Radium concentration in water samples from the Northeast Atlantic, supplement to: Kromer, Bernd; Roether, Wolfgang (1983): Field measurements of air-sea gas exchange by the radon deficit method during JASIN 1978 and FGGE 1979. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A/B Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A/B24, 55-76

• Main Authors: Kromer, Bernd, Roether, Wolfgang
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 1983
• Subjects: Water sample; CTD/Rosette; M49; M51; M57; Meteor 1964; Northeast Atlantic
• Online Access: https://dx.doi.org/10.1594/pangaea.604844; https://doi.pangaea.de/10.1594/PANGAEA.604844

We present field measurements of air-sea gas exchange by the radon deficit method that were carried out during JASIN 1978 (NE Atlantic) and FGGE 1979 (Equatorial Atlantic). Both experiments comprised repeated deficit measurements at fixed position over periods of days or longer, using a previously descibed precise and fast-acquiaition, automatic radon measuring system. The deficit time series exhibit variations that only partly reflect the expected changes in gas transfer. By evaluating averages over each time series we deduce the following gas transfer velocities (average wind velocity and water temperature in parentheses):JASIN phase 1: 1.6 ± 0.8 m/d (at ~6 m/s, 13°C)JASIN phase 2: 4.3 ± 1.2 m/d (at ~8 m/s, 13°C)FGGE: 1.2 ± 0.4 m/d (at ~5 m/s, 28°C)0.9 ± 0.4 m/d (at ~7 m/s, 28°C)1.5 ± 0.4 m/d (at ~7 m/s, 28°C)The large difference betwen the JASIN phase 2 and FGGE values despite quite similare average wind velocity becomes even larger when the values are, however, fully compatible with the range of gas transfer velocities observed in laboratory experiments and the conclusion is suggested that their difference is caused by the highly different wind variability in JASIN and FGGE. We conclude that in gas exchange parameterization it is not sufficinent to consider wind velocity only. A comparison of our observations with laboratory results outlines the range of variations of air-sea gas transfer velocities with wind velocity and sea state.We also reformulate the radon deficit method, in the light of our observed deficit variations, to account explicitely for non-stationary and horizontal inhomogeneity in previous radon work introduces considerable uncertainty in deduced gas transfere velocity. We furthermore discuss the observational rewuirements that have to be met for an adequate exploitation of the radon deficit method, of which an observation area of minimum horizontal inhomogeneity and monitoring of the remaining inhomogeneities are thought to be the most stringent ones.