Arctic fjords are social-ecological systems
Glacier fronts and sea ice systems are hotspots of biodiversity. Their retreat will pose threats to Arctic coastal ecosystem function and eventually local livelihoods. The Arctic is a harbinger of the consequences of multiple global and regional environmental change on ecosystems and livelihoods: The overarching objective of FACE-IT is to enable adaptive co-management of social-ecological fjord systems in the Arctic in the face of rapid cryosphere and biodiversity changes.
14
International
institutions
7
Unique
sample sites
8
Countries
Latest Updates
Impact of climate change on Arctic macroalgal communities
The Arctic region faces a warming rate that is more than twice the global average. Sea-ice loss, increase in precipitation and freshwater discharge, changes in underwater light, and amplification of ocean acidification modify benthic habitats and the communities they host.
FACE-IT Scenario Workshop in Longyearbyen, Svalbard
On 26 August 2022, FACE-IT will be hosting a scenario workshop in Nuuk, Greenland, inviting stakeholders of the Nuup Kangerlua fjord to explore how climate change and other factors might affect the fjord and its future value for fishing and hunting, tourism, recreation and other activities.
Arctic fjords without ice? Biological and societal effects of melting glaciers
Public Colloquium: 30 November 2022
High Ecophysiological Plasticity of Desmarestia aculeata (Phaeophyceae) Present in an Arctic Fjord under Varying Salinity and Irradiance Conditions
The seaweed Desmarestia aculeata (Phaeophyceae) is distributed in the temperate zone of the North Atlantic up to the Arctic, where it is exposed to a high Arctic light regime and fluctuating salinity conditions resulting from glacial and terrestrial run-off. Information on how this species is able to thrive under current and future Arctic conditions is scarce.
Light and freshwater discharge drive the biogeochemistry and microbial ecology in a sub-Arctic fjord over the Polar night
The polar night has recently received increased attention as a surprisingly active biological season. Yet, polar night microbial ecology is a vastly understudied field. To identify the physical and biogeochemical parameters driving microbial activity over the dark season, we studied a sub-Arctic fjord system in northern Norway from autumn to early spring with detailed monthly sampling.
Coastal freshening drives acidification state in Greenland fjords
Greenland’s fjords and coastal waters are highly productive and sustain important fisheries. However, retreating glaciers and increasing meltwater are changing fjord circulation and biogeochemistry, which may threaten future productivity. The freshening of Greenland fjords caused by unprecedented melting of the Greenland Ice Sheet may alter carbonate chemistry in coastal waters, influencing CO2 uptake and causing biological consequences from acidification.
Seasonal mesozooplankton patterns and timing of life history events in high-arctic fjord environments
Seasonal patterns in mesozooplankton composition, vertical distribution, and timing of reproduction are challenging to study in the open sea due to ocean currents and mix of populations of different origins. Sill fjords, on the other hand, with restricted water exchange, are ideal locations for studying taxa- and community-specific adaptations to the prevailing environment.