| 词条 | Solenoid (meteorology) |
| 释义 |
In the context of meteorology, a solenoid is a tube-shaped region in the atmosphere where isobaric (constant pressure) and isopycnal (constant density) surfaces intersect, causing vertical circulation.[1][2] They are so-named because they are driven by the solenoid term of the vorticity equation.[3] Examples of solenoids include the sea breeze circulation and the mountain–plains solenoid.[4][5] References1. ^{{cite web|url=http://accessscience.com/content/Solenoid%20%28meteorology%29/634300 |title=Solenoid (meteorology) |author1=Frederick Sanders |author2=Howard B. Bluestein |publisher=McGraw-Hill Companies |year=2008}} 2. ^{{cite web |url=http://meteora.ucsd.edu/~mpritchard/bib/KocZhaKap01/index.html |title=Notes on mountain plains solenoid literature from Koch et al., MWR, 2001 |author=Mike Pritchard |date=2011-02-04}} 3. ^{{cite web |url=http://www.eumetcal.org/euromet/english/nwp/n2a20/n2a20005.htm |title=Sea Breeze |author=Eumetcal}} 4. ^{{cite web |url=http://kkd.ou.edu/METR4433_Spring_2011/Land_Sea_Breezes.pdf |title=Sea and Land Breezes |publisher=University of Oklahoma |year=2006 |format=PDF}} 5. ^{{cite journal | author1 = Jianhua Sun | author2 = Fuqing Zhang |date=February 2012 | title = Impacts of Mountain–Plains Solenoid on Diurnal Variations of Rainfalls along the Mei-Yu Front over the East China Plains | journal = Monthly Weather Review | volume = 140 | issue = 2 | pages = 379–397 | publisher = American Meteorological Society | doi = 10.1175/MWR-D-11-00041.1 | accessdate = 2012-05-10 | url = http://journals.ametsoc.org/doi/abs/10.1175/MWR-D-11-00041.1|bibcode = 2012MWRv..140..379S }} 1 : Atmospheric dynamics |
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