The Greenland ice SHEET is melting at an accelerating rate, now over 100 cubic kilometers per year, which contributes about 0.35mm by itself to sea level rise each year.
Source:
Ramillien, G., A. Lombard, A. Cazenave, E. R. Ivins, M. Llubes, F. Remy, and R. Biancale (2006), Interannual variations of the mass balance of the Antarctica and Greenland ice sheets from GRACE, Global Planet.Change, 53(3), 198-208, doi: DOI: 10.1016/j.gloplacha.2006.06.003.
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The ice sheets in Greenland are melting due to a combination of factors, including rising global temperatures caused by human activities such as burning fossil fuels, deforestation, and industrial processes. This leads to increased melting at the surface, as well as the calving of icebergs at the edges of the ice sheet. The meltwater also contributes to rising sea levels, which can have significant impacts on coastal communities worldwide.
The only thing to do to stop the Greenland ice cap melting it to slow and eventually reverse global warming.
To do this we have to stop emitting carbon dioxide into the atmosphere. This is mostly done when we burn fossil fuels (coal, oil and natural gas) in industry, transport and to generate electricity.
We also cut down great forests all around the world, which used to absorb and store carbon.
So we have to quickly find other ways of powering transport and generating electricity, and we have to replant the forests.
Global warming is melting ice all over the world. In Greenland there are ravines in the ice which are allowing melt water to go down to the rock under the ice cap. This seems to be letting glaciers move faster towards the sea where they break off to form icebergs.
Glaciers all over the world are melting. There are individual glaciers here and there that are not melting constantly, or even have periods of growth. This does not change the fact that on average the world's glaciers are seriously melting.
this, of course has serious consequences for the great rivers of the world and the people who rely on them for existence, because glaciers are the source for many of these rivers, and if the glaciers disappear, the rivers will be seriously diminished.
The amount of ice lost from 1986-1995 was double the mass loss of 1976-1985, and the mass loss from 1986-1995 was more than double again, according to the World Glacier Monitoring Service, which has been collecting data on glaciers since 1946.
The world is getting warmer. This is probably the result of the buildup of carbon dioxide in the atmosphere, resulting from the burning of fossil fuels for the past few centuries.
A) Too fast too soon; and B) water running to the base of Glaciers acts as a process speeding lubricant; and C) the outflow of cold, fresh water can shut down the warm Atlantic Gulf Stream.
Ice sheets exist in Greenland and Antarctica today. Greenland's ice sheet is the second largest in the world, while Antarctica's ice sheet is the largest and contains about 90% of the world's ice. These ice sheets play a crucial role in regulating global sea levels and climate.
These are known as ice sheets, massive expanses of glacial ice that cover land areas. Antarctica and Greenland have the largest ice sheets in the world, containing the majority of Earth's fresh water. The ice sheets can be several kilometers thick and have a significant impact on global climate and sea levels.
They are called ice sheets and/or continental glaciers if they cover more than 50,000 square kilometers of land area.continental
An ice sheet is a large mass of glacial ice that covers an area greater than 50,000 square kilometers. Ice sheets can be found in Antarctica and Greenland and play a significant role in regulating global climate by reflecting sunlight and storing freshwater. They are a key indicator of climate change, as their melting can contribute to rising sea levels.
An ice shelf is a floating ice platform attached to a coast, while an ice sheet is a vast expanse of land ice covering an area larger than 50,000 square kilometers. Ice shelves are mostly found in Antarctica and Greenland, whereas ice sheets cover large portions of Antarctica and Greenland, as well as parts of the Arctic.