1 Ekman V W. On the influence of the earth's rotation on ocean currents. Ark Mat Astron Fys, 1905, 2: l-53
[2]
2 Wirth A. On the Ekman spiral with an anisotropic eddy viscosity. Boundary Layer Meteorol, 2010, 137: 327-331
[3]
3 Dubos T, Barthlott C, Drobiski P. Emergence and secondary instability of Ekman layer rolls. J Atmos Sci, 2008, 65: 2326-2342
[4]
4 Zhang G Z, Xu X D, Wang J Z. A dynamic study of Ekman characteriscs by using 1998 SCSMEX and TIPEX boundary layer data. Adv Atmos Sci, 2003, 20: 249-356
[5]
8 Wang J Z, Wang Y Q, Liu H, et al. Diagnostic identification of the impact of meteorological conditions on PM2.5 concentrations in Beijing. Atmos Environ, 2013, 81: 158-165
16 Wang Y T, Bian L G, Ma Y F. Surface ozone monitoring and background characteristics at Zhongshan station over Antarctica. Chin Sci Bull, 2011, 56: 1011-1019
6 Zhang G Z, Bian L G, Wang J Z, et al. The boundary layer characteristics in the heavy fog formation process over Beijing and its adjacent areas. Sci China Ser D-Earth Sci, 2005, 48: 88-101
[12]
7 Wang J Z, Gong S, Zhang X Y, et al. A parameterized method for air quality diagnosis and its applications. Adv Meteorol, 2012, doi:10.1155/2012/238589
[13]
11 Ling J, Li C Y, Zhou W, et al. Effect of boundary 1ayer latent heating on MJ0 simulations. Adv Atmos Sci, 2013, 30: 101-115
[14]
12 Hart J E. A note on nonlinear corrections to the Ekman layer pumping velocity. Phys Fluids, 2000, 12: 131
[15]
13 Tan Z M, Fang J, Wu R S. Nonlinear Ekman layer theories and their applications. Acta Meteorol Sin, 2006, 20: 210-222
[16]
14 Hui F M, Cheng X, Liu Y, et al. An improved land sat image mosaic of Antarctic. Sci China Ser D-Earth Sci, 2013, 56: 1312
[17]
17 效存德, 李院生, 侯书贵, 等. 南极冰盖最高点满足钻取最古老冰芯的必要条件: Dome A 最新实测结果. 科学通报, 2007, 52: 2456-2460
[18]
18 Ma Y F, Bian L G, Xiao C D. Near surface climate of the traverse route from Zhongshan Station to Dome A, East Antarctica. Antarctic Sci, 2012, 22: 443-459
23 Argentini A, Viola A, Sempreviva A M, et al. Summer boundary-layer height at the plateau site of Dome C Antarctica. Bound Layer Meteorol, 2005, 115: 409-422