the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
30 months dataset of glider physico-chemical data off Mayotte Island near the Fani Maoré volcano
Abstract. In May 2018, an unprecedented long and intense seismic-volcanic crisis broke out off the island of Mayotte (Indian Ocean) and was associated with the birth of an underwater volcano (Fani Maoré). Since then, an integrated observation network has been created (REVOSIMA), with the given objective of monitoring and better understanding underwater volcanic phenomena. Recently, an unmanned submarine glider (SeaExplorer glider) has been deployed to supplement the data obtained during a series of oceanographic surveys (MAYOBS) carried out on an annual basis. Operated by ALSEAMAR, the glider performed a continuous monitoring of 30 months of the water column from the sea surface to 1250 meters water depth with the objective to acquire hydrological properties, water currents and dissolved gas concentrations. This monitoring already showed that it is feasible and valuable to measure autonomously, continuously and at a high spatio-temporal scale, physical (temperature, salinity, ocean current) and biogeochemical parameters (O2, CH4, CO2, bubbles/droplets, vertical speeds anomalies related to droplets) over several months from a glider. In particular, innovating sensing capabilities (e.g., MINICO2, ADCP) have shown a great potential in the context of the Mayotte seismic volcano crisis, despite technical challenges (complex algorithms, sensor capabilities, etc.).
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Status: open (until 18 Jan 2025)
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RC1: 'Comment on essd-2024-377', Anonymous Referee #1, 22 Nov 2024
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This data paper present a unique dataset of glider data equipped of both hydrological, biogeochemical sensors to investigate the source, fate and fluxes of magmatic fluid into the ocean close to Mayotte.
This 30 months data-set combined measurements acquired with different sensors and an effort was made to fix discontinuity in the dataset.
The datapaper is well presented and illustrations are clear. The present datapaper is suitable to be published in ESSD but I have several comments to be adressed before.
The strategy of underwater glider profiles to detect fluid dynamics is not well described. It seems that a multiple yos strategy between the bottom and about 100m above the seabed was adopted. Please clarify. How is the impact of this strategy on the estimation of the currents? Please give some uncertainty.
Corrections were applied such as thermal lag on CTD measurements but also on O2 measurements. It would be useful to show some vertical profiles with and without corrections to show the effectiveness of the correction.
Two CTD sensors were used during the 30 months glider deployment, how do they compare or not? is there some periods with concomitant measurements?
Additional comments are included in the additional pdf files I added.
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