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using the Magnus formula ( Murray 1967 ) and a constant salinity correction factor of 0.98. The parameterization of the bulk transfer coefficient C E additionally depends on the air temperature, which is estimated from the sea surface temperature by the mean of the assumptions of 80% humidity and 1 K sea–air temperature difference. However, the impact of these assumptions on the accuracy of C E is regarded to be of secondary order ( Liu et al. 1994 ). 2) Precipitation Similar to the wind speed
using the Magnus formula ( Murray 1967 ) and a constant salinity correction factor of 0.98. The parameterization of the bulk transfer coefficient C E additionally depends on the air temperature, which is estimated from the sea surface temperature by the mean of the assumptions of 80% humidity and 1 K sea–air temperature difference. However, the impact of these assumptions on the accuracy of C E is regarded to be of secondary order ( Liu et al. 1994 ). 2) Precipitation Similar to the wind speed
