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KuROS: A new airborne Ku-band Doppler radar for observation of the ocean surface

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Academic year: 2021

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Figure

Fig. 1. Geometry of observation, for  both the LI and MI antennae
Fig. 4.Normalized  radar  cross  section  σ°  averaged  over  the  azimuthal  directions (~120 s of data), as a function of  incidence angle
Fig. 7. Omnidirectional sea wave frequency spectrum as a function of wave  frequency from the buoy (solid line) and from KuROS just before  overflight of the buoy (dotted line), and just after overflight (dashed
Fig. 8a-c  show, for  two 30s  data  sets of  a  same  flight  (wind  speed ~14 m/s, fully-developed wind sea with significant wave  height H s ~3 m), the speckle energy density spectrum averaged  in  azimuth
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