Snapshots of the 2012/2013 summer on the frozen continent

Scientists studying Antarctic’s Ross Ice Shelf found that the ice emits a strange sound as the ice begins to melt. The team of scientists stumbled on this finding, never having heard the weird noise the upper layers of ice create.

The team of scientists, who recently published their research in Geophysical Research Letters, found that both wind and melting cause the surface slabs of ice on the Ross Ice Shelf to vibrate, producing strange sounds as a result.

Extremely sensitive seismic sensors were used to monitor the sound patterns across the Ross Ice Shelf in western Antartica. The initial intent of the research was not to measure this acoustic anomaly but to study the crust and mantle beneath Antarctica.

After 2 years of listening to the surface layers of the Ross Ice Shelf, scientists found that the ice nearly continuously “sings” in different frequencies depending on wind and melting. The singing is produced from high-frequency wave trapped in the upper couple meters of snow. As winds blow across the ice shelf, they vibrate these upper layers, called firn. The seismic sensors, buried within the firn layers, can measure and record these waves and their “sound” through time.

Frost and firn after a snowstorm.

Unexpectedly, the researchers found that the pitch of the sound from the ice shelf changed when temperatures rose to above freezing and the ice began to melt. The sound waves began to slow down and the pitch dropped as a response. This was an indication of both melting and degree of melting. Once temperatures dipped below freezing again, the upper firn refroze but did not regain the initial pitch it had before the firn melted. This could be an indication that once melted, the upper layers of ice shelves do not simply return back to original form.

Scientists are keen to measure and understand the characteristics of melting in Antarctica and the upper firn layers as they represent a key variable in sea level rise over the coming decades. It is estimated that if the Antarctic Ice Sheets melted in entirety sea level would rise by 60 meters (197 feet).

Ice Highway on Ross Ice Shelf, Ross Island, Antarctica

In the worst case scenario where all land ice has melted and drained into the oceans, scientists estimate that sea level will rise by 216 feet. It’s important to note that even on rapid timescales this process would take thousands of years. If it did happen, however, our world would look quite different, with most coastal cities sitting squarely in the ocean.

Through constant seismic monitoring of ice shelves in Antarctica, we can understand and project into the future what we expect for sea level rise. Whether you’re a global oil and gas giant considering where to build your next coastal refinery, a governmental body debating legislation, or a personal homeowner weighing a mountain or beach home, it is important to understand what lies ahead.

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Pictures of the(************************************* )/2013 summer season on the frozen continent

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Researchers studying Antarctic’s Ross Ice Rack discovered that the ice gives off an unusual noise as the ice starts to melt. The group of researchers discovered this finding, never ever having actually heard the odd sound the upper layers of ice develop.

The group of researchers, who just recently released their research study in Geophysical Research Study Letters, discovered that both wind and melting trigger the surface area pieces of ice on the Ross Ice Rack to vibrate, producing odd noises as an outcome.

Very delicate seismic sensing units were utilized to keep an eye on the noise patterns throughout the Ross Ice Rack in western Antartica. The preliminary intent of the research study was not to determine this acoustic abnormality however to study the crust and mantle underneath Antarctica.

After 2 years of listening to the surface area layers of the Ross Ice Rack, researchers discovered that the ice almost continually “sings” in various frequencies depending upon wind and melting. The singing is produced from high-frequency wave caught in the upper couple meters of snow. As winds blow throughout the ice rack, they vibrate these upper layers, called firn. The seismic sensing units, buried within the firn layers, can determine and tape-record these waves and their “noise” through time.

Frost and firn after a snowstorm.

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All of a sudden, the scientists discovered that the pitch of the noise from the ice rack altered when temperature levels increased to above freezing and the ice started to melt. The acoustic waves started to decrease and the pitch dropped as an action. This was a sign of both melting and degree of melting. As soon as temperature levels dipped listed below freezing once again, the upper firn refroze however did not restore the preliminary pitch it had prior to the firn melted. This might be a sign that when melted, the upper layers of ice racks do not merely return back to initial type.

Researchers are eager to determine and comprehend the qualities of melting in Antarctica and the upper firn layers as they represent a crucial variable in water level increase over the coming years. It is approximated that if the Antarctic Ice Sheets melted in totality water level would increase by 60 meters(197 feet).

Ice Highway on Ross Ice Rack, Ross Island, Antarctica

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In the worst case circumstance where all land ice has actually melted and drained pipes into the oceans, researchers approximate that water level will increase by 216 feet. It is very important to keep in mind that even on fast timescales this procedure would take countless years. If it did occur, nevertheless, our world would look rather various, with many seaside cities sitting directly in the ocean.

Through continuous seismic tracking of ice racks in Antarctica, we can comprehend and predict into the future what we anticipate for water level increase. Whether you’re an international oil and gas giant thinking about where to develop your next seaside refinery, a governmental body disputing legislation, or an individual house owner weighing a mountain or beach house, it is essential to comprehend what lies ahead.

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2242137301″ >

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Pictures of the 2012/ 2013 summer season on the frozen continent

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.

Researchers studying Antarctic’s Ross Ice Rack discovered that the ice gives off an unusual noise as the ice starts to melt. The group of researchers discovered this finding, never ever having actually heard the odd sound the upper layers of ice develop.

The group of researchers, who just recently released their research study in Geophysical Research Study Letters , discovered that both wind and melting trigger the surface area pieces of ice on the Ross Ice Rack to vibrate, producing odd noises as an outcome.

Very delicate seismic sensing units were utilized to keep an eye on the noise patterns throughout the Ross Ice Rack in western Antartica. The preliminary intent of the research study was not to determine this acoustic abnormality however to study the crust and mantle underneath Antarctica.

After 2 years of listening to the surface area layers of the Ross Ice Rack, researchers discovered that the ice almost continually “sings” in various frequencies depending upon wind and melting. The singing is produced from high-frequency wave caught in the upper couple meters of snow. As winds blow throughout the ice rack, they vibrate these upper layers, called firn. The seismic sensing units, buried within the firn layers, can determine and tape-record these waves and their “noise” through time.

.

.

Frost and firn after a snowstorm.

.

.

All of a sudden, the scientists discovered that the pitch of the noise from the ice rack altered when temperature levels increased to above freezing and the ice started to melt. The acoustic waves started to decrease and the pitch dropped as an action. This was a sign of both melting and degree of melting. As soon as temperature levels dipped listed below freezing once again, the upper firn refroze however did not restore the preliminary pitch it had prior to the firn melted. This might be a sign that when melted, the upper layers of ice racks do not merely return back to initial type.

Researchers are eager to determine and comprehend the qualities of melting in Antarctica and the upper firn layers as they represent a crucial variable in water level increase over the coming years. It is approximated that if the Antarctic Ice Sheets melted in totality water level would increase by 60 meters (197 feet).

.

.

Ice Highway on Ross Ice Rack, Ross Island, Antarctica

.

.

In the worst case circumstance where all land ice has actually melted and drained pipes into the oceans, researchers approximate that water level will increase by 216 feet. It is very important to keep in mind that even on fast timescales this procedure would take countless years. If it did occur, nevertheless, our world would look rather various, with many seaside cities sitting directly in the ocean.

Through continuous seismic tracking of ice racks in Antarctica, we can comprehend and predict into the future what we anticipate for water level increase. Whether you’re an international oil and gas giant thinking about where to develop your next seaside refinery, a governmental body disputing legislation, or an individual house owner weighing a mountain or beach house, it is essential to comprehend what lies ahead.

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