CARDONE V J, GREENWOOD J G, CANE M A. On trends in historical marine wind data[J]. Journal of Climate, 1990, 3: 113-127.
[2]
CHELTON D B, SCHLAX M G, FREILICH M H, et al. Satellite measurements reveal persistent small-scale features in ocean winds[J]. Science, 2004, 303: 978-983.
[3]
SONG Q, HARA T, CORNILLON P, et al. A comparison between observations and MM5 simulations of the marine atmospheric boundary layer across a temperature front[J]. Journal of Atmospheric and Oceanic Technology, 2004, 21: 170-178.
Jet Propulsion Laboratory.QuikSCAT Science Data Product User’s Manual: Overview and Geophysical Data Products . Publ D-18053, Pasadena, Calif, 2001.
[7]
CLEVELAND W S. Robust locally weighted regression and smoothing scatterplots[J]. Journal of the American Statistical Association, 1979, 83:596-610.
[8]
LIU W T, TANG W. Equivalent neutral wind . JPL Publication.Pasadena, CA.1996:96-17.
[9]
LARGE W G, POND S. Sensible and latent heat flux measurements over the ocean[J]. J Phys Oceanogr, 1982, 12: 464-482.
[10]
ANDERSON R J. A study of wind stress and heat flux over the open ocean by the inertial-dissipation method[J]. Journal of Physical Oceanography, 1993, 23: 2154-2161.
WUNSCH, C. What is the thermohaline circulation[J]. Science, 2002, 298: 1180-1181.
[14]
KALNAY E, KANAMITSU M, KISTLER R,et al. The NCEP/NCAR 40-year reanalysis project[J]. Bulletin of the American Meteorological Society, 1996, 77: 437-471.
[15]
SONG Q, CHELTON D B, ESBENSEN S K, et al.Coupling between sea surface temperature and low-level winds in mesoscale numerical models[J]. Journal of Climate, 2009, 22: 146-164.
[16]
CHELTON D B, SCHLAX M G, SAMELSON R M, et al. Global observations of large oceanic eddies[J]. Geophys Res Lett, 2007, 34: doi:10.1029/2007GL030812.
[17]
SPALL M A. Midlatitude wind stress-sea surface temperature coupling in the vicinity of oceanic fronts[J]. Journal of Climate, 2007, 20: 2785-3801.
FREILICH M, DUNBAR R S. The accuracy of the NSCAT1 vector winds: comparisons with National Data Buoy Center buoys[J]. Journal of Geophysical Research, 1999, 104: 11231-11246.
[20]
CHELTON D B, FREILICH M H. Scatterometer-based assessment of 10-m wind analyses from the operational ECMWF and NCEP numerical weather prediction models[J]. Mon Wea Rev, 2005, 133: 409-429.
[21]
FREILICH M H, VANHOFF B. The accuracy of preliminary WindSat vector wind measurements: comparisons with NDBC buoys and QuikSCAT[J].Geoscience and Remote Sensing, IEEE Transactions, 2005, 44(3): 622-637.
[22]
O’NEILL L W, CHELTON D B, ESBENSEN S K, et al. High-resolution satellite measurements of the atmospheric boundary layer response to SST variations along the Agulhas Return Current[J]. J Climate, 2005, 18: 2706-2723.
[23]
SCHLAX M G, CHELTON D B, FREILICH M H. Sampling errors in wind fields constructed from single and tandem scatterometer datasets[J]. J Atmos Oceanic Technol, 2001, 18: 1014-1036.
[24]
RISIEN C M, CHELTON D B. A satellite-derived climatology of global ocean winds[J]. Remote Sensing Environment, 2006, 105: 221-236.
[25]
KARA A B, HURLBURT H E.WALLCRAFT A J. Stability dependent exchange coefficients for air-sea fluxes[J].J Atmos Oceanic Technol, 2005, 22: 1080-1094.