Приклади вживання Ice loss Англійська мовою та їх переклад на Українською
{-}
-
Colloquial
-
Ecclesiastic
-
Computer
Winter rain in Greenland is driving rapid ice loss.
If the ice loss will slow down, then rise to 18 centimeters.
The rest of Greenland is seeing massive ice loss as well.
Ice loss in West Antarctica has increased substantially in the last few decades, and is continuing.
There are other environmental and economic implications to ice loss as well.
Up until 2012, Antarctic ice loss was contributing just 0.2 mm per year to sea level, and did not appear to be increasing.
The rest of Greenland is seeing massive ice loss as well.
Since 1979 Antarctica's ice loss has grown six times faster, and Greenland's four times since the turn of the century.
But until now it was unclear how thesenaturally-occurring wind variations could cause the ice loss.
Prior to 2012, Antarctic ice loss resulted in a 0.2 mm sea level increase each year, with no notable increase from that over time.
It means that if/when humans reduce our aerosol pollution,the warming in the Arctic and the ice loss there will be worse.
At this stage the role of thenew heat source is unclear, but ice loss already triggered by rising temperatures could be exposing the glacier to more of the volcanic activity.
As the grounding line retreats further into thicker parts of the ice sheet, the flow speeds up,further increasing ice loss.
The signs and impacts of climate change- such as sea level rise, ice loss and extreme weather- increased during 2015-2019.
From nearly 12 square kilometers in 1912, the ice-covered area has shrunk to just 1.76 square kilometers by 2011-that's more than 80 percent ice loss.
That suggests that if we want to stabilize today's accelerating ice loss, we need to see a little cooling of our own.'.
Total ice loss during the 25-year period contributed to sea level rise of about 0.3 inches(around 8 millimeters), approximately 40 percent of which- about 0.1 inches(3 mm)- happened in the past five years.
These findings imply that preventing substantial Antarctic ice loss relies on limiting global emissions to- or below- RCP2.6.
Reports published recently revealed that Antarctica has lost around 3 trillion tons ofice in just the past 25 years, and this ice loss has accelerated rapidly over the last five years.
It's important to monitor and understand ice loss in major mountain systems, but subnival ecosystems cover a much larger area than permanent snow and ice, and we know very little about them and how they moderate water supply.”.
Antarctica has lost 3 trilliontons of ice in the past 25 years, and that ice loss has accelerated rapidly over the last five years.
Our results indicate that glaciers across the Himalayas experienced significant ice loss over the past 40 years, with the average rate of ice loss twice as rapid in the 21st century compared to the end of the 20th century,” the study's authors said.
Thermal expansion of the oceans by global warming and the melting of glaciers, which so far have been the most important factors in sea level rise,will add to the contribution from Antarctic ice loss, making the overall sea level rise risk even bigger.
It suggests that better accounting for some of the physical processes affecting ice loss in Antarctica could double the sea-level rise expected under severe climate change scenarios.
Sea levels may threaten coastal cities sooner than expected,scientists say, as ice loss speeds up and Antarctic temperatures rise.
Our results indicate that glaciers across the Himalayas experienced significant ice loss over the past 40 years, with the average rate of ice loss twice as rapid in the 21st century compared to the end of the 20th century”, say the researchers about their findings.
We have known for some timethat varying winds near the West Antarctic Ice Sheet have contributed to the ice loss, but it has not been clear why the ice sheet is changing now.
At the end of the last ice age around 11,000 years ago, the ice sheet went through a period of rapid,sustained ice loss when changes in global weather patterns and rising sea levels pushed warm water closer to the ice sheet- just as is happening today.
Glaciers in temperate regions such as in the European Alps andthe Caucasus mountain range did not escape ice loss either, but are too small to make a significant contribution to sea level.