| 词条 | Air stagnation |
| 释义 |
In the U.S., the numbers of stagnation days during winter and spring tend to be much smaller than those during summer and fall.[5] Spatial variations during winter and spring tend to be incoherent as well.[6] References1. ^{{cite journal|last1=Leung|first1=L. Ruby|last2=Gustafson Jr|first2=William I.|title=Potential regional climate change and implications to U.S. air quality|journal=Geophysical Research Letters|date=Aug 26, 2005|volume=32|issue=16|doi=10.1029/2005GL022911|bibcode=2005GeoRL..3216711L}} {{climate-stub}}2. ^Myanmar government (2007). Haze. {{webarchive|url=https://web.archive.org/web/20080224035453/http://www.kjc.gov.my/english/education/weather/haze01.html |date=2008-02-24 }} Retrieved on 2007-02-11. 3. ^Robert Tardif (2002). Fog characteristics. {{webarchive|url=https://web.archive.org/web/20110520021633/http://www.rap.ucar.edu/staff/tardif/Documents/CUprojects/ATOC5600/fog_characteristics.htm |date=2011-05-20 }} University Corporation for Atmospheric Research. Retrieved on 2007-02-11. 4. ^National Weather Service glossary. Air Stagnation. Retrieved on 2008-05-31. 5. ^{{cite journal|last1=Leung|first1=L. Ruby|last2=Gustafson Jr|first2=William I.|title=Potential regional climate change and implications to U.S. air quality|journal=Geophysical Research Letters|date=Aug 26, 2005|volume=32|issue=16|doi=10.1029/2005GL022911|bibcode=2005GeoRL..3216711L}} 6. ^{{cite journal|last1=Leung|first1=L. Ruby|last2=Gustafson Jr|first2=William I.|title=Potential regional climate change and implications to U.S. air quality|journal=Geophysical Research Letters|date=Aug 26, 2005|volume=32|issue=16|doi=10.1029/2005GL022911|bibcode=2005GeoRL..3216711L}} 2 : Air pollution|Atmospheric circulation |
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