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Ekman Veering Observed near the Ocean Bottom

Ekman Veering Observed near the Ocean Bottom,10.1175/1520-0485(1976)006<0238:EVONTO>2.0.CO;2,Journal of Physical Oceanography,Pijush K. Kundu

Ekman Veering Observed near the Ocean Bottom   (Citations: 130)
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Journal: Journal of Physical Oceanography - J PHYS OCEANOGR , vol. 6, no. 2, pp. 238-242, 1976
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    • ...A vector correlation analysis (Kundu 1976) has been performed to characterize the difference between the original ECMWF winds and the analyzed winds...

    Alexander Barthet al. Correcting surface winds by assimilating high-frequency radar surface ...

    • ...similarity was confirmed by estimating the correlation between HF radar patterns and HF radar + ALADIN/HR patterns, using a complex correlation coefficient [Kundu, 1976] together with the mean angular offset of veering (Table 1). The highest correlation was found between characteristic wind patterns, especially between the most pronounced ones, i.e., BMU1 (bora) and BMU4 (sirocco)...

    Hrvoje Mihanovicet al. Surface current patterns in the northern Adriatic extracted from high-...

    • ...The vector cross correlations were also evaluated according to Kundu [1976]...

    Jian Zhaoet al. Dynamics of surface currents over Qingdao coastal waters in August 200...

    • ...To examine the correlation between surface currents and wind, the complex correlation coefficient ρ (Kundu 1976) between the time series of two-dimensional surface currents at each grid point of the HFR observation grid and a corresponding time series of the two-dimensional wind field was calculated...
    • ...This definition was adopted from Kundu (1976 )w ho analysed the systematic deviation to the left (cyclonic in the northern hemisphere) of currents in the bottom layer compared to the direction of geostrophic velocities...
    • ...Kundu (1976) demonstrated that the capabilities of classical approaches to evaluate the veering suffer from strongly varying angles (weak currents events increase the uncertainty in veering angle)...

    Alexander Portet al. Tidal and wind-driven surface currents in the German Bight: HFR observ...

    • ...[23] The above three model runs have poor visual agreement of surface currents (not shown here) with the spatial distributions of HF radar derived surface currents (Figure 4). The magnitude r and the angular displacement � of the complex correlation coefficient between the mooring M1 ADCP and the model currents for a particular depth are estimated using the approach outlined by Kundu [1976]...

    Igor Shulmanet al. Comparisons of upwelling and relaxation events in the Monterey Bay are...

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