About My Health Careers Internship MedBlogs Contact us

Low-Level Clouds Responsible for the Ice-Melt in 2012

by Enozia Vakil on April 6, 2013 at 4:20 PM
Font : A-A+

 Low-Level Clouds Responsible for the Ice-Melt in 2012

Low, thin clouds may be the culprit to the record-shattering level of ice-melting in Greenland in 2012, study reveals.

If the ice sheet covering Greenland were to melt in its entirety, sea levels would rise by 24 feet globally.


Three million cubic kilometers of ice won't wash into the ocean overnight, but researchers have been tracking increasing melt rates since at least 1979.

Last summer, however, the melt was so large that similar events show up in ice core records only once every 150 years or so over the last four millennia.

"In July 2012, a historically rare period of extended surface melting raised questions about the frequency and extent of such events," Ralf Bennartz, professor of atmospheric and oceanic sciences and scientist at the University of Wisconsin-Madison's Space Science and Engineering Center, said.

"Of course, there is more than one cause for such widespread change. We focused our study on certain kinds of low-level clouds," he said.

In a study, Bennartz and collaborators describe the moving parts that led to the melt, which was observed from the ICECAPS experiment funded by the National Science Foundation and run by UW-Madison and several partners atop the Greenland ice sheet.

"The July 2012 event was triggered by an influx of unusually warm air, but that was only one factor," Dave Turner, physical scientist at the National Oceanic and Atmospheric Administration's National Severe Storms Laboratory, said.

"In our paper we show that low-level clouds were instrumental in pushing temperatures up above freezing," he said.

Low-level clouds typically reflect solar energy back into space, and snow cover also tends to bounce energy from the sun back from the Earth's surface.

Under particular temperature conditions, however, clouds can be both thin enough to allow solar energy to pass through to the surface and thick enough to "trap" some of that heat even if it is turned back by snow and ice on the ground.

While low, thin cloud cover is just one element within a complex interaction of wind speed, turbulence and humidity, the extra heat energy trapped close to the surface can push temperatures above freezing.

That is exactly what happened in July 2012 over large parts of the Greenland ice sheet, and similar conditions may help answer climate conundrums elsewhere.

"We know that these thin, low-level clouds occur frequently," Bennartz said.

"Our results may help to explain some of the difficulties that current global climate models have in simulating the Arctic surface energy budget," he added.

The study is set to be published in the journal Nature.


News A-Z
News Category
What's New on Medindia
Turmeric: Magic Ingredient to Keep you Healthy in Winter
Top 7 Benefits of Good Oral Hygiene
Healthy and Safer Thanksgiving 2021
View all

Medindia Newsletters Subscribe to our Free Newsletters!
Terms & Conditions and Privacy Policy.

Recommended Reading
30-Year Record Broken by Greenland's Ice Sheet Melting
Research has revealed that melting over the Greenland ice sheet broke the seasonal record on August ...
Greenland's Contribution to Sea-level Rise
Glaciers which behave independently from the ice sheet is being looked by scientists, despite ......
Ice Cores in Greenland Provide Clues to a Warmer World in the Past
Researchers analyzing ice cores drilled in Greenland have found that the ancient world was warmer .....
Ice Melt in Greenland is Accelerating With Time
Since 2003, Greenland has had an average net loss of 200 million tons of ice every year, scientists ...

Disclaimer - All information and content on this site are for information and educational purposes only. The information should not be used for either diagnosis or treatment or both for any health related problem or disease. Always seek the advice of a qualified physician for medical diagnosis and treatment. Full Disclaimer

© All Rights Reserved 1997 - 2021

This site uses cookies to deliver our services. By using our site, you acknowledge that you have read and understand our Cookie Policy, Privacy Policy, and our Terms of Use