂霍次克海两个阻塞高压，更有利于冷空气的堆积和加强，所以造成冷空气活动频繁。\n在东北信风或东南信风的控制地区，副热带高压影响不到的地区，风从高纬吹向低纬，气温升高，不易成云致雨，形成热带沙漠气候。由于降水稀少，动植物难以生存，植被稀疏形成荒漠自然带，只不过热带沙漠气候位于“热带”地区，温带沙漠气候位于“温带”地区。 \n热带沙漠气候的分布地区主要位于南北回归线穿过的副热带地区，由于常年受到副热带高气压带的控制，盛行下沉气流，空气下沉增温，难以成云致雨，降水稀少。\n\n卡塔尔为啥没有像西伯利亚寒流这样的冷空气呢？\n北极气团形成在北极冰封的洋面上及其邻近陆地上的气团。其特点是气温很低，水汽少（但相对湿度不低），大气层结稳定，低层常有强逆温层。冬季入侵大陆时，带来严寒和暴风雪天气。\n世界的风-4(气团和锋面)https://zhuanlan.zhihu.com/p/235677388?utm_id=0\n\n高气压空气自中心向外围流散（辐散），因受地球转动的影响，在北半球作顺时针方向流动，在南半球作逆时针方向流动。高气压也被称为反气旋，但前者是按气压场命名，后者则按气流场命名（与旋涡方向相反）。\n在高压区内无锋面存在，因气流辐散，高空空气下沉补充，下沉过程中气温升高，相对湿度降低，形成少云、雨和大风天气。\n\n『『』』我国地处世界上最大的大陆亚欧大陆和世界上最大的海洋太平洋之间，海陆热力性质差异巨大，所以我国形成了全球最典型的季风气候分布区，特别是亚热带季风和温带季风气候。夏季高温多雨、冬季寒冷少雨、雨热同期、四季分明是其主要特征。其次，我国的大陆性气候表现在与同纬度其他地区相比，冬季我国是世界上同纬度最冷的国家，而夏季则是世界上同纬度最热的国家（沙漠除外）。\n我国的降水主要是由东南季风带来。『『』』\n太阳怎样加热大气:http://www.kepu.net.cn/vmuseum/earth/weather/sun/index.html\n\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/1f0022120d2bcb97b3870d7d5416daaf6ef9cb2f.jpg","width":719,"height":656,"size":347405,"status":"loaded"}}},{"insert":"\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/458de12eeece0a8ea40de2e1a53b0228bfe14441.jpg","width":719,"height":1272,"size":545033,"status":"loaded"}}},{"insert":"\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/e2616f77cb4fc810d9d46cba61272f911ecaf0d3.jpg","width":719,"height":215,"size":76408,"status":"loaded"}}},{"insert":"\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/c529852b52b3342eb99e3d4b9a94ea409fd21ffd.jpg","width":719,"height":385,"size":133678,"status":"loaded"}}},{"insert":"\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/223dd1f1fb6342c8aa958f97ad16b9b0afdfb804.jpg","width":719,"height":268,"size":92250,"status":"loaded"}}},{"insert":"\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/38dbab438f8179b70301e4281c61ff2f7bd7fbcf.jpg","width":1600,"height":720,"size":427259,"status":"loaded"}}},{"insert":"\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/288c334455f24c2e5be332c90f0d6b584bfe120f.jpg","width":720,"height":1600,"size":559981,"status":"loaded"}}},{"insert":"温度对一些动物的影响:比如巴沙鱼最适宜生长的水温为22～32℃，低于20℃时，水温降低生长速度放缓；当水温低于13℃时会冻伤直至死亡，腹腔内积累有三块较大的油脂，占体重的58%。\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/a9456cc579c14ce9114a9a30b2745de75b04998e.jpg","width":719,"height":691,"size":241772,"status":"loaded"}}},{"insert":"\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/f1d37d918ae2a4395c06c3430aad01ec05eaef5d.jpg","width":500,"height":333,"size":95972,"status":"loaded"}}},{"insert":"\n\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/7c250977756ff68cb17de446517d680b6a5c02e2.jpg","width":820,"height":480,"size":331976,"status":"loaded"}}},{"insert":"\n当空气强烈受热时,湿热空气膨胀上升,空气中的水汽冷却凝结形成的降雨就叫做对流雨.赤道地区全年以对流雨为主,我们国家的对流雨多见于夏季的午后；地形雨是因潮湿的空气前进时,受到山地阻挡,被迫沿着山坡爬升.在上升过程中,空气中的水冷却凝结形成的降水.如印度东北部和我国西藏东南部的降水；两种性质不同的气流相遇,它们中间的交界面叫锋面.在锋面上,暖、湿、较轻的空气被抬升到冷、干、较重的空气上面去.在抬升的过程中,空气中的水汽冷却凝结,形成的降水叫锋面雨；台风雨降雨一种特殊的降雨形式,一般在台风到来时发生.且伴有强烈的雷电大风!特殊的一点情况是：台风的风眼经过的地区天空反而是非常平静的!\n\n\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/5b5eb71ab07900f065073512f4c7761fef697a09.jpg","width":719,"height":265,"size":89979,"status":"loaded"}}},{"insert":"\n百科词条，"},{"attributes":{"color":"#18191c","bold":true},"insert":"行星大气:包裹着行星体的中性气体和电离气体的总称"},{"insert":":\n火星大气密度不足地球大气的1%，主要是二氧化碳，火星表面的平均大气压相当地球上30～40公里高空的大气压。极低的气压下，人体血管会膨胀。\n在火星赤道，夏天白天最高30摄氏度左右。\n地球由于质量较小，由地球内部物质衰变产生的轻气体绝大部分从大气层逃逸，只有较重的气体如氮氧等气体保留在地球周围形成地球大气层。\n在海拔4500米的高原，能够明显感觉到缺氧，这个高度的大气压大概为标准大气压的59%。\n\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/be9c4c9abcfbda043c9cf85a4b99ee49c6f94561.jpg","width":719,"height":926,"size":323757,"status":"loaded"}}},{"insert":"\n木星由中心至71370公里处，依次为由以铁硅为主的固体核、液态金属氢（其中分子离解为独立原子，形成导电流体）、液态分子氢。再向外是大气层，厚度约8050千米，主要由氢构成，在下面是热的液体氢的海洋，超过1732摄氏度，氢也不会沸腾而逃逸。液态氢层厚度超过48280千米。在它的下面可能是一个水和氨的层，然后是岩石核心。液氢呈现出一些金属的特性：电流能在其中流动，产生磁场，在太阳系中是除了太阳外最强的。\n当氢气被充分压缩产生: 液态金属氢是一种简并态物质，H2的同素异形体；液氢，是由氢气经过降温而得到的液体。\n\n"},{"attributes":{"class":"normal-img"},"insert":{"native-image":{"alt":"read-normal-img","url":"https://b2.sanwen.net/b_article/f311cf5350ed4ae761f62493e95ee1db90ed5206.jpg","width":649,"height":510,"size":158551,"status":"loaded"}}},{"insert":"\n紫外辐射在高空被臭氧吸收，对大气有增温作用。臭氧层是大气层的平流层中臭氧浓度高的层次。温室效应气体 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