JPL
Careers
Education
Science & Technology
JPL Logo
JPL Logo
Earth
.

OMG, the Water's Warm! NASA Study Solves Glacier Puzzle

Jun 21, 2018
Tracy and Heilprin glaciers in northwest Greenland. The two glaciers flow into a fjord that appears black in this image.
Credit: NASA
This figure shows estimated ice flow velocities of Tracy and Heilprin glaciers (right) and the depths of the fjord in front of the glaciers. The approximate location of the sill in front of Tracy is shown as a dashed yellow line. Research ship cruise tracks are shown in orange.
Credit: NASA/JPL-Caltech

A plume of warm water is the reason one of two adjoining glaciers in Greenland is melting almost four times as fast as the other.

A new NASA study explains why the Tracy and Heilprin glaciers, which flow side by side into Inglefield Gulf in northwest Greenland, are melting at radically different rates.

Using ocean data from NASA's Oceans Melting Greenland (OMG) campaign, the study documents a plume of warm water flowing up Tracy's underwater face, and a much colder plume in front of Heilprin. Scientists have assumed plumes like these exist for glaciers all around Greenland, but this is the first time their effects have been measured.

The finding highlights the critical role of oceans in glacial ice loss and their importance for understanding future sea level rise. A paper on the research was published June 21 in the journal Oceanography.

Tracy and Heilprin were first observed by explorers in 1892 and have been measured sporadically ever since. Even though the adjoining glaciers experience the same weather and ocean conditions, Heilprin has retreated upstream less than 2.5 miles (4 kilometers) in 125 years, while Tracy has retreated more than 9.5 miles (15 kilometers). That means Tracy is losing ice almost four times faster than its next-door neighbor.

This is the kind of puzzle OMG was designed to explain. The five-year campaign is quantifying ice loss from all glaciers that drain the Greenland Ice Sheet with an airborne survey of ocean and ice conditions around the entire coastline, collecting data through 2020. OMG is making additional boat-based measurements in areas where the seafloor topography and depths are inadequately known.

About a decade ago, NASA's Operation IceBridge used ice-penetrating radar to document a major difference between the glaciers: Tracy is seated on bedrock at a depth of about 2,000 feet (610 meters) below the ocean surface, while Heilprin extends only 1,100 feet (350 meters) beneath the waves.

Scientists would expect this difference to affect the melt rates, because the top ocean layer around Greenland is colder than the deep water, which has traveled north from the midlatitudes in ocean currents. The warm water layer starts about 660 feet (200 meters) down from the surface, and the deeper the water, the warmer it is. Naturally, a deeper glacier would be exposed to more of this warm water than a shallower glacier would.

When OMG Principal Investigator Josh Willis of NASA's Jet Propulsion Laboratory in Pasadena, California, looked for more data to quantify the difference between Tracy and Heilprin, "I couldn't find any previous observations of ocean temperature and salinity in the fjord at all," he said. There was also no map of the seafloor in the gulf.

OMG sent a research boat into the Inglefield Gulf in the summer of 2016 to fill in the data gap. The boat's soundings of ocean temperature and salinity showed a river of meltwater draining out from under Tracy. Because freshwater is more buoyant than the surrounding seawater, as soon as the water escapes from under the glacier, it swirls upward along the glacier's icy face. The turbulent flow pulls in surrounding subsurface water, which is warm for a polar ocean at about 33 degrees Fahrenheit (0.5 degree Celsius). As it gains volume, the plume spreads like smoke rising from a smokestack.

"Most of the melting happens as the water rises up Tracy's face," Willis said. "It eats away at a huge chunk of the glacier."

Heilprin also has a plume, but its shallower depth limits the plume's damage in two ways: the plume has a shorter distance to rise and gathers less seawater; and the shallow seawater it pulls in has a temperature of only about 31 degrees Fahrenheit (minus 0.5 degree Celsius). As a result, even though Heilprin is a bigger glacier and more water drains from underneath it than from Tracy, its plume is smaller and colder.

The study produced another surprise by first mapping a ridge, called a sill, only about 820 feet (250 meters) below the ocean surface in front of Tracy, and then proving that this sill did not keep warm water from the ocean depths away from the glacier. "In fact, quite a lot of warm water comes in from offshore, mixes with the shallower layers and comes over the sill," Willis said. Tracy's destructive plume is evidence of that.

News Media Contact

Written by Carol Rasmussen

Alan Buis

818-354-0474

alan.buis@jpl.nasa.gov

2018-144

Related News

Climate Change .

Warming Seas Are Accelerating Greenland’s Glacier Retreat

Earth .

NASA, US and European Partner Satellite Returns First Sea Level Measurements

Technology .

NASA Confirms New SIMPLEx Mission Small Satellite to Blaze Trails Studying Lunar Surface

Earth .

New Data Confirm 2020 SO to Be the Upper Centaur Rocket Booster From the 1960's

Earth .

Follow Sentinel-6 Michael Freilich in Real Time As It Orbits Earth

Climate Change .

US-European Mission Launches to Monitor the World's Oceans

Climate Change .

Sentinel-6 Michael Freilich Satellite Prepared for Launch

Climate Change .

Study: Urban Greenery Plays a Surprising Role in Greenhouse Gas Emissions

Climate Change .

NASA TV to Air Sentinel-6 Michael Freilich Launch, Prelaunch Activities

Earth .

Earth May Have Captured a 1960s-Era Rocket Booster

Explore More

Image .

Glacier Undercutting in Action

Image .

Hulhumale, Maldives

Topic .

Earth

Image .

Kilauea Volcano, Hawaii

Infographic .

Inside Hurrricanes

Image .

Mt. Etna, Italy

Image .

Sentinel-6 Michael Freilich First Light Waveform

Image .

Sentinel-6 Michael Freilich First Light Sea Level

Image .

Providencia Island, Colombia

Image .

Kliuchevskoi Volcano, Kamchatka, Russia

About JPL
Who We Are
Executive Council
Directors of JPL
JPL History
Documentary Series
Virtual Tour
Annual Reports
Missions
All
Current
Past
Future
News
All
Earth
Mars
Solar System
Universe
Technology
Galleries
Images
Videos
Audio
Podcasts
Infographics
Engage
JPL and the Community
Lecture Series
Public Tours
Events
Team Competitions
JPL Speakers Bureau
Topics
Solar System
Mars
Earth
Climate Change
Stars and Galaxies
Exoplanets
Technology
JPL Life
For Media
Contacts and Information
Press Kits
More
Asteroid Watch
Robotics at JPL
Subscribe to Newsletter
Social Media
Get the Latest from JPL
Follow Us

JPL is a federally funded research and development center managed for NASA by Caltech.

More from JPL
Careers Education Science & Technology Acquisitions JPL Store
Careers
Education
Science & Technology
Acquisitions
JPL Store
Related NASA Sites
Basics of Spaceflight
Climate Kids
Earth / Global Climate Change
Exoplanet Exploration
Mars Exploration
Solar System Exploration
Space Place
NASA's Eyes Visualization Project
Voyager Interstellar Mission
NASA
Caltech
Privacy
Image Policy
FAQ
Feedback
Site Manager: Veronica McGregor
Site Editors: Tony Greicius, Randal Jackson, Naomi Hartono