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Shrubs lend an insight into a glacier's past

Scientists have discovered a method using shrubs to create historical climate data on glaciers, providing more accurate predictions of future changes. The method allows researchers to extend the current record of glacier melting back by many decades, giving them a better understanding of how glaciers behave in the summer.

SourceIOP Publishing·JournalEnvironmental Research Letters·DateNov 26, 2012

Melting glaciers raise sea level

A University of Innsbruck team assessed glacier contribution to sea level rise from 1902 to 2009, finding that melting glaciers caused about 11 cm of sea level increase. Glaciers' melt rates were surprisingly constant over time, with brief warm episodes leading to Arctic glacier retreat.

SourceUniversity of Innsbruck·JournalThe Cryosphere·DateNov 14, 2012

Warming ocean could start big shift of Antarctic ice

A new study reveals how warming waters in the Southern Ocean can connect with the movement of massive ice-sheets deep in the Antarctic interior. The research found that ocean warming can trigger increased flow of ice through narrow glaciers, causing inland sectors of the ice-sheet to become thinner and flow faster.

SourceUniversity of New South Wales·JournalProceedings of the National Academy of Sciences·DateSep 19, 2012

Alpine glaciers contribute to carbon cycling

Researchers have discovered that Alpine glaciers contain diverse biogeochemical complexes of dissolved organic matter, which is surprisingly bioavailable. This finding highlights the importance of glaciers as 'freezers' that preserve organic matter for microbial heterotrophs.

SourceUniversity of Vienna·JournalNature Geoscience·DateSep 17, 2012

How fast can ice sheets respond to climate change?

Scientists found that glaciers on Baffin Island expanded quickly during a short-lived cold snap about 8,200 years ago, providing insight into ice sheets' response to past climate change. This discovery suggests that ice sheets may react rapidly to temperature shifts, raising concerns for future climate change.

SourceUniversity at Buffalo·JournalScience·DateSep 13, 2012

Ancient story of Dartmoor tors has an ice-cold twist

A new study reveals that an ice cap and valley glaciers were present in the centre of Dartmoor during the last Ice Age, sculpting its rocky landscape. The research found distinctive outer tors survived while inner tors were destroyed or prevented from forming due to the glacier's presence.

SourceDurham University·JournalQuaternary Science Reviews·DateJun 12, 2012

Greenland's current loss of ice mass

Research reveals Greenland's ice sheet is losing mass at an unprecedented rate, with melting and calving processes increasing by 0.07mm/year annually since 2005. The study provides insights into the impact of regional weather patterns on ice sheet dynamics.

SourceHelmholtz Association·JournalEarth and Planetary Science Letters·DateMay 29, 2012

Glacial carbon may hold record of environmental change

A study published in Nature Geoscience reveals that glaciers provide a significant source of modern organic carbon to downstream ecosystems, indicating the widespread influence of human activities on pristine environments. The findings suggest that glacier ecosystems are highly sensitive to climate warming and industrial pollution.

SourceYale University·JournalNature Geoscience·DateFeb 20, 2012

Land-cover changes do not impact glacier loss

A recent study by University of Innsbruck climate researchers found that land-cover changes have a limited effect on glacier loss in the Kilimanjaro area. The team's novel methodology showed that LCC mainly alter precipitation over glaciers, resulting in local increases or decreases in glacier mass.

SourceUniversity of Innsbruck·JournalNature Climate Change·DateFeb 5, 2012

Hardy bacteria help make case for life in the extreme

Researchers have discovered two types of bacteria that can survive at extremely cold temperatures, including the bottom of Arctic and Antarctic glaciers. The bacteria, Chryseobacterium and Paenisporosarcina, respire in ice at temperatures ranging from -27 to 24 degrees Fahrenheit, using acetate as an energy source.

SourcePenn State·JournalEnvironmental Microbiology Reports·DateJan 19, 2012