We report the first simultaneous eddy covariance flux measurements of CO2 and dimethylsulfide (DMS) over the open ocean for two North Atlantic cruises. After normalization for Schmidt number, the two gases give essentially identical gas transfer coefficients and wind speed dependences for the wind speed range 2–10 ms−1. The data indicate a linear relationship between the gas transfer coefficient and mean wind speed, with measured gas transfer coefficients slightly above the Wanninkhof (1992) parameterization, particularly at low wind speeds
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
We report the first simultaneous eddy covariance flux measurements of CO2 and dimethylsulfide (DMS) ...
We report the first simultaneous eddy covariance flux measurements of CO2 and dimethylsulfide (DMS) ...
We report the first simultaneous eddy covariance flux measurements of CO2 and dimethylsulfide (DMS) ...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air–sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air–sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air–sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air-sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air-sea fluxes and seawater concentr...
The air-sea gas transfer velocity k is frequently estimated as an empirical function of wind speed. ...
The air-sea gas transfer velocity k is frequently estimated as an empirical function of wind speed. ...
The air-sea gas transfer velocity (K-660) is typically assessed as a function of the 10-m neutral wi...
The air-sea gas transfer velocity (K660) is typically assessed as a function of the 10-m neutral win...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
We report the first simultaneous eddy covariance flux measurements of CO2 and dimethylsulfide (DMS) ...
We report the first simultaneous eddy covariance flux measurements of CO2 and dimethylsulfide (DMS) ...
We report the first simultaneous eddy covariance flux measurements of CO2 and dimethylsulfide (DMS) ...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air–sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air–sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air–sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air-sea fluxes and seawater concentr...
Shipboard measurements of eddy covariance dimethylsulfide (DMS) air-sea fluxes and seawater concentr...
The air-sea gas transfer velocity k is frequently estimated as an empirical function of wind speed. ...
The air-sea gas transfer velocity k is frequently estimated as an empirical function of wind speed. ...
The air-sea gas transfer velocity (K-660) is typically assessed as a function of the 10-m neutral wi...
The air-sea gas transfer velocity (K660) is typically assessed as a function of the 10-m neutral win...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...
Simultaneous air–sea fluxes and concentration differences of dimethylsulfide (DMS) and carbon dioxid...