A previously developed renewal model included parameterizations for the thermal skin effect and interfacial gas transfer velocity. The more readily available cool skin data were used for an adjustment of the gas transfer parameterization. In this work, the renewal concept is extended to include the velocity difference across the viscous sublayer and to account for the stage of surface wave development. As a result, the empirical coefficients that enter the renewal model have been specified more accurately using laboratory data on the surface wind drift current. In addition, the coefficient linking the cool skin and gas transfer parameterization formulas has been determined from the probability distribution function for renewal events. A com...
For sparingly soluble gases, theory predicts that the gas transfer velocity, k, is controlled by tur...
The aqueous thermal boundary layer near to the ocean surface, or skin layer, has thickness O(1 mm) a...
A 1-dimensional slab model is developed that describes the deepening of the well-mixed surface layer...
A previously developed renewal model included parameterizations for the thermal skin effect and inte...
Heat and gas transport in molecular sublayers at the air-sea interface is governed by similar laws. ...
Absorption of solar radiation within the thermal molecular sublayer of the ocean can modify the temp...
Previously, we reported on laboratory results from a wind-wave tunnel comparing transfer velocities ...
Measurements of the Gas-Exchange Experiment GasEx-98 that took place in the North Atlantic Ocean fro...
The gas flux of weakly soluble gases through the air–sea interface is controlled by the transport me...
The primary purpose of this project was to evaluate and improve models for the bulk-skin temperature...
[1] During the two recent GasEx field experiments, direct covariance measurements of air-sea carbon ...
The nonlinear dependence of gas transfer velocity on wind speed typically results in the best fit of...
Although the air-sea gas transfer velocity k is usually parameterized with wind speed, the so-called...
One of the dominant sources of uncertainty in the calculation of air–sea flux of carbon dioxide on a...
The gas transfer at the water surface is more complicated than the bulk aerodynamic relation for the...
For sparingly soluble gases, theory predicts that the gas transfer velocity, k, is controlled by tur...
The aqueous thermal boundary layer near to the ocean surface, or skin layer, has thickness O(1 mm) a...
A 1-dimensional slab model is developed that describes the deepening of the well-mixed surface layer...
A previously developed renewal model included parameterizations for the thermal skin effect and inte...
Heat and gas transport in molecular sublayers at the air-sea interface is governed by similar laws. ...
Absorption of solar radiation within the thermal molecular sublayer of the ocean can modify the temp...
Previously, we reported on laboratory results from a wind-wave tunnel comparing transfer velocities ...
Measurements of the Gas-Exchange Experiment GasEx-98 that took place in the North Atlantic Ocean fro...
The gas flux of weakly soluble gases through the air–sea interface is controlled by the transport me...
The primary purpose of this project was to evaluate and improve models for the bulk-skin temperature...
[1] During the two recent GasEx field experiments, direct covariance measurements of air-sea carbon ...
The nonlinear dependence of gas transfer velocity on wind speed typically results in the best fit of...
Although the air-sea gas transfer velocity k is usually parameterized with wind speed, the so-called...
One of the dominant sources of uncertainty in the calculation of air–sea flux of carbon dioxide on a...
The gas transfer at the water surface is more complicated than the bulk aerodynamic relation for the...
For sparingly soluble gases, theory predicts that the gas transfer velocity, k, is controlled by tur...
The aqueous thermal boundary layer near to the ocean surface, or skin layer, has thickness O(1 mm) a...
A 1-dimensional slab model is developed that describes the deepening of the well-mixed surface layer...