Direct measurements of ocean surface velocity from space: Interpretation and validation

By Bertrand Chapron, Fabrice Collard, Fabrice Ardhuin. 2005

379 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Oceanography

View Paper: https://www.semanticscholar.org/paper/7bdc06686dea3ea4dfd7ce3eae3f680794bb8775

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Earth-Surface Processes

In Oceanography

Citations in the corpus

Small-scale open-ocean currents have large effects on wind-wave heights (2017, background): “In this context, the measurement noise and possible errors are of particular interest, and some of these errors are related to waves [e.g., Peral et al., 2015; Chapron et al., 2005].”
Three‐dimensional reconstruction of oceanic mesoscale currents from surface information (2008, background): “…for the Gulf Stream region, early space-borne optical [Strong and DeRycke, 1973] as well as recent radar high-resolution observations [e.g., Chapron et al., 2005] have enabled the identification of very well delineated surface signatures of the upper ocean mesoscales (30 km-200 km) and…”
The physical oceanography of the transport of floating marine debris (2020, methodology): “Finally, in recent years, the technology to measure surface currents directly using Doppler scatterometry have been demonstrated using airborne and spaceborne sensors (Chapron et al 2005, Romeiser et al 2010, Kudryavtsev et al 2012, Rodríguez et al 2018).”
Global C-Band Envisat, RADARSAT-2 and Sentinel-1 SAR measurements in copolarization and cross-polarization (2015, background): “For almost 10 years (2002–2012), ENVISAT ASAR provided large amount of high quality wide swath C-band radar images in vertical (VV) or horizontal (HH) copolarization, illustrating the potential to resolve fine-scale atmospheric and oceanic features, as well as to interpret and possibly exploit the e”
A global wave parameter database for geophysical applications. Part 1: Wave-current turbulence interaction parameters for the open ocean based on traditional parameterizations (2008, methodology): “, 2006), and third moments of the frequency spectrum, to be used for the correction of ocean currents derived from Along-Track interferometry or Doppler analysis methods (Chapron et al., 2005).”