Melting of Antarctica's ice shelves occurs underwater, based on warming ocean water. which melts the shelves from underneath. This phenomenon occurs all year and is not limited to summer.
The summer temperatures in Antarctica are not warm enough to melt the ice sheet.
Your question is really about ice shelves, not the Antarctic ice sheet. The ice shelves are deteriorating because of warmer ocean waters that melt the ice shelf from below.
The Ross Ice Shelf and the Ronnie Ice Shelf are the two biggest ice shelves in Antarctica.
Antarctica is a continent and continents do not melt. However, during the summer months of 2012, melting of the ice sheet did occur, and during the winter months of 2012 and 2013, the ice sheet froze again.
Because when it's summer most of the ice melt in the winter everything is covered in snow :p
Antarctica is a continent, and continents do not melt. However, the ice shelves attached to 44% of the continent are disintegrating, due to the warming of the Southern Ocean. The ice sheet that covers 98% of the continent melts and freezes cyclically.
The ice shelves attached to Antarctica have begun to disintegrate -- melt, because of warming ocean waters. The Ross and Ronne have not been as severely affected as have the Larson ice shelves east of the Trans Antarctic mountains. Any melting of ice shelves will contribute to rising ocean levels all over the planet, which can displace people living at or near sea level. You can learn more about their concerns with a visit to antarcticglaciers.org.
A person in Antarctica who wanted fresh water would apply heat to melt ice.
Ice shelves are attached to about 44% of the continent. Less than 40 named shelves remain in July 2015.
pak you XD
Ice shelves in Antarctica are melting at an accelerating rate due to warming ocean temperatures and increased melting from the bottom. This can lead to the destabilization of the ice shelves and contribute to rising sea levels as more ice flows into the ocean. Scientists are closely monitoring these changes to understand their impact on the stability of the Antarctic ice sheet.
The centre of Antarctica has had snow falling on it for about 100,000 years. This snow doesn't melt but becomes ice with the weight of more snow on top. This is 7 million cubic miles (30 million cubic km) of ice.This huge weight of ice forces the ice outwards radially all round the coast in the form of ice shelves that float out on the surface of the ocean. Some of these shelves rest on the sea bed. The ocean is warming and the warmer water melts the ice underneath the shelves, so the shelves become thinner and break off to form icebergs.