Abstract

Validation of satellite-based retrieval of ocean parameters like Sea Surface Temperature (SST) and Sea Surface Salinity (SSS) is commonly done via statistical comparison with in situ measurements. Because in situ observations derived from coastal/tropical moored buoys and Argo floats are only representatives of one specific geographical point, they cannot be used to measure spatial gradients of ocean parameters (i.e., two-dimensional vectors). In this study, we exploit the high temporal sampling of the unmanned surface vehicle (USV) Saildrone (i.e., one measurement per minute) and describe a methodology to compare the magnitude of SST and SSS gradients derived from satellite-based products with those captured by Saildrone. Using two Saildrone campaigns conducted in the California/Baja region in 2018 and in the North Atlantic Gulf Stream in 2019, we compare the magnitude of gradients derived from six different GHRSST Level 4 SST (MUR, OSTIA, CMC, K10, REMSS, and DMI) and two SSS (JPLSMAP, RSS40km) datasets. While results indicate strong consistency between Saildrone- and satellite-based observations of SST and SSS, this is not the case for derived gradients with correlations lower than 0.4 for SST and 0.1 for SSS products.

Highlights

  • The paper aims to follow-up on the work of [1], where the authors compared sea surface temperatures (SSTs) and sea surface salinities (SSSs) from the Saildrone deployment along the California and Baja coasts with satellite-derived products

  • For SST, six GHRSST compliant Level 4 products were used for the comparison, namely the Multi-Scale Ultra-High Resolution (MUR) SST, the Operational Sea Surface Temperature and Sea Ice Analysis (OSTIA) SST, the Canadian Meteorological Center (CMC) SST, the NAVOCEANO K10 SST, the Remote Sensing Systems (RSS) REMMS_MW_IR SST and the Danish Meteorological Institute (DMI) SST

  • The unique ability of Saildrone to sample at high spatio-temporal resolutions over an extended period allows for the validation of both SST, SSS, and their corresponding gradients using data from two separate campaigns conducted in the California/Baja region and in the North Atlantic Gulf Stream

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Summary

Introduction

The paper aims to follow-up on the work of [1], where the authors compared sea surface temperatures (SSTs) and sea surface salinities (SSSs) from the Saildrone deployment along the California and Baja coasts with satellite-derived products. We extend the previous results by comparing satellite-based SST and SSS gradients with Saildrone measurements.

Results
Conclusion

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