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准静止锋可能由移动缓慢的[[冷锋]]或[[暖锋]]转变而成,当锋的移动速度降低至 9 km/h 以下时,就会演变成为准静止锋。准静止锋两侧的风向通常与锋面平行且方向相反,这亦是阻碍准静止锋移动的原因之一。<ref name=":2">{{Cite book|chapter=|url=https://www.cengage.com/c/meteorology-today-an-introduction-to-weather-climate-and-the-environment-12e-ahrens/9781337616669PF|publisher=Brooks/Cole, Cengage Learning|date=|isbn=978-1-337-61666-9|language=en|first=C. Donald|last=Ahrens|title=Meteorology Today: An Introduction to Weather, Climate, and the Environment|year=2017|location=|pages=|edition=12|access-date=2020-06-17}}</ref><ref>{{Cite web|title=Fronts|url=https://climate.ncsu.edu/edu/Fronts|accessdate=2020-06-17|author=|date=|format=|work=|publisher=North Carolina Climate Office|language=en-us}}</ref> |
准静止锋可能由移动缓慢的[[冷锋]]或[[暖锋]]转变而成,当锋的移动速度降低至 9 km/h 以下时,就会演变成为准静止锋。准静止锋两侧的风向通常与锋面平行且方向相反,这亦是阻碍准静止锋移动的原因之一。<ref name=":2">{{Cite book|chapter=|url=https://www.cengage.com/c/meteorology-today-an-introduction-to-weather-climate-and-the-environment-12e-ahrens/9781337616669PF|publisher=Brooks/Cole, Cengage Learning|date=|isbn=978-1-337-61666-9|language=en|first=C. Donald|last=Ahrens|title=Meteorology Today: An Introduction to Weather, Climate, and the Environment|year=2017|location=|pages=|edition=12|access-date=2020-06-17}}</ref><ref>{{Cite web|title=Fronts|url=https://climate.ncsu.edu/edu/Fronts|accessdate=2020-06-17|author=|date=|format=|work=|publisher=North Carolina Climate Office|language=en-us}}</ref> |
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[[寒潮|冷空气]]在移动过程中遇山受阻时常会形成准静止锋,[[中国地理|中国 |
[[寒潮|冷空气]]在移动过程中遇山受阻时常会形成准静止锋,[[中国地理|中国]]常见的此类准静止锋有天山准静止锋、秦岭准静止锋、南岭准静止锋和云贵准静止锋等。<ref name=":1" /> |
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== 天气过程 == |
== 天气过程 == |