coastline which contributes/requires reconciling altimetry, tide gauge and vertical land motion. The fundamental use of the MDT computed using altimetry, ocean models or through the use of tide gauges has values of between -2 and +1 meters at different points in the ocean. However, close to the coast the determination of the MDT is problematic due to i.e., the altimeter footprint, land motion or parameterization/modelling of coastal currents. The presentation also outlines a new addendum to the project on the use of GPS reflectometry as Coastal tide gauge and the correspondence with SAR altimetry from Cryosat-2 and Sentinel-3.
|Publication status||Published - 2018|
|Event||25 years of progress in radar altimetry symposium - , Portugal|
Duration: 24 Sep 2018 → 29 Sep 2018
|Conference||25 years of progress in radar altimetry symposium|
|Period||24/09/2018 → 29/09/2018|