Land - based ice in glaciers and ice - sheets will keep contributing to sea level rise as long as melting
exceeds snowfall accumulation; stopping the growth of temperature would not stop the net melting.
Not exact matches
The Greenland, and possibly the Antarctic, ice sheets have been losing mass recently, because losses by ablation including outlet glaciers
exceed accumulation of
snowfall.
Like a glacier, an ice sheet forms through the
accumulation of
snowfall, when annual
snowfall exceeds annual snowmelt.
The remainder of the ice loss from Greenland has occurred because losses due to melting have
exceeded accumulation due to
snowfall.