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Albedo Effect

     While melting glaciers are caused by global warming, glaciers melting can also impact the temperatures across the globe. According to Wikipedia, the albedo (a measure of the reflective ability of a surface) of snow is about 0.8 to 0.9. This means that snow-covered glaciers can reflect back about 80% to 90% of the energy from the sun’s rays.

 

     So when ice on glaciers melts, the reflective properties of the glaciers are lost. The earth beneath the ice sheets gets uncovered. The glacier then absorbs more heat, which in turn causes more of its ice sheets to melt away, resulting in further increase in the global temperatures. This phenomena is called ‘ice-albedo feedback’.

 

 

 

     Professor Peter Wadhams from Cambridge University, UK, is an expert on Arctic ice. He said white ice reflects more sunlight than open water, acting like a parasol. Melting of white Arctic ice, currently at its lowest level in recent history, is causing more absorption.

 

     Prof Wadhams calculates this absorption of the sun's rays is having an effect "the equivalent of about 20 years of additional CO2 being added by man".

 

   The Cambridge University expert says that the Arctic ice cap is "heading for oblivion".

 

   In 1980, the Arctic ice in summer made up some 2% of the Earth's surface. But since then the ice has roughly halved in area.

 

   "Thirty years ago there was typically about eight million square kilometres of ice left in the Arctic in the summer, and by 2007 that had halved, it had gone down to about four million, and this year it has gone down below that," Prof Wadhams said.

 

   And the volume of ice has dropped, with the ice getting thinner:

   "The volume of ice in the summer is only a quarter of what it was 30 years ago and that's really the prelude to this final collapse," Prof Wadhams said.

 

     Parts of the Arctic Ocean are now as warm in summer as the North Sea is in winter, Prof Wadhams said.

Vatnajökull, Iceland

Reference article & vidio

Arctic ice melt 'like adding 20 years of CO2 emissions'

By Susan WattsNewsnight Science editor, BBC News

 
http://www.bbc.com/news/science-environment-19496674

     The polar ice cap acts as a giant parasol, reflecting sunlight back into the atmosphere in what is known as the albedo effect. But white ice and snow reflect far more of the sun's energy than the open water that is replacing it as the ice melts.

 

 

    Instead of being reflected away from the Earth, this energy is absorbed, and contributes to warming:

 

    "Over that 1% of the Earth's surface you are replacing a bright surface which reflects nearly all of the radiation falling on it with a dark surface which absorbs nearly all.

 

    "The difference, the extra radiation that's absorbed is, from our calculations, the equivalent of about 20 years of additional CO2 being added by man," Prof Wadhams said.

 

 

    If his calculations are correct then that means that over recent decades the melting of the Arctic ice cap has put as much heat into the system as all the CO2 we have generated in that time. And if the ice continues to decline at the current rate it could play an even bigger role than greenhouse gases.

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