A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2019; you can also visit the original URL.
The file type is application/pdf
.
Beyond Craig and Gordon: A model of water vapor isotopologues in the marine boundary layer
2018
Atmospheric Chemistry and Physics Discussions
<p><strong>Abstract.</strong> We develop a one-dimensional (1D) steady state isotope marine boundary layer (MBL) model that includes meteorologically important features missing in Craig and Gordon type models, namely height-dependent diffusion/mixing, lifting to deliver air to the free troposphere, and convergence of subsiding air. Kinetic isotopic fractionation results from this height-dependent diffusion that starts as pure molecular diffusion at the air-water interface and increases with
doi:10.5194/acp-2018-709
fatcat:xkueynueojbhfdfrbaur5tjiyq