Modeling the Distribution of OCS in the Lower Atmosphere of Venus

Astronomy and Astrophysics – Astronomy

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

Scientific paper

Recent high quality data of OCS from ground-based and Venus Express observations provide a unique opportunity to test our understanding of chemistry and transport in the atmosphere of Venus. OCS is produced by heterogeneous reactions on the surface; the middle atmosphere is a net sink for OCS. Thus, the spatial distribution of OCS in the middle atmosphere of Venus reflects a sensitive balance between chemistry and transport. A simple two-dimensional chemistry and transport (CTM) model is used to study the spatial distribution of OCS in the lower atmosphere of Venus. The residual circulation and horizontal eddy diffusivities are derived from winds from Lee et al's (2007) general circulation model. The results from our 2-D CTM are compared to recent observations. There is generally good agreement between the model and data. The sulfur chemistry in the lower atmosphere of Venus remains highly uncertain. New laboratory experiments and observations are urgently needed.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Modeling the Distribution of OCS in the Lower Atmosphere of Venus does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Modeling the Distribution of OCS in the Lower Atmosphere of Venus, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Modeling the Distribution of OCS in the Lower Atmosphere of Venus will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1066726

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.