New research reveals that glaciers are melting at a quicker pace in the ocean than previously projected. Over the initial two decades of the current century, the ice has significantly thinned, with an average annual melt rate escalating from 10 feet per year in the 1990s to 30 feet per year in the 2020s.

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A study funded by NASA found that about half of the Himalayas glaciers have melted because global temperatures have risen beyond 1.5 degrees Celsius.

Alarming Rate of Glacier Melting 

Intrigued by the accelerated melting of northwest Greenland's Petermann Glacier over the past fifteen years, scientists delve into the underlying causes driving this phenomenon. 

Their focus zeroes in on the infiltration of warm ocean waters beneath the glacier, prompting them to embark on a comprehensive observation and modeling study. 

Spearheaded by NASA's Jet Propulsion Laboratory in collaboration with researchers from the University of California, Irvine, Interesting Engineering reported that this endeavor aims to unravel the potential implications of ice melt. 

The computer analysis conducted during the study reveals that the projected sea level rise could surpass previous estimates, signifying a graver scenario than anticipated. 

Such a rise in sea levels could pose significant threats worldwide, including heightened risks of flooding, particularly imperiling coastal communities and their livelihoods.

Analyzing Tidal Movements

Researchers utilized radar interferometry data from multiple European satellite missions to analyze the tidal movements of Petermann Glacier.

Apart from satellite data, Massachusetts Institute of Technology (MIT) developed a comprehensive computational model to evaluate the effects of climate change in intricate environments comprising ice, seawater, and land.

The model tracks the interplay among these components, encompassing tidal effects and temperature fluctuations induced by climate change.

In their analysis of climate-induced changes in ice melting intensity, scientists observed significant shifts in glaciers, spanning several kilometers, in response to tidal variations.

Lead author Ratnakar Gadi, a Ph.D. candidate in Earth system science at UCI, explained that by incorporating this glacier migration into the MIT numerical ocean model, they estimated a thinning of approximately 460 feet of ice between 2000 and 2020. 

Over this period, the average melt rate surged from around 10 feet per year in the 1990s to 30 feet per year in the 2020s.

Also Read: Greenland's Lesser-Known Glaciers Surge in Melting Rates, Revealing Alarming Impact on Sea Levels

Senior co-author Eric Rignot, a professor of Earth system science at UCI, noted that traditionally, the transition boundary between ice and ocean was perceived as sharp, but their study revealed it to be diffuse, extending over a wide zone known as the 'grounding zone,' which spans several kilometers.

He explained that in this zone, seawater rises and falls with tidal fluctuations, resulting in vigorous melting of grounded ice from beneath.

Furthermore, Gadi highlighted that the model depicted exceedingly high melt rates near the entrance of the grounding zone cavity, surpassing rates observed elsewhere in the ice shelf cavity.

He clarified that the heightened temperatures of the water and increased intrusion of seawater beneath the ice are the primary factors driving the thinning of ice along the central flowline of the Petermann Glacier.

Interestingly, the grounding zone plays a pivotal role in the escalated ice melting process. Through analysis using the numerical model, scientists observed a thinning of approximately 12 feet solely attributable to warmer ocean temperatures.

Related Article: NASA Study Reveals Himalayas Glaciers Rapidly Melting Amid Worsening Climate Crisis