| dc.creator | Nielsen-Gammon, John | |
| dc.creator | Schultz, David | |
| dc.date.accessioned | 2016-10-28T18:52:17Z | |
| dc.date.available | 2016-10-28T18:52:17Z | |
| dc.date.issued | 1999-09-01 | |
| dc.identifier.citation | Nielsen-Gammon, J. W., and D. M. Schultz, 1999: Comments on "The intensification of the low-level jet during the development of mesoscale convective systems on a mei-yu front". Mon. Wea. Rev., 127, 2227-2231. | en |
| dc.identifier.uri | https://hdl.handle.net/1969.1/158221 | |
| dc.description | © Copyright 1999 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (https://www.ametsoc.org/) or from the AMS at 617-227-2425 or copyrights@ametsoc.org. | en |
| dc.description.abstract | The recent article by Chen et al. (1998; henceforth Chen) concludes that three processes were important to the development of a particular low-level jet (LLJ) associated with a mei-yu front: (1) a transverse circulation caused by thermal wind adjustment at the entrance region of a jet streak; (2) a direct circulation driven by deep convection along the frontal zone; and (3) slantwise convection maintained by conditional symmetric instability. We find problems with the methodology and interpretation of all three phenomena. | en |
| dc.description.sponsorship | National Science Foundation | en |
| dc.language.iso | en_US | |
| dc.publisher | American Meteorological Society | |
| dc.title | Comments on “The Intensification of the Low-Level Jet during the Development of Mesoscale Convective Systems on a Mei-Yu Front” | en |
| dc.type | Article | en |
| local.department | Atmospheric Sciences | en |
| dc.identifier.doi | 10.1175/1520-0493(1999)127<2227:COTIOT>2.0.CO;2 | |
