As albedo in the Arctic region is getting higher, incoming radiant energy of the sun will be more reflected. If albedo in the Arctic region is falling, incomig radiant of the sun will be more absorbed.
Albedo is a name of overall reflectivity in terms of the Sun's spectrum.
Can’t see diagram. Could you attach the photo.
I am pretty sure Osmosis sorry if Im wrong
<span>nothing actually happens to convection currents when heat is no longer supplied.
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