边界流(英语:Boundary Current)是指在大陆边缘的洋流,因此其动力受海岸线的影响。边界流可分为两个不同的类别:西部边界流和东部边界流。
| 本条目存在以下问题,请协助 改善本条目或在 讨论页针对议题发表看法。
|
东部边界流位于大洋盆地的东侧(毗邻大陆的西海岸),其特性一般较浅、较宽而且流动缓慢。位于副热带的东部边界洋流是向赤道流动的,把冷水从高纬度地区输送到低纬度地区。本格拉洋流[1]、加那利洋流[2]、 洪堡洋流[3] 和加利福尼亚洋流(英语:California Current)[4]等均属于东部边界流。在这些地区的沿岸上升流,经常把富含海鲜的深水带入东部边界洋流区,使其成为海产丰富区域[5][6]。
西部边界流则分为亚热带和低纬度西部边界流两种洋流。亚热带西部边界洋流是由于大环流的西环强化(英语:Western intensification)作用的,而在洋盆西侧形成的温暖、深、窄和快速流动的洋流,它们从热带向极地方向运送温水。墨西哥湾流[7]、阿古拉斯洋流[8]和黑潮[9]等均属此种西部边界流。低纬度西部边界流类似于亚热带西部边界流,但将冷水从亚热带流向赤道方向。棉兰老岛洋流(英语:Mindanao Current)[10]和巴西北部洋流(英语:North Brazil Current)[11]等也属于此种西部边界流。[12][13]。
Garzoli, S. L., and Gordon, A. L. (1996), Origins and variability of the Benguela Current, J. Geophys. Res., 101( C1), 897– 906, doi:10.1029/95JC03221
M Knoll, A Hernández-Guerra, B Lenz, F López Laatzen, F Machı́n, T.J Müller, G Siedler (2002) The Eastern Boundary Current system between the Canary Islands and the African Coast,Deep Sea Research Part II: Topical Studies in Oceanography,Volume 49, Issue 17,Pages 3427-3440,ISSN 0967-0645,https://doi.org/10.1016/S0967-0645(02)00105-4
R. N. Gibson, R. J. A. Atkinson, J. D. M. Gordon( 2007). THE HUMBOLDT CURRENT SYSTEM OF NORTHERN AND CENTRAL CHILE, Oceanography and Marine Biology, CRC Press, ISBN 9780429144905
B.M. Hickery and T.C.Royer (2009) Califrona and Alaska Currents in Ocean Current, editor Steve A. Thorpe ISBN 978-0-08-096486-7
S. G. H. Philander and J-H. Yoon (1982) Eastern Boundary Currents and Coastal Upwelling, Jour. of Physical Oceanography, vol 12, issure 8. Page(s): 862–879. https://doi.org/10.1175/1520-0485(1982)012<0862:EBCACU>2.0.CO;2
Rykaczewski, R. R., Dunne, J. P., Sydeman, W. J., García-Reyes, M., Black, B. A., and Bograd, S. J. (2015), Poleward displacement of coastal upwelling-favorable winds in the ocean's eastern boundary currents through the 21st century, Geophys. Res. Lett., 42, 6424– 6431, doi:10.1002/2015GL064694
Charney J.G. (1990) The Gulf Stream as an Inertial Boundary Layer. In: Lindzen R.S., Lorenz E.N., Platzman G.W. (eds) The Atmosphere — A Challenge. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-944970-35-2_16
Kathryn A. Kelly, R. Justin Small,R. M. Samelson, Bo Qiu, Terrence M. Joyce, Young-Oh Kwon, and Meghan F. Cronin (2010)Western Boundary Currents and Frontal Air–Sea Interaction: Gulf Stream and Kuroshio Extension Jour of Climate Vol. 23 Issue 21, p 5644-5667.DOI: https://doi.org/10.1175/2010JCLI3346.1
Lukas, R., Firing, E., Hacker, P., Richardson, P. L., Collins, C. A., Fine, R., and Gammon, R. (1991), Observations of the Mindanao Current during the western equatorial Pacific Ocean circulation study, J. Geophys. Res., 96( C4), 7089– 7104, doi:10.1029/91JC00062
Müller, T. J., Ikeda, Y., Zangenberg, N., and Nonato, L. V. (1998), Direct measurements of western boundary currents off Brazil between 20°S and 28°S, J. Geophys. Res., 103( C3), 5429– 5437, doi:10.1029/97JC03529
Shiro Imawaki, Amy S. Bower, Lisa Beal, Bo Qiu,Chapter 13 - Western Boundary Currents,Editor(s): Gerold Siedler, Stephen M. Griffies, John Gould, John A. Church, International Geophysics,Academic Press, Volume 103, 2013, Pages 305-338, ISSN 0074-6142, ISBN 9780123918512,https://doi.org/10.1016/B978-0-12-391851-2.00013-1.(https://www.sciencedirect.com/science/article/pii/B9780123918512000131)
Hogg, N. G., and Johns, W. E. (1995), Western boundary currents, Rev. Geophys., 33( S2), 1311– 1334, doi:10.1029/95RG00491