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Notes from the Field

CASCADES: A Journey Along Greenland’s Coast Where Ocean Meets Ice 

By Simon Bélanger, Université du Québec à Rimouski (UQAR), Québec, Canada 

What an extraordinary feeling it is to witness the beauty of these icy landscapes, where the ice sheet flows down to the sea through fjords with steep, towering walls—watching, in real time, as the ice sculpts this raw, mineral landscape… Breathtaking!

An instrument with radiometers is shown mounted on the bow of a research ship in one corner of a glorious view of an oceanic channel so still that the sky is reflected in a mirror image. Through a layer of cloud, the sun has rainbow edges.  
The pySAS solar tracking instrument is deployed in the Kennedy Channel between Greenland and Ellesmere Island.  
Simon Bélanger 

A red-hulled research ship with a white superstructure boasting the Canadian maple leaf sits on a glassy, bergy-bit-strewn sea with bare hills on the horizon.
The Canadian Coast Guard Ship (CCGS) Amundsen, an icebreaker, sails near the community of Kullorsuaq, Greenland.  
Amundsen Science/Véronique Rochefort 

A low, nearly flat ice berg floats not far from the research ship’s red rail.  
Petermann Ice Island drifts in the Robeson Channel. 
Simon Bélanger 

Into the Unknown  

We all know that Greenland’s glaciers are melting fast in response to global warming. But how that meltwater changes the surrounding ocean is still largely unknown, since field observations here are scarce and sailing among sea ice and icebergs is challenging and costly. From August 6 to September 3, 2026, I had the rare opportunity to join the CASCADES (a ‘thematic’ name, not an acronym) expedition, sailing more than 3,000 nautical miles (5,500 kilometers) to reach the Robeson Channel. This body of water runs between Ellesmere Island and Greenland at 82°N, where cold water and sea ice flow south out of the Arctic Ocean. Along the way, we collected oceanographic measurements in fjords and near settlements with names as striking as the landscapes themselves—Ilulissat (Jakobshavn), Uummannaq, Kullorsuaq, Petermann, and Qaanaaq (Thule)—places where ocean, ice, and meltwater interact. 

A scientist in outdoor garb poses in front of open water that leads to the white ice cliffs of a glacier front.  
Simon Bélanger poses in front of the Jakobshavn Glacier.  
Jonathan Gagnon

Two people in outdoor clothing explore a rocky shore. In the background : sea ice, open water, and the white ice cliffs of a glacier front.  
Meltwater is sampled in front of the Upernavik Glacier by the chief scientist, Jean-Éric Tremblay, and Lucie Mallard.
Amundsen Science/Véronique Rochefort

Path to the Sea 

As an ocean-color remote-sensing specialist, my job on board was to measure how sunlight interacts with the water and its constituents—the same frequency of light (wavelength) NASA’s PACE (Plankton, Aerosol, Cloud, ocean Ecosystem) satellite measures from space—and to collect water samples to identify the tiny drifting algae, or phytoplankton, and non-living suspended matter that give the ocean its colorful aspect. These measurements will help validate what PACE measures from orbit. But CASCADES is much bigger than my own work: it is an international (Canada, Switzerland, France, and Greenland), multidisciplinary expedition bringing together glaciologists measuring ice thickness, marine-mammal observers, microbiologists, geologists, and biogeochemists. Together, we are trying to understand how carbon and nutrients move from the ocean’s surface to the deep sea, and how glacier meltwater changes that journey. 

The map of the research trip’s route is keyed to four photographs taken during the journey.  
This map shows the sampling voyage, using PACE imagery and photographs.  
NASA PACE-OCI/Carina Poulin

Ops and Opportunity  

No two days aboard the CCGS Amundsen were alike. Our operations ranged from water sampling with a CTD rosette (an instrument that measures temperature, salinity, and depth), to catching zooplankton and fish with nets, to pulling up surface sediments and six-meter-long sediment cores that let us reconstruct the history of these fjords. And, of course, I had my own work: measuring how light travels through the water column at different wavelengths across the visible spectrum and taking water color spectra at the surface. These water color spectra tell us about the abundance of biological activity and possibly about the composition of the phytoplankton communities that form the base of the marine ecosystems.  

The ship’s yellow crane extends over a turquoise sea; its cable descends into the sea. The gray, tan, and white striations of the glacier front’s ice tower in the background.  
Water sampling with the CTD rosette takes place at a land-terminating glacier (Ukkusissat) near Uummannaq Fjord.  
Jonathan Gagnon 

A glowing cloudy sky casts a pearly light over a bay dotted with icebergs. In the foreground, small boxy houses perch on a grassy hillside speckled with patches of snow.  
The CCGS Amundsen icebreaker sits just offshore in Kullorsuaq, Greenland.
Simon Bélanger 

An instrument with radiometers is mounted on a gray metal « tower » aboard the ship. It overlooks a placid deep blue sea edged with icebergs and purple hills.  
Near the community of Kullorsuaq, Greenland, a hyperspectral instrument (pySAS) measures water color to validate PACE observations.  
Université du Québec à Rimouski/Simon Bélanger 

Glowing with neon green light, a woman works with a water filtration system in a lab inside the ship.  
Juliette Provencher filters seawater under green light in the filtration lab. 
Jonathan Gagnon 

International Exploration  

The CASCADES expedition is led by Jean-Éric Tremblay of Université Laval, with funding from Amundsen Science, l’Institut Nordique du Québec (INQ), the Swiss Polar Institute (SPI), and the Transforming Climate Action (TCA) initiative. My remote sensing work is supported by the Canadian Space Agency (CSA).  

Globs of pinkish ice form amid shards of aquamarine and royal blue.  
Frazil ice forming at the sea surface is observed with polarized light filtering. 
Jonathan Gagnon

A brown rocky cliff emerges from a dark blue sea. It is capped and nearly overwhelmed by a low-hanging cloud.  
Petermann Fjord is located at 81.5°N. 
Jonathan Gagnon