Titan has
a thin atmospheric layer of roughly constant temperature above the troposphere, followed by an extensive stratosphere ranging from 50 to 200 km (30 to 120 miles) in altitude, where temperatures steadily increase with altitude to a maximum of 160 to 180 K (− 172 to − 136 °F, − 113 to − 93 °C).
Not exact matches
In his early career, Olitski depicted abstract shapes with thick, heavily impastoed surfaces, but later took to
layering thin films of spraypaint onto his canvases, creating a trademark
atmospheric effect.
The standard assumption has been that, while heat is transferred rapidly into a relatively
thin, well - mixed surface
layer of the ocean (averaging about 70 m in depth), the transfer into the deeper waters is so slow that the
atmospheric temperature reaches effective equilibrium with the mixed
layer in a decade or so.
The visible hydrate was found as
thin icelike
layers that released methane gas initially upon retrieval, but stabilized for up to 4 h at
atmospheric pressure conditions and subfreezing temperatures.