Titlebook: Oceanography from Space; Revisited Vittorio Barale,J.F.R. Gower,L. Alberotanza Book 2010 Springer Science+Business Media B.V. 2010 AVHRR.Co

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Passive Microwave Remote Sensing of the Ocean: An Overview,n rate, and sea ice that have lead to significant advances in meteorological and oceanographic research as well as improvements in monitoring and forecasting both weather and climate. Future instruments are planned to measure sea surface salinity. The calibration of passive microwave radiometers has

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Direct Surface Current Field Imaging from Space by Along-Track InSAR and Conventional SAR,ations. However, despite the fact that a SAR is a Doppler radar, conventional SAR images do not provide direct information on target velocities, since all Doppler information is normally utilised to obtain the best possible spatial resolution under the assumption that targets are not moving. Recent

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,Scatterometer’s Unique Capability in Measuring Ocean Surface Stress,tress, which is the turbulent air-sea momentum exchange. The difficulty of finding a wind theory that is generally applicable to explain the ubiquitous spatial coherence of scatterometer measurements with ocean surface temperature and current is attributed to the overlook of the two ocean factors th

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Interpretation of SAR Signatures of the Sea Surface: A Multi-sensor Approach,the most complex and least understood data provided by remote sensing. The sea surface can appear featureless or contain the signatures of such diverse phenomena as surface and internal waves, upwelling, current boundaries, eddies, shallow water bathymetry, wind, storms, rainfall, convective rolls a

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Perspectives on Oil Spill Detection Using Synthetic Aperture Radar,e last decades, satellite based Synthetic Aperture Radar (SAR) images have been consistently and progressively used to achieve global monitoring of the seas. Satellite based oil spill detection is nowadays an operational service in Europe (CleanSeaNet run by EMSA), placing increasingly strict requir

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Absolute Dynamic Topography from Altimetry: Status and Prospects in the Upcoming GOCE Era,m the altimetric Mean Sea Surface height above the reference ellipsoid, or by estimating the ocean Mean Dynamic Topography and adding it to the altimetric sea level anomalies, which are known with centimeric accuracy. Huge improvements have been made since the launch of the first satellite altimeter

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The Marine Geoid and Satellite Altimetry,ectly observable, but its height above a reference ellipsoid may be calculated from a model of the Earth’s gravity field. Satellite altimeters measure the instantaneous sea surface height, which is the sum of the geoid plus the dynamic topography associated with the ocean’s responses to tidal and at