| 词条 | Misoscale meteorology |
| 释义 |
Misoscale is an unofficial scale of meteorological phenomena that ranges in size from 40 meters to about 4 kilometers.[1] This scale was proposed by Ted Fujita, the father of the Fujita scale, to classify phenomenon of the order of the rotation within a thunderstorm, the scale of the funnel cloud of a tornado, and the size of the swath of destruction of a microburst.[2] It is a subdivision of the microscale. References1. ^{{Cite web| url= http://www.weather.gov/glossary/index.php?letter=m | title= Letter M of meteorological Glossary | publisher=National Weather Service Glossary | accessdate = 28 December 2014 }} 2. ^{{cite journal | url= http://journals.ametsoc.org/doi/pdf/10.1175/1520-0469%281981%29038%3C1511%3ATADITC%3E2.0.CO%3B2 | doi = 10.1175/1520-0469(1981)038<1511:TADITC>2.0.CO;2 | title= Tornadoes and Downbursts in the Context of Generalized Planetary Scales | author= Ted Fujita | journal = Journal of the Atmospheric Sciences | publisher = American Meteorological Society | place= Boston | volume = 38 | issue = 8 |date=August 1981 | issn = 1520-0469 | pages = 1511–1534 | accessdate = 28 December 2014 | bibcode= 1981JAtS...38.1511F }} See also
1 : Mesoscale meteorology |
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