[astro-ph.EP] The knowledge of Titan’s near-surface atmosphere is sparse. The Huygens descent probe measured winds, and the multiple dune field observations and possible dust storms suggest active near-surface dynamics.
Huygens
Topographically Forced Stationary Waves Can Explain The Near-Surface Zonal Winds Observed By Huygens On Titan
[astro-ph.EP] Titan’s equatorial superrotation is associated with climatological retrograde (westward) near-surface winds at low latitudes, as consistently simulated by Titan general circulation models.
Thermal Inertia Controls on Titan’s Surface Temperature and Planetary Boundary Layer Structure
Understanding Titan’s planetary boundary layer (PBL) — the lowest region of the atmosphere influenced by surface conditions — remains challenging due to Titan’s thick atmosphere and limited observations.
The Top 10 Huygens Discoveries At Titan
On 14 January 2005, at 13:34 CET (12:34 UTC), ESA’s Huygens probe entered the history books by descending to the surface of Titan, Saturn’s largest moon.
Titan’s Fluvial and Lacustrine Landscapes
In this chapter we begin with a review of Titan’s fluvial and lacustrine landscapes as observed with Cassini remote sensing data, and what the many discoveries have revealed about Titan’s […]
Titan’s Rocks Of Ice – An Interview with Christopher McKay
Huygens sent back only one picture from the surface of Titan. Some people ask, “Are there any more pictures?” They’re used to the Mars rovers, where every day you get […]
