A new study shows that glacier ice walls are vital for the climate, Inland Antarctic ice contains volumes of water that can raise global sea levels by several meters. A new study shows that glacier wall glaciers are very important for the climate, because they prevent rising sea temperatures and melting glaciers.

The ocean can store more heat than the atmosphere. The deep sea around Antarctica stores the heat associated with warming the air over the continent by 400 degrees.

Current measurements show an increase in melting, especially near the coast in parts of Antarctica and Greenland.

This increase may be related to warm, salty ocean currents that circulate on the continental shelf and melt the ice beneath, researchers say.

The inland Antarctic Ice is gradually moving towards the ocean. Although ice cream is very important, its stability remains a mystery, as is the answer to what can make it melt faster. A new study shows that glacier ice walls are vital for the climate.

Because glaciers are difficult to access, researchers cannot find much information about active processes.

Hertz has a floating section as thick as 300 to 800 meters, below which there is sea water that connects to the ocean outside.

The glacier ends on a vertical edge, a wall of ice that extends 300 to 400 meters into the sea. Below this edge, warm sea water flows into continents and deeper ice in the south.

If we examine instrument measurement data, we find that ocean currents are blocked by ice edges. This limits the extent to which warm water can reach continents

We now understand that only a small amount of electricity can penetrate the glacier, researchers say. This means that about two-thirds of the heat that reaches the continental shelf from the deep ocean never reaches ice. A new study shows that glacier ice walls are vital for the climate.

The results of the study have given researchers a better understanding of how this glacier area works.

“From the Getz Glacier we get measurements of heat transfer in the ocean corresponding to melting ice measured by satellites.

This also means that floating glaciers, especially ice surfaces, are the main areas that need to be monitored closely. When the ice wall disappears, more heat is given to the ice on land.

Therefore, we no longer expect a direct link between rising winds from the west and rising ice melts.

Conversely, increased water levels can be caused by processes that pump warmer and heavier water to the continental shelf, such as when a low pressure system approaches the continent.

The researchers believe that this study has given them a far better tool to predict future water levels and make more accurate climate predictions. The continental shelf is part of the seabed, which is one of the tectonic plates. In general, continental shelf has a depth of 0 to 500 meters and ends on a continental slope.