Not exact matches
That size means gravity has pulled Ceres into a sphere, with a core of rock, an icy coating and perhaps an
ocean of
liquid water locked
between.
Scientists don't want to risk a run - in
between Juno and any of the icy moons, such as Europa, which could conceivably harbor life in its buried
liquid water
ocean.
Either because there's flow through the subsurface
between the seas or because the channels
between them allow enough
liquid to pass through, the
oceans on Titan are all at the same elevation.
Imagine that you are floating thousands of kilometres below the surface of a vast
ocean that is neither
liquid nor gas, but somewhere in
between.
Because the interiors of icy planetary bodies might also be salty, due to interactions
between the ice and the surrounding rocks or a
liquid ocean, lead author Livia Eleonora Bove of the CNRS & Université Pierre et Marie Curie in France and the Ecole Polytechnique Federal de Lausanne in Switzerland and the rest of the team studied the effects of salts on the formation of the ice X from ice VII.
-LSB-...] with hypotheses including that of a possible shared atmosphere
between Pluto and Charon, to the possible existence of past
liquid water
oceans inside Charon billions of years ago.
One wonders if the sound of the Atlantic
Ocean's drift
between Granger Bay and Three Anchor Bay inspired the naming of this coastal portion lending itself gently to Wikipedia's suggestion that «Mouille is a phonetic term that applies to certain consonants having a palatalised, «
liquid» or softened sound».
There is no surprise that the CO2 in the atmosphere winds up partially in the
oceans, nor that the amount of CO2 going into or coming out of the
oceans varies in time and space — that's simple equilibrium chemistry
between the
liquid (that is, dissolved) and gaseous phases, and does explain part of the variability about the long term rising trend.
You state in the response to # 10, ``... There is no surprise that the CO2 in the atmosphere winds up partially in the
oceans, nor that the amount of CO2 going into or coming out of the
oceans varies in time and space — that's simple equilibrium chemistry
between the
liquid (that is, dissolved) and gaseous phases...» Are the buffers a part of simple equilibrium chemistry, and where can I go to read up on this and how it pertains to the Models.
While there are some similarities
between the approaches, an important difference is that the slab -
ocean approach allows surface and MBL temperatures to adjust to the energetic perturbation: positive energetic forcing of the surface leads to warming, weakens the inversion, and reduces low - cloud cover and
liquid water path (LWP).
The main difference
between H2O and CO2 (apart from the numerical differences of their specific physical properites such as degree of freedom, thermal capacity, physical mass, etc) in terms of their effects on the atmosphere is that water is capable of condensing into
liquid to form clouds and readily and rapidly moves
between surface and atmosphere, daily, seasonally, annually and on even greater time scales, but CO2 does not liquify in the biosphere and transfers over mostly long time periods
between surface (primarily
oceans, seas, etc) and the atmosphere.
Relationship
between decadal variations in temperatures in the Pacific and the tropopause identified From the HELMHOLTZ CENTRE FOR
OCEAN RESEARCH KIEL (GEOMAR) Water plays a major role for our planet not only in its
liquid form at the surface.