An analysis of acetone (CH3COCH3) and acetonitrile (CH3CN) measurements, pe
rformed during the Indian Ocean Experiment (INDOEX), using a chemistry gene
ral circulation model is presented. A comparison with measurements indicate
s that the model simulates realistic CO and acetone distributions, except t
oward the Indian west coast near the surface. The latter may be related to
a sea breeze circulation at the Indian west coast, which is not resolved by
the model. A comparison of the measured and modeled correlation between CO
and acetone indicates the presence of a background marine acetone source.
A model sensitivity study suggests a global marine emission strength of 15-
20 Tg acetone yr(-1), which is a significant contribution to the estimated
global acetone source of 56 (37-80) Tg acetone yr(-1). The comparison of me
asured and modeled CO-acetonitrile correlation from surface measurements in
dicates that a model sink of acetonitrile in the marine boundary layer is m
issing. A model sensitivity study suggests that this could be dry depositio
n (deposition velocity estimate: 0.01-0.05 cm s(-1)) on the ocean surface.
A comparison of measured and modeled tropospheric acetonitrile indicates th
at the model overestimates the free tropospheric acetonitrile mixing ratios
up to a factor of 3, which points to a missing free tropospheric sink of a
cetonitrile in the model. A possible explanation may be stratospheric loss
and subsequent stratosphere-troposphere exchange, which was not included in
the model.