GNSS equipped buoys remain an important tool in altimetry validation. Progressive advances in altimetry missions require associated development in such validation tools. In this paper, we enhanced an existing buoy approach and gained further understanding of the buoy dynamics based on in situ observations. First, we implemented the capability to separate the ambiguity fixing strategy for different constellations in the processing software TRACK. A comparison between GPS and GNSS solutions suggested up to 3 cm reduction in the root mean square of the buoy minus co-located mooring SSH residuals over the selected sidereal periods. Then, comparison between double differencing and precise point positioning solutions suggested a possible common mode error external to GNSS processing. To assess buoy performance in different ocean conditions and sea states, GNSS and INS observations were used during periods where external forcings (waves, current and wind) were not interacting substantially. For the deployments investigated, no significant relationship was found, noting the maximum significant wave height and current velocity was ~2.3 m and ~0.3 m/s, respectively. In the lead up to the validation required for the SWOT mission, these results place important bounds on the performance of the buoy design under real operating conditions.
History
Sub-type
Article
Publication title
Remote Sensing
Volume
15
Issue
1
Article number
287
Pagination
1-22
eISSN
2072-4292
ISSN
2072-4292
Department/School
Australian Antarctic Program Partnership, Physics, Geography, Planning and Spatial Sciences
Publisher
MDPI AG
Publication status
Published
Place of publication
Switzerland
Rights statement
Copyright 2023 by the authors. Licensee MDPI, Basel, Switzerland.This article is an open access article distributed under the terms and conditions of the Creative Commons
Attribution (CC BY) license (https://creativecommons.org/licenses/by/
4.0/).
Socio-economic Objectives
280110 Expanding knowledge in engineering, 180506 Oceanic processes (excl. in the Antarctic and Southern Ocean)