New study: Thick sea-ice warms Greenland fjords

New study: Thick sea-ice warms Greenland fjords
Helicopter view over the Ryder Glacier ice tongue. Credit: Martin Jakobsson

A new study led by Stockholm University Assistant Professor Christian Stranne shows that thick sea ice outside the fjords can actually increase the sensitivity of Greenlandic fjords to warming. Stranne and a team of researchers from Sweden, Greenland, the Netherlands, the U.S. and Canada have reported on expeditions to two distinct fjords in northern Greenland during the 2015 and 2019 summers.

"These fjords were practically inaccessible to researchers until quite recently because the sea ice was too thick—they are some of the least-studied areas on the planet, and require a large icebreaker to reach them, even in the summer," says Stranne. The inaccessibility and sea ice build-up is due to the direction of Arctic Ocean currents; the Beaufort Gyre and Transpolar Drift push ice from across the Arctic up against the northern Greenland coast.

Writing in Communications Earth & Environment, the research team reported on measurements made during the Petermann 2015 and Ryder 2019 expeditions, when the Swedish icebreaker Oden made detailed studies of Petermann Fjord and Sherard Osborn Fjord in northern Greenland. Even in summer, the entrance to Sherard Osborn Fjord on the northern coast of Greenland is blocked by thick sea ice, but the more southerly located Petermann Fjord has for several years opened to the Nares Strait, connecting the Arctic Ocean with Baffin Bay. Both fjords host large glaciers with floating ice tongues extending from Greenland glaciers many kilometers into the fjords. Unsurprisingly, tend to melt these floating portions of the glaciers and icebergs in the fjord faster than cooler . But how does the presence or absence of the thick sea ice barrier outside a fjord affect water temperatures inside?

In 2019, air temperatures in northern Greenland reached record highs. Despite similar high air temperatures and conditions, Petermann Fjord's near surface sea temperatures never exceeded 0 degrees C. "But in the Sherard Osborn Fjord, cut off from the by thick sea ice, near surface sea temperatures reached 4 degrees C—which was 3 degrees C higher than any previous seawater measurement north of Greenland," explains Stranne.

New study: Thick sea-ice warms Greenland fjords
A satellite image over the study area north of Greenland with inset showing the Arctic Ocean sea-ice thickness during the expedition, derived from satellite data. Colored dots indicate discrete and continuous near-surface temperature data collected during the Ryder 2019 expedition with icebreaker Oden. Arrows show large-scale sea-ice drift patterns with Beaufort Gyre (BG) and transpolar drift (TPD). Credit: Modified from Stranne et al., Communications Earth & Environment (2021), DOI:10.1038/s43247-021-00140-8

Summertime melt produces a warm freshwater layer floating atop saltier water in the fjord; here the sea ice barrier trapped this meltwater inside the fjord. Because of the difference in salt content, the surface water became isolated also from the water below, allowing time for intense solar heating of the fresher surface water. Such warmer water temperatures can contribute to faster melting of the Ryder Glacier in Sherard Osborn Fjord, as well as changing the biogeochemistry in the fjord waters. Conversely, the researchers suggest, that neighboring Petermann Fjord, which was open to the sea during 2015 and 2019, experienced colder surface water temperatures because its surface water was not isolated within the fjord by a sea ice barrier.

These observations are counterintuitive: thick sea ice is associated with , yet it can lead to warmer surface water temperatures inside the fjords. For this reason, fjords along the northern Greenland coast are more sensitive to climate warming than fjords without a sea ice barrier.

But each fjord is a little different. Last year, another study from the 2015 and 2019 expeditions pointed out that Ryder Glacier in Sherard Osborn Fjord is less affected by melting of the ice tongue from underneath, compared to Petermann Glacier in Petermann Fjord. In this case, the explanation is not sea ice but the shape of the seafloor that produces a shallower opening to the sea. The physical block of rock and sediment dampens intrusions of deeper warm water from outside the fjord (of Atlantic origin) which tends to make Ryder Glacier less sensitive to climate warming—while at the same time, sea ice in the adjacent Lincoln Sea can make it more sensitive. "It's a complex interaction. Overall, we know that warming climate will lead to faster moving and less ice on Greenland. But how fast this happens, and to what extent, remains a key research topic," says Stranne.

Explore further

Scientists report ocean data from under Greenland's Petermann Glacier

More information: The climate sensitivity of northern Greenland fjords is amplified through sea-ice damming, Communications Earth & Environment, 2021, DOI: 10.1038/s43247-021-00140-8
Citation: New study: Thick sea-ice warms Greenland fjords (2021, April 12) retrieved 4 October 2022 from
This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no part may be reproduced without the written permission. The content is provided for information purposes only.

Feedback to editors