Atmospheric manifestation of tropical instability wave observed by QuikSCAT and tropical rain measuring mission

By Timothy W. Liu, Xiaosu Xie, P. Polito, Shang-Ping Xie, H. Hashizume. 2000

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Air–sea interaction over ocean fronts and eddies (2008, background): “3b and c) as shown by Liu et al. (2000), Chelton et al. (2001), and Hashizume et al. (2001).”
Local and remote atmospheric response to tropical instability waves: A global view from space (2001, methodology): “Coinciding with the developing TIWs, NASA’s QuikSCAT satellite was launched into the space in June, and its scatterometer SeaWinds offers a high-resolution, nearly global view of the world ocean on a daily basis [Liu et al., 2000].”
Progress in Scatterometer Application (2002, background): “The phase differences imply that the wind-SST coupling is caused by buoyancy instability and mixing in the atmospheric boundary layer, which has been confirmed by wind profiles measured on a research ship (Liu et al., 2000b).”
Coupled ocean-atmosphere interaction at oceanic mesoscales (2010, background): “…53 Oceanography | Vol.23, No.4 54 detailed investigations of the spacetime structure of the response of the surface wind field to TIW-induced SST variations in the eastern tropical Pacific region (Liu et al., 2000; Chelton et al., 2001; Polito et al., 2001; Hashizume et al., 2002; Chelton, 2005).”
Aquarius reveals salinity structure of tropical instability waves (2012, background): “ocean-atmosphere coupling [Xie et al., 1998; Liu et al., 2000; Chelton et al., 2001; Yu and Liu, 2003], and marine biogeochemistry [e.”