Not exact matches
When it's cold enough to form
ice shelves that extend over the Antarctic
land mass and into the ocean, much of what drops to the seafloor is sand and gravel that the glacier has picked up
on its slow march from the continent's
ice cap.
However, most of the Antarctic glaciers are
on land, and rapidly adding new
ice shelf material to the floating
mass will increase sea level rise.
The timing and severity of
ice ages are determined by two major factors, namely the level of sunlight falling
on northern
land masses and the associated levels of atmospheric greenhouse gases.
Sea levels are effected by movement of
land masses both upward and downward, changes in gravitational pulls
on the water due to changes in
ice masses.
The timing and severity of
ice ages are determined by two major factors, namely the level of sunlight falling
on northern
land masses and the associated levels of atmospheric greenhouse gases.
Surely the issue relating to the
mass of the
ice sheet in the case of
on -
land ice sheets is precipitation as well as temperature.
The objective of the article that focuses
on land mass ice, being the more significant component, and Sea Ice being an anual effect stated, but not quantified, as the absolute measure being the more important eleme
ice, being the more significant component, and Sea
Ice being an anual effect stated, but not quantified, as the absolute measure being the more important eleme
Ice being an anual effect stated, but not quantified, as the absolute measure being the more important element.
However, most of the Antarctic glaciers are
on land, and rapidly adding new
ice shelf material to the floating
mass will increase sea level rise.
The confusion
on this subject lies in the fact that only about 2 percent of global warming is used in heating air, whereas about 90 percent of global warming goes into heating the oceans (the rest heats
ice and
land masses).
«A high - resolution record of Greenland
mass balance» «Antarctica, Greenland and Gulf of Alaska
land -
ice evolution from an iterated GRACE global mascon solution» «Greenland and Antarctica
ice sheet
mass changes and effects
on global sea level»
Need to take a global perspective,
on both sources and destination for the
mass exchange of waster into
ice and between
land and ocean that is likely to occur in the 21st Century.
AGW climate scientists seem to ignore that while the earth's surface may be warming, our atmosphere above 10,000 ft. above MSL is a refrigerator that can take water vapor scavenged from the vast oceans
on earth (which are also a formidable heat sink), lift it to cold zones in the atmosphere by convective physical processes, chill it (removing vast amounts of heat from the atmosphere) or freeze it, (removing even more vast amounts of heat from the atmosphere) drop it
on land and oceans as rain, sleet or snow, moisturizing and cooling the soil, cooling the oceans and building polar
ice caps and even more importantly, increasing the albedo of the earth, with a critical negative feedback determining how much of the sun's energy is reflected back into space, changing the moment of inertia of the earth by removing water
mass from equatorial latitudes and transporting this water vapor
mass to the poles, reducing the earth's spin axis moment of inertia and speeding up its spin rate, etc..
How «small» that is would depend
on the total
mass and area of the
land based
ice.
when the ocean is warm and the arctic is open, it snows more and moves water
mass from the oceans and adds
ice mass on land and the axis does shift.
We use realistic estimates of
mass redistribution from
ice mass loss and
land water storage to quantify the resulting ocean bottom deformation and its effect
on global and regional ocean volume change estimates.
It was evidence of the laws of physics at play
on the variably floating portion of the
ice mass at a breaking hinge point near the non-boiant
land born art of the entire
ice feature.
Mean sea level (MSL) evolution has a direct impact
on coastal areas and is a crucial index of climate change since it reflects both the amount of heat added in the ocean and the
mass loss due to
land ice melt (e.g. IPCC, 2013; Dieng et al., 2017) Long - term and inter-annual variations of the sea level are observed at global and regional scales.
AFAIK man was certainly
on the planet long before the end of the last
ice age, when there was an
ice cap covering a great deal of the Northern hemisphere
land mass (I don't know about the Southern).
You've got a 2 mile thick slab of
ice sitting
on a
land mass that is tough for any outside energy from atmosphere (and certainly not ocean) to penetrate.
Depending
on how the continents are arranged the global ocean conveyor belt changes and having a
land mass over a pole blocks warm water from getting at the
ice to melt it.
The cause would be melting of
ice on Greenland and other
land masses, since the melting of floating
ice would not change sea level.
So for
land ice, more snow falls
on Antarctica, but the
land ice mass is dropping due to increased calving rates.