Air-Sea CO2 flux measurements from an autonomous drifting buoy in July-August 2016 in the Jade Bay

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Bibliographic Details
Main Authors: Ribas-Ribas, Mariana, Wurl, Oliver
Format: Dataset Open Access
Language:en
Published: PANGAEA 2017
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author Ribas-Ribas, Mariana
Wurl, Oliver
author_facet Ribas-Ribas, Mariana
Wurl, Oliver
collection Datos científicos de ciencias marinas y ambientales
contents Data from autonomous, drifting buoy with a floating chamber to measure air-sea CO2 fluxes and gas transfer velocities (k) with high temporal and spatial resolution. The buoy is equipped with a sensor to measure aqueous and atmospheric pCO2, and to monitor the increase or loss of CO2 inside the chamber. Two complete cycle last 70 minutes, and after flushing the chamber a new cycle is initiated. The buoy can be deployed for more than 15 hours, and at wind speeds of up to 10 m/s. Floating chambers are known to overestimate fluxes due to the creation of additional turbulence at the water surface. We correct fluxes by measuring turbulence with two Acoustic Doppler Velocimeter, one directly underneath the center of the floating chamber and the other one positioned sideways to measure turbulence outside the perimeter of the buoy.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_873428
institution PANGAEA
language en
publishDate 2017
publisher PANGAEA
record_format pangaea
spellingShingle Air-Sea CO2 flux measurements from an autonomous drifting buoy in July-August 2016 in the Jade Bay
Ribas-Ribas, Mariana
Wurl, Oliver

Data from autonomous, drifting buoy with a floating chamber to measure air-sea CO2 fluxes and gas transfer velocities (k) with high temporal and spatial resolution. The buoy is equipped with a sensor to measure aqueous and atmospheric pCO2, and to monitor the increase or loss of CO2 inside the chamber. Two complete cycle last 70 minutes, and after flushing the chamber a new cycle is initiated. The buoy can be deployed for more than 15 hours, and at wind speeds of up to 10 m/s. Floating chambers are known to overestimate fluxes due to the creation of additional turbulence at the water surface. We correct fluxes by measuring turbulence with two Acoustic Doppler Velocimeter, one directly underneath the center of the floating chamber and the other one positioned sideways to measure turbulence outside the perimeter of the buoy.
title Air-Sea CO2 flux measurements from an autonomous drifting buoy in July-August 2016 in the Jade Bay
topic
url https://doi.org/10.1594/PANGAEA.873428