大氣邊界層
参考资料

1 2 3 4 5 6 7 8 9 10 11 12 13 14  Wallace, John; Hobbs, Peter. . Academic Press. 2006. ISBN 978-0-12-732951-2 （英语）.
1 2  Ahrens, C. Donald.  Twelfth edition. Boston, MA.   [2020-06-16]. ISBN 978-1-337-61666-9. OCLC 1021858090. （原始内容存档于2020-06-16）.  引文格式1维护：冗余文本 (link)
↑  . American Meteorological Society.   [2020-06-02]. （原始内容存档于2020-09-19）.
↑  . American Meteorological Society.   [2020-06-02]. （原始内容存档于2020-08-04）.
↑  Wizelius, Tore. . London: Earthscan Publications Ltd. 2007: 40. ISBN 978-1-84407-262-0. The relation between wind speed and height is called the wind profile or wind gradient.
1 2  Brown, G. . New York: Wiley. 2001: 18. ISBN 0-471-34877-5.
↑  Oke, T. . London: Methuen. 1987: 54. ISBN 0-415-04319-0. Therefore the vertical gradient of mean wind speed (dū/dz) is greatest over smooth terrain, and least over rough surfaces.
1 2  Crawley, Stanley. . New York: Wiley. 1993: 272. ISBN 0-471-84298-2.
↑  Harrison, Roy. . Cambridge: Royal Society of Chemistry. 1999: 11. ISBN 0-85404-584-8.
1 2  Thompson, Russell. . New York: Routledge. 1998: 102–103. ISBN 0-415-17145-8.
↑  Maeda, Takao, Shuichiro Homma, and Yoshiki Ito. . 2008-07-04.
↑  Lubosny, Zbigniew. . Berlin: Springer. 2003: 17. ISBN 3-540-40340-X.
↑  Gupta, Ajaya. . Boca Raton: CRC Press. 1993: 49. ISBN 0-8493-8969-0.
↑  Stoltman, Joseph. . Berlin: Springer. 2005: 73. ISBN 1-4020-2850-4.
↑  Chen, Wai-Fah. . Boca Raton: CRC Press. 1997: 12–50. ISBN 0-8493-2674-5.
↑  Ghosal, M. . . City: Alpha Science International, Ltd. 2005: 378–379. ISBN 978-1-84265-125-4.
↑  Stull, Roland. . Boston: Kluwer Academic Publishers. 1997: 442. ISBN 90-277-2768-6. ...both the wind gradient and the mean wind profile itself can usually be described diagnostically by the log wind profile.
↑  Thuillier, R.H.; Lappe, U.O. . Journal of Applied Meteorology (American Meteorological Society). 1964, 3 (3): 299–306. Bibcode:1964JApMe...3..299T. ISSN 1520-0450. doi:10.1175/1520-0450(1964)003<0299:WATPCF>2.0.CO;2.
↑  Dalgliesh, W. A. & D. W. Boyd. . Canadian Building Digest. 1962-04-01  [2007-06-30]. （原始内容存档于2007-11-12）. Flow near the surface encounters small obstacles that change the wind speed and introduce random vertical and horizontal velocity components at right angles to the main direction of flow.
↑  Stensrud, D.J.; Coniglio, M.C.; Knopfmeier, K.H.; Clark, A.J. . . Elsevier. 2015: 167–180  [2020-06-24]. ISBN 978-0-12-382225-3. doi:10.1016/b978-0-12-382225-3.00493-x. （原始内容存档于2020-08-15） （英语）.
↑  Chen, Xuelong; Škerlak, Bojan; Rotach, Mathias W.; Añel, Juan A.; Su, Zhonbgo; Ma, Yaoming; Li, Maoshan. . Journal of the Atmospheric Sciences. 2016-05-01, 73 (5): 2021–2038. ISSN 0022-4928. doi:10.1175/JAS-D-15-0148.1 （英语）.
1 2 3 4  Pielke, Roger; Hayden, Bruce. . Encyclopædia Britannica, inc.  使用|accessdate=需要含有|url= (帮助)
↑  Köpp, F.; Schwiesow, R.L.; Werner, C. . Journal of Applied Meteorology and Climatology (American Meteorological Society). January 1984, 23 (1): 153. Bibcode:1984JApMe..23..148K. ISSN 1520-0450. doi:10.1175/1520-0450(1984)023<0148:RMOBLW>2.0.CO;2.
↑  Pat Arnott.  (pdf).   [2020-06-24]. （原始内容存档 (PDF)于2020-06-25） （英语）.
↑  Hadlock, Charles. . Washington: Mathematical Association of America. 1998. ISBN 0-88385-709-X.
↑  Lal, R. . New York: Marcel Dekker. 2005: 618. ISBN 0-8493-5053-0.
卡门涡街示意图