Greenland is the world’s largest “non-continental” island, and about 80per centof this island is covered by the Greenland Ice Sheet. In recent years, however, the melting of this ice sheet hasaccelerated, leading to an increased contribution torisingsea levels.

A portion ofthisincreasedmelting can be attributed to the presence of dark algae on the ice sheet surface. Contrary to white, reflective ice, the darkpigmentationofthesealgae absorbssunlight and warmsthe surroundingice, causing melting.Climate change is causing Arctic summers to become warmer and longer than in the past. These longer summers allow for increased ice algal growth, and the resulting algal blooms are causing increased darkening and melting.

As ageomicrobiologist,JenineMcCutcheon, a professor in the Earth and Environmental Sciences department at the University of ݮƵ,has been studying Greenland’s glacieralgae in an effort to uncover their changing annual patterns. This research, done during her postdoctoral fellowship at the University of Leeds,was publishedJanuary 25th in Nature Communications.

“What we’re tryingto do is to better understand how algal blooms form, why they form where they do and is there a way to predict how they’ll form in future melt seasons,”saysMcCutcheon. “One season to the next,algal blooms may change and vary in intensity, making them difficult to model year-to-year.”

Prof JenineMcCutcheon

>ProfessorJenineMcCutcheonsampling snow and ice on the Greenland Ice Sheet.
> Photo: AndrewTedstone, PhD

Understanding algal bloom development is important because these blooms darken the ice sheet surface, causing it to melt more quickly than ice that is free of glacier algae. Ice sheet darkening by glacier algae is just one reasonwhysurface melting of the Greenland Ice Sheet has accelerated in recent decades. Since the Greenland Ice Sheet contains enough water to raise sea level by overseven meters, it is crucial to understand all of the processes that impact melting in order to predict how melting will proceed in the years to come.

Behind the research

The study focused onfivedifferent locations alonga large bandon the Western edgeof the Greenland Ice Sheet known as the “Dark Zone” due to itslow albedo (a measure ofthe amount ofsolarradiationreflectedbyasurface).The ice surface in this zone is made dark byimpurities such as algal cells, mineral dust, and black carbon (particles produced by fossil fuel combustion). Algal blooms are the primary cause ofthedarkeningobservedin this region.

dark zone pictured

>Aerial photo of the Greenland Ice Sheet’s Dark Zone.
>Photo:ProfessorJenineMcCutcheon

In order to determine whereglacieralgae gettheirnutrients, the team measured the photosynthesis rate ofglacieralgaein the presence of the different nutrients.Theyfound thatthere was a distinct improvement whenthe algaewere provided with phosphorus.The team concluded that the algal bloomsin this regionwere regulated and limited by the presence of phosphorus.

Upon finding this, they analyzedthe surfacedust present in the Dark Zone aroundthealgal blooms, and foundthe mineralhydroxylapatite.Hydroxylapatitecontainsthebio-availablephosphorusneeded to nourish the algae, andlikelyfacilitates the development of glacier algal blooms by supplying phosphorus to theicesurface habitat.

The reliance of algae on this mineral dust then creates a positive feedback loop, whereinthe more algae that bloom, the greater the ice sheet melting.Asmore ice melts, mineraldust frozen in the icebecomesexposed, thusproviding more nutrients to helptheglacieralgae grow. However, more studies are needed to quantify this feedback loop and measure its extent.

“The findings of this study will impact howwepredict where the blooms will happen in the future,” McCutcheonsays.“We’re working to be able to model these algal blooms and match them with satellite data toget a better understanding of the overall impact of these algal blooms on ice sheet albedo reduction and resulting melting.”

This research was done through an international collaboration by researchers from the United Kingdom, Germany, Belgium,Canada,and Denmark, and was funded by the UK Natural Environmental Research Council Consortium Grant.