Long-term monitoring via at-sea surveys is a method used to examine seabird responses to anomalously warm or ice-free conditions in the Arctic.
The Arctic marine mammal community consists of 11 resident Arctic endemic species and approximately 25 seasonally-resident species that migrate into Arctic waters to forage during the open-water period.
Fish species in the Arctic may respond more directly and quickly to physical changes than other marine vertebrates, but they are generally more limited in mobility than seabirds and marine mammals.
As Arctic conditions change, the movement of frontal boundaries will impact the location, duration, and energetic costs of fish migration.
Global warming has induced variability in the timing of migration for many marine mammal species, including Arctic endemics.
Matthews et al. (2020b) concluded that the presence of killer whales influences bowhead whales to select sea ice habitats as a defensive strategy in Arctic environments.
A 2016 study by Hamilton et al. examined the use of glacial refugia by ringed seals (Pusa hispida) following a regional sea-ice collapse in the Arctic.
Longer open-water seasons, warmer ocean temperatures, and stronger winds in the Arctic have resulted in earlier spring production blooms and often extended open-ocean plankton blooms into late summer, which alters prey types and distributions.
Hauser et al. (2018a) studied the indirect effects of sea ice loss on the summer-fall habitat and behavior of sympatric populations of an Arctic marine predator.
Post-breeding seabirds and migrant baleen whales arrive in the Arctic from the Subarctic or nearby temperate realms.
Arctic cod (Boreogadus saida) and polar cod (Arctogadus glacialis) are important forage fishes for predators in Arctic and Subarctic regions.
Capelin (Mallotus villosus) and several gadid species are marine fishes that migrate seasonally to the Arctic.
Matthews et al. (2024) inferred that dietary plasticity and broad North Atlantic origins, as indicated by bulk and amino acid-specific δ15N and δ13C isotope analysis, support the expansion of killer whale ranges into Arctic waters.
Kuletz et al. (2024) documented seabird responses to ecosystem changes driven by marine heatwaves in a warming Arctic.
Pettitt‐Wade, H., Loseto, L. L., Majewski, A., and Hussey, N. E. published the paper 'Cod movement ecology in a warming world: circumpolar arctic gadids' in Fish and Fisheries in 2021.
Kittlitz’s murrelets (Brachyramphus brevirostris) nest in Subarctic coastal areas of the northern Gulf of Alaska and migrate to the Arctic post-breeding.
Arctic and Subarctic regions provide resources for both resident species and species that migrate north from more southerly regions.
The energetic costs of extending the Arctic portion of the non-breeding route for short-tailed shearwaters could negatively impact their survival and reproductive success.
Declines in landfast ice in fjords and along Arctic coasts have increased the seasonal mixing of Arctic and Subarctic fish, avian, and mammalian species.
Klaassen (2003) examined the relationships between migration and breeding strategies in Arctic breeding birds.
Historically, seasonal sea-ice formation in the Arctic expanded from November to March.
Short-tailed shearwaters make few foraging stops when migrating from the Arctic to their Australian breeding grounds.
Marine vertebrates that migrate to or within the Arctic face challenges to their survival and reproductive success due to increasing environmental unpredictability caused by climate change.
The high-Arctic seabird community is undergoing ongoing shifts as the Arctic becomes boreal.
The most abundant anadromous fishes in the Arctic include members of the sub-family Salmoninae (Pacific salmon, Atlantic salmon, sea trout, and char) and members of the Coregoninae (whitefishes and ciscoes).
Increased ship traffic and human activities in the Arctic are anticipated to affect the movement patterns of Arctic cod, seabirds, and marine mammals.
The Greenland shark is the most migratory elasmobranch in the Arctic, capable of long-distance migrations exceeding 1,000 km and conducting excursions between inshore and offshore waters, according to Campana et al. (2015) and Edwards et al. (2022).
The Arctic coastline within the CAFF-defined region is approximately 45,390 km.
At least a portion of the black-legged kittiwake (Rissa tridactyla) population travels over the Arctic from a colony in the Barents Region to overwintering sites in the Chukchi and Bering seas, and more cross-Arctic migrations of this species could occur as sea ice declines.
The expansion of Subarctic fish species into the Arctic is primarily driven by increasing water temperatures and declining sea-ice distribution (Mueter et al., 2021).
Atlantic drift-ice seals, specifically harp seals (Pagophilus groenlandicus) and hooded seals (Cystophora cristata), breed in the spring in the southern parts of their ranges, migrate northward to molt and forage during the summer in Arctic waters, and return south in the fall.
The retraction of sea ice removes essential habitat for certain animals and increases the spatial overlap between different species.
Watt et al. (2016) observed a shift in the foraging behavior of beluga whales (Delphinapterus leucas) from the Cumberland Sound population, which may reflect a changing Arctic food web.
Changes in spring blooms and zooplankton biomass affect competition among species at different trophic levels in the Arctic.
Many marine mammals have adjusted to changing environmental conditions by arriving earlier and staying longer in summer Arctic foraging areas, utilizing their large body size and body fat reserves (Hauser et al., 2017; Szesciorka et al., 2024).
Animals that remain in the Arctic year-round often conduct seasonal movements within Arctic areas, as documented by Alerstam et al. (2007) and Pettitt-Wade et al. (2021).
ICC-Alaska (2015) published 'Alaskan inuit food security conceptual framework: how to assess the Arctic from an Inuit perspective: summary report and recommendations report' in Anchorage, Alaska.
In Arctic and Subarctic regions, migratory fishes are categorized into two types: anadromous fishes, which hatch in fresh water, migrate to the ocean, and return to freshwater to reproduce, and strictly marine fishes, which complete their entire life cycle in the ocean.
Subarctic and temperate animals that depend on the Arctic’s summer production period migrate north as sea ice retreats and return south as winter advances, darkness increases, and temperatures drop, as described by Berge et al. (2015a).
Establishing adaptable monitoring programs for Arctic species requires planning for contingencies and collaboration with local Arctic residents.
Anadromous and marine fishes, certain marine mammals, and at least three species of seabirds exhibit resident migration patterns within Subarctic or Arctic areas.
The article titled 'A review of climate change impacts on migration patterns of marine vertebrates in Arctic and Subarctic ecosystems' was published in the journal Frontiers in Environmental Science on October 25, 2024.
Warmer conditions and early spring sea-ice melt in the Arctic have led to earlier spring blooms, increased chlorophyll levels, and higher zooplankton biomass that experiences faster turnover, though this biomass consists of smaller, low-nutrient prey species.
Extreme seasonal patterns of daylight in the Arctic likely restrain the effectiveness of phenological responses of marine vertebrates to environmental change, particularly for species that breed in the Arctic.
Ford, J. D., Pearce, T., Canosa, I. V., and Harper, S. (2021) published 'The rapidly changing Arctic and its societal implications' in WIREs Climate Change, volume 12, article e735, discussing the societal impacts of environmental changes in the Arctic.
Polar cod (Boreogadus saida) and capelin (Mallotus villosus) serve as key species in the marine food webs of the Arctic and the Barents Sea, as described in a 2013 study by Hop and Gjøsæter.
The decline in the area, thickness, and seasonal duration of Arctic sea ice over the last 20 years has significantly altered the Arctic ecosystem, a trajectory predicted to continue as northern-latitude temperatures rise due to anthropogenic carbon emissions.
Ocean warming may facilitate the movement of efficient predatory fishes into the Arctic, potentially causing cascading top-down effects on marine food webs.
A 2021 study published in the Journal of Hydrology (Vol. 600, 126462) examines patterns, trends, and connections between Bering Sea marine heatwaves and the Arctic.
Arctic marine mammals are increasingly vulnerable to vessel traffic in the Northwest Passage and Northern Sea Route due to the region becoming increasingly ice-free, according to a 2018 study by Hauser et al.
Sexson et al. (2016) published a study titled 'Shifts in the distribution of molting spectacled eiders (Somateria fischeri) indicate ecosystem change in the Arctic' in Ornithological Applications.
Breeding migrants are seabird species that migrate from the Subarctic and other regions to breed in the Arctic.
Climate change is impacting endemic Arctic marine mammals through direct habitat alterations, ecosystem changes, and changing patterns of human activity.
Rapid changes in the Arctic environment will strain evolutionary-scale relationships regarding seabird migration timing.
von Biela et al. (2023) documented the 'borealization' (a shift toward boreal species) of nearshore fishes on an interior Arctic shelf over multiple decades.
The timing and extent of sea-ice retreat in the Arctic acts as a primary driver for marine systems, affecting water-column characteristics, the phenology and spatial extent of primary production, and the abundance, species composition, and nutritional quality of lower trophic organisms.
Most migration to the Arctic occurs latitudinally, with some species migrating from the Antarctic to the Arctic, while other migration occurs longitudinally across the circumpolar realm.
Moore and Hauser (2019) advocate for integrating conventional science and indigenous knowledge to track Arctic ecosystem variability, specifically regarding marine mammal ecology and health.
Altered animal distributions, changes in phenology, and reduced sea ice affect access to animals that are critical nutritional, economical, and cultural components of Indigenous people’s lives in the Arctic.
Mueter et al. (2021) developed future scenarios for Subarctic and Arctic marine systems in the gateways to the Arctic, focusing on prey resources, food webs, fish, and fisheries.
Huntington et al. (2021) discussed whale hunting practices within indigenous Arctic cultures.
Vihtakari et al. (2018) identified black-legged kittiwakes as indicators of 'Atlantification' (the influx of Atlantic water) in the Arctic.
Arctic sea ice has experienced a decline in area, thickness, and seasonal duration over the last 20 years, a trend expected to continue as northern latitude air and water temperatures increase.
Fossheim, M., Primicerio, R., Johannesen, E., Ingvaldsen, R. B., Aschan, M. M., and Dolgov, A. V. (2015) published 'Recent warming leads to a rapid borealization of fish communities in the Arctic' in Nature Climate Change, volume 5, pages 673–677, reporting on the shift in Arctic fish community composition due to warming.
Perrette, M., Yool, A., Quartly, G. D., and Popova, E. E. published the paper 'Near-ubiquity of ice-edge blooms in the Arctic' in Biogeosciences in 2011.
Approximately 64 seabird species utilize the Arctic, with about 30 of those species breeding exclusively within the Conservation of Arctic Flora and Fauna (CAFF) boundaries.
The reduction in sea ice in the Arctic is likely to increase human activities such as vessel traffic, oil, gas, and mining exploration and extraction, and coastal construction, which introduce artificial light, ocean noise, and collision risks that impact the migratory behaviors of some species.
Several boreal fish species, including capelin, Atlantic cod (Gadus morhua), and haddock (Melanogrammus aeglefinus), migrate seasonally to the Arctic to feed on lipid-rich prey.
Indigenous hunting opportunities in the Arctic have been lost due to accelerating climate change, as revealed through co-production of knowledge in a 2021 study by Hauser et al.
Seasonal and long-term sea ice have historically functioned as critical structural components of marine ecosystems throughout the circumpolar Arctic and Subarctic, as noted by Taylor et al. (2022) and IPCC et al. (2023).
Boreal species typically have distribution centers farther south and undertake seasonal migrations to the Arctic to feed, arriving in early summer and departing before freeze-up, according to Lynghammar et al. (2024).
Climate warming has caused increased ocean temperatures and significant reductions in sea-ice thickness, extent, and seasonal duration across the North Atlantic and Arctic range of hooded seals over the past three decades, leading to the 'Atlantification' of physical and biological conditions.
Sea-ice loss removes ecological barriers and creates ecological bridges across the Arctic, providing marine animals with increased access to prey and new travel corridors.
Some avian species are long-distance migrants that travel from the Southern Hemisphere to the Subarctic and Arctic solely to feed and increase body reserves.
Resident species in Subarctic or Arctic areas spend most or all of their life cycle within those regions but exhibit regular movements within those areas, a pattern observed in some anadromous and marine fishes, certain marine mammals, and at least three species of seabirds.
McMeans et al. (2013) assessed the role of Greenland sharks (Somniosus microcephalus) in the Arctic ecosystem using stable isotope and fatty acid analysis.
Clairbaux et al. (2019) suggest that climate change could alter bird migration patterns, potentially leading to transarctic flights and high-latitude residency in an Arctic free of sea ice.
The review scope covers the marine and associated freshwater inflows across the circumpolar Arctic as defined by the Arctic Council’s Conservation of Arctic Flora and Fauna (CAFF) boundaries.
Kokelj et al. (2021) reported that thaw-driven mass wasting couples slopes with downstream systems, with effects propagating through Arctic drainage networks.
Polyakov, I. V., Ingvaldsen, R. B., Pnyushkov, A. V., Bhatt, U. S., Francis, J. A., and Janout, M. published the paper 'Fluctuating Atlantic inflows modulate Arctic atlantification' in the journal Science in 2023.
Forecasting changes in migratory phenology and routes for most Arctic and many Subarctic species is challenging due to limited historic and current data.
A 2022 report by Harris et al. discussed the status of Arctic char in a rapidly changing North.
Large demersal species in the Arctic that extend to the Subarctic include flatfishes such as Greenland halibut (Reinhardtius hippoglossiodes), Arctic skate (Amblyraja hyperborea), and the Greenland shark.
Unpredictability in Arctic physical and biological conditions poses a significant challenge for marine vertebrates that rely on migration for survival and reproductive success.
J. Lin, P. Yang, X. Pan, M. Ishitsuka, and Y. (2021) published 'Recent changes to Arctic river discharge' in Nature Communications, volume 12, article 6917, documenting hydrological shifts in the Arctic.
Climate change is altering seasonal habitats and food bases for fishes, seabirds, and marine mammals throughout the circumpolar Arctic.
The establishment of new northern gannet colonies in the Arctic is associated with the northward movement of prey species like herring (Clupea harengus) and mackerel, driven by the warming of the Barents Sea.
In nearshore Arctic areas, earlier ice break-up and warming air and sea surface temperatures negatively impact food security and traditional cultural practices that rely on access to migratory marine vertebrates.
Hooded seals (Cystophora cristata) have changed their migration phenology by departing northward earlier and departing southward later, which has resulted in an extended period of residency in the Arctic.
Mackerel and Atlantic bluefin tuna occasionally migrate to the Arctic from their southern ranges, despite their spawning areas remaining in the eastern North Atlantic and the Mediterranean Sea, respectively, according to Mackenzie et al. (2014) and Berge et al. (2015b).
Indigenous Knowledge contributes to the interpretation of observed changes in animal migration and helps identify equitable solutions to Arctic climate change.
The open water season in Arctic gateway areas currently extends from May to December, according to Stabeno and Bell (2019), Efstathiou et al. (2022), Isaksen et al. (2022), and Urbanski and Litwicka (2022).
In the Arctic, marine-based prey that support upper trophic level taxa are typically only available during the brief Arctic summer and fall.
The Fram Strait serves as the Atlantic gateway to the Arctic, measuring approximately 450 km wide and 5,500 meters deep, with the relatively warm West Spitsbergen Current acting as the primary inflow.
Adult polar cod (Arctogadus glacialis) may perform long seasonal movements of less than 200 kilometers within the Arctic.
Silber and Adams (2019) published a study titled 'Vessel operations in the Arctic, 2015–2017' in Frontiers in Marine Science.
Shearwaters act as capital migrants in the Arctic and Subarctic by storing fat reserves for long southerly transits with minimal foraging, according to Woehler and Hobday (2024).
Increased numbers of Subarctic species in the Arctic can result in greater competition for resources, such as diet overlap, which potentially causes declines in endemic populations and alters ecosystem structure, as observed with Arctic cod in the Atlantic Arctic (Renaud et al., 2012; Christiansen, 2017).
Some seabird species, such as Ardenna shearwaters and Aethia auklets, nest in regions south of the Arctic or in Subarctic regions but migrate seasonally to the Arctic to forage opportunistically during post-breeding periods.
Non-breeding migrants arrive in the Arctic during summer and fall specifically to feed.
For seabirds that migrate to the Arctic for post-breeding replenishment, the additional distance to prey fields that have moved farther north may no longer be energetically beneficial (Kuletz et al., 2024).
Matthews et al. (2020a) determined that the presence of epizoic barnacles on Arctic killer whales indicates that these whales previously resided in warmer waters.
Arctic marine vertebrates are categorized into three groups regarding migration: 1) Arctic residents with seasonal movements (species that complete their life cycle within the Arctic but move seasonally), 2) Breeding migrants (seabirds that enter the Arctic to breed and migrate south in the fall), and 3) Summer visitors for feeding (boreal fishes, seabirds, and marine mammals that arrive in the northern summer to feed but breed elsewhere).
The review of Arctic marine ecology regarding migration covers fishes, seabirds, and marine mammals, utilizing sources from scientific journals, books, and agency reports identified via Google Scholar and Web of Science.
The spatio-temporal match between Arctic-breeding seabirds and their prey is critical due to the region's brief summer season and extreme seasonal variations in daylight, temperature, open water access, and prey availability.
Animals must synchronize the timing of their movements with food resource availability, a requirement that is particularly critical for species migrating to the Arctic to breed.
The Atlantic Arctic region is experiencing more rapid environmental changes than any other Arctic area.
Arctic-breeding seabirds exhibit diverse migratory patterns, ranging from movements within a single ocean basin to long-distance migration between the Arctic and Antarctic, as seen in Arctic terns (Sterna paradisaea).
M. Daase, S. Falk-Petersen, Ø. Varpe, G. Darnis, J. E. Søreide, and A. Wold examined the timing of reproductive events in the marine copepod Calanus glacialis from a pan-Arctic perspective in a 2013 study.
Leu et al. (2015) identified the steering principles behind the phenology of vernal ice algal blooms in the Arctic.