The profound, climate-driven transformation of the Arctic can radically alter carbon dioxide balance in downstream oceanic regions. It is crucial to understand how changing deliveries of meltwater, nutrients and organic matter in the western North Atlantic impact carbon fluxes regionally and globally.
There is evidence that the ocean’s ability to filter carbon from the atmosphere is changing. As a result, global climate goals are likely well off the mark. With support from the Canada First Research Excellence Fund, Dalhousie and its academic and industry partners will find solutions and make Canada a global leader in the science to avert climate change.
Laval oceanographer, Dr. Jean-Éric Tremblay, seeks to understand how the nutrient and freshwater content of waters that flow out of the Arctic are changing and affecting biological carbon fluxes at a variety of scales in the ocean.
“Nutrients are the fundamental building blocks of all life,” says Dr. Tremblay. “The cycling and availability of nutrients largely set the biomass that marine algae and animals can reach and, consequently, their impact on marine carbon fluxes.”
The ocean is highly interconnected. Currents dictate how nutrients are redistributed horizontally between ocean areas. Freshwater content of the upper ocean affects how nutrients move vertically through the stratified layers of the ocean, between the deep reservoir and the surface, where algae can use them. The ocean’s nitrogen cycle also includes microbial processes that lead to net losses or gains of nutrients over time, modulating the ocean’s ability to capture carbon dioxide.
With his students and postdoctoral fellows, Dr. Tremblay investigates nutrient dynamics in the ocean and their changes by analyzing time-series of ship-based measurements gathered at key locations along the path of major currents in the western Arctic, the northwest Atlantic and the St. Lawrence system.
Using sensors and assays, measurements are collected for physical water properties, nutrient concentrations, nitrogen cycling processes, and the characterization of particulate organic matter.
A major concern is that key ocean areas like the deep-water formation node in the Labrador Sea and the fishing grounds that span the eastern North American shelf lay in the path of the massive water outflow descending from the high Arctic.
Much like waterfalls on land, cascades of Arctic water converge into the eastern North Atlantic carrying the telltale signs of a polar ocean transformed by amplified warming and freshwater loading from melting multi-year sea ice and glaciers.
Resulting changes in stratification, circulation pathways, pH, nutrient load and biological productivity are bound to have major repercussions on marine carbon fluxes, regionally at first and globally as meltwater and nutrients propagate through the ocean.
Dalhousie University and its research partners L’Université du Québec à Rimouski, Université Laval and Memorial University are seeking support from the Canada First Research Excellence Fund to ensure the ocean’s ability to absorb carbon from the atmosphere is accounted for in global climate goals. Together, the universities are the world’s most productive ocean research team, capable of bringing the most sophisticated science to the Earth’s most pressing challenge.Learn more