Not exact matches
So no matter how
far you end up off of the beaten path, Bogs Classic will help to keep you
warm, dry,
grounded, and camouflaged!
Covering the
ground as
far as the eye could see were large rocks and boulders, constantly tripping me in my cumbersome standard - issue «bunny boots» — white, clownlike shoes with a sole about an inch thick and little valves on the side to restrict the outflow of
warm air.
Since so much of the ice sheet is
grounded underwater, rising sea levels may have the effect of lifting the sheets, allowing more - and increasingly
warmer - water underneath it, leading to
further bottom melting, more ice shelf disintegration, accelerated glacial flow, and
further sea level rise, and so on and on, another vicious cycle.
And with each increment of
warming, ice would retreat
further, vegetation would advance accordingly, and more greenhouse gases would be released from ocean waters or frozen
ground.
Warm waters have been eating away at ice from below in this region, and once
grounding lines retreat
far enough inland, entire glaciers can become unstable and collapse.
So it's by
far the simplest to chose
warm - toned pastels, and
ground them with one piece in a dark cool tone like a deep, dark blue or black.
Remember that a clear night is colder by
far than a cloudy one, and whether a cloud is cooling or
warming depends on how high it is: high clouds radiate back out into space, low clouds are just «high
ground» as
far as
warming the air is concerned.
The ocean surface
warmed a bit, too, releasing carbon dioxide to the atmosphere and strengthening the
warming trend
further, and as frozen
ground thawed, the potent greenhouse gas methane would have been released as well, increasing the «longwave forcing».
http://upload.wikimedia.org/wikipedia/commons/b/b7/AntarcticBedrock.jpg The
further it retreats, the deeper the
grounding line gets, and the more efficient the thermohaline pump where heavy
warmer salt water dives to replace fresh meltwater at the
grounding line.
«Glaciers in higher colder mountainous regions will be slower to melt even as temps rise, the lower tundra areas will respond more quickly to such changes and this is shown by the quicker responses in tree line to the lesser
warming periods like the MWP at
ground level
further north from him, and not just fossil remains but old farming settlements uncovered, and so on.»
However, I admit I do not understand why he was opposed to handing the information over to Keenan as he has no axe to
grind as
far as temperature is concerned or global
warming (which is something that came very late in his career and was probably of little interest to him).
At some later time (e g the
warm early Holocene) the ice cap might change to being
warm - based and start eroding the
ground it is lying on, in which case the eemian mosses may be
far from their original position.
There are also concerns that pumping sequestered CO2 into oil and gas wells to help make the fuels easier to pump out of the
ground will lead to
further consumption of fossil fuels, and CO2 emissions, thus adding to global
warming.
Therefore that IR scattering back to the surface CAN NOT
warm the surface any
further because the atoms and molecules of the
ground are already kinetically excited to this level.
These effects are magnified by snow and ice: by reducing snow and ice cover,
warming reduces the reflectivity of the
ground and allows more solar energy to be absorbed,
further increasing the
warming; conversely for cooling.»
The Pine Island glacier is
grounded on continental bedrock below sea level, which means that
warming ocean water could penetrate
far inland beneath the shelf, without anyone being conscious of any change.
The long (30 years) trend of conventional
ground / city based land data is so
warm that the gaps / peaks never reaches back to equilibrium, in fact they go
further and
further from equilibrium which at some point is difficult to explain thermodynamically.