Arctic marine mammal population status, sea ice habitat loss, and conservation recommendations for the 21st century DOI Open Access
Kristin L. Laidre, Harry L. Stern, Kit M. Kovacs

et al.

Conservation Biology, Journal Year: 2015, Volume and Issue: 29(3), P. 724 - 737

Published: March 17, 2015

Arctic marine mammals (AMMs) are icons of climate change, largely because their close association with sea ice. However, neither a circumpolar assessment AMM status nor standardized metric ice habitat change is available. We summarized available data on abundance and trend for each species recognized subpopulation. also examined diversity, the extent human use, temporal trends in 12 regions by calculating dates spring retreat fall advance from satellite (1979–2013). Estimates varied greatly quality, few studies were long enough analysis. Of subpopulations, 78% (61 78) legally harvested subsistence purposes. Changes phenology have been profound. In all except Bering Sea, duration summer (i.e., reduced ice) period increased 5–10 weeks >20 Barents Sea between 1979 2013. light generally poor data, importance forecasted environmental changes 21st century, we recommend following effective conservation: maintain improve comanagement local, federal, international partners; recognize spatial variability subpopulation response to change; implement monitoring programs clear goals; mitigate cumulative impacts activity; limits current protected legislation. Estado de las Poblaciones Mamíferos Marinos del Ártico, la Pérdida Hábitats Hielo Marino y Recomendaciones Conservación para el Siglo XXI Los mamíferos marinos Ártico (MMA) son emblemas cambio climático, principalmente por su asociación cercana con hielo marino. Sin embargo, no se encuentran disponibles ni una evaluación estado los MMA medida estandarizada en hábitat Resumimos datos sobre abundancia tendencia cada especie reconocimos subpoblaciones. También examinamos diversidad especies, extensión uso parte humanos tendencias temporales marino doce regiones al calcular fechas retroceso hielos primavera avance otoño partir satelitales estimados variaron enormemente calidad pocos estudios fueron lo suficientemente largos como realizar un análisis tendencia. De subpoblaciones MMA, cazadas legalmente razones subsistencia. cambios fenología han sido profundos. En todas regiones, salvo Mar Bering, duración periodo verano (es decir, reducción hielo) incrementó semanas entre A razón generalmente pobres, importancia ambientales pronosticados XX1, recomendamos siguiente conservación efectiva MMA: mantener mejorar co-manejo socios locales, federales e internacionales; reconocer variabilidad espacial respuesta sub-poblaciones climático; implementar monitoreo programas objetivos claros; mitigar impactos acumulativos incremento actividad humana; límites legislación actual especies protegidas. The world's disproportionately threatened compared terrestrial counterparts (Schipper et al. 2008), 11 arctic particularly vulnerable due dependence (Laidre 2008a; Kovacs 2012; Reid & Laidre 2013). Some AMMs obligates, meaning life history events (e.g., reproduction, molting, resting) feeding depend ice, whereas others use but do not it completely 2008a). By mean that occur north Circle (66° 33′ N) most year ecosystem aspects selected seasonally inhabit waters may live outside part year. include 3 cetaceans (narwhal [Monodon monoceros], beluga [Delphinapterus leucas], bowhead [Balaena mysticetus] whales); 7 pinnipeds (ringed [Pusa hispida], bearded [Erignathus barbatus], spotted [Phoca largha], ribbon [Histriophoca fasciata], harp [Pagophilus groenlandicus], hooded [Cystophora cristata] seals walrus [Odobenus rosmarus]); polar bear (Ursus maritimus). Throughout much range, these animals important cultural nutritional resources indigenous nonindigenous peoples. Recent reviews outline vulnerabilities 2011). Warming over past decades has about 2 times greater than global (IPCC rate loss faster predicted models (Stroeve 2012), projections suggest an ice-free 2040 (Overland Wang Even if greenhouse gases, primary driver limited immediately, likely continue several Therefore, appears continued unprecedented habitats inevitable. reviewed what known population abundance, or stock. evaluated richness across quantified use. assessed provide first comparative measure change. Based our findings, make recommendations conservation relative gaps, forecasts, anthropogenic activities, complex social, economic, political context rapidly warming Arctic. compiled estimates published unpublished sources. Subpopulations included those management bodies advisory groups such as International Whaling Commission (IWC), North Atlantic Marine Mammal (NAMMCO), Union Conservation Nature (IUCN) specialist groups. Trends associated time frames reported authors noted. delineated regions, modified slightly Flora Fauna (CAFF) Circumpolar Biodiversity Monitoring Plan (CAFF 2011) (Fig. 1). central Basin was excluded paucity data. calculated number per region determining whether had legal commercial harvest. Habitat 1979–2013 daily concentration satellites (Supporting Information). date given when area fell below specific threshold, rose above same threshold. used region-specific threshold halfway March September areas baseline decade (1982–1991) characterize biologically transitions winter conditions. highest Baffin Bay, Davis Strait, Sea; lowest Okhotsk Beaufort Sea. availability quality here through 2015 widely (Table 1 Fig. 2). many cases, knowledge consisted single point estimate large uncertainty based expert opinion without formal bias. For cetaceans, 5 19 0 narwhal 4 subpopulations. Abundance ringed seal outdated, some small surveyed repeatedly seals. areas; however, represented only portion discreteness subpopulations uncertain. Trend suggested increased, stable declined. bears, 14, although out uncertainty. Current 10 derived projection untested assumptions Evaluation complicated unknown structure partial surveys seasonal aggregations. High survey methods, surveys, levels precision made summary difficult. Nonetheless, 35% 78 identified found taken nations Norway (including Svalbard). review subspecies, (n = 61) regularly 76% (74% belugas, 91% narwhals, 50% whales), including stocks which whales captured aquaria (White Sea). Approximately 80% pinniped walruses subsistence, purposes Norway, Canada, Russia (harp [Table 1]). Kara Laptev where illegal harvest occurs. Large occurred nearly habitats. Eleven showed statistically significant toward earlier retreat, later advance, and, consequently, longer summers 3, Supporting Only trend. effect 34-year season 2013 1979. largest 20 this period. sensitive choice they defined Information) typically fall. negatively correlated Climate widespread ecological (Rosenzweig 2008; Gilg Post 2013), yet its effects relatively underreported despite abiotic exceed temperate, tropical, montane biomes (ACIA 2005). quantitative evidence negative ice-obligate (Stirling 1999; Regehr 2007; Øigard 2010, 2013; 2010). species- subpopulation-specific responses vary space, evidenced delayed even positive (Moore 2006; Quakenbush 2011; Stirling Rode 2014; George 2015). Variability can arise differences exploitation histories, strategies, biological productivity, trophic interactions. Such heterogeneity respect systems, tend be more rich (Moritz Agudo Assessing mammal populations difficult wide distributions cryptic behavior compounded logistical challenges surveying remote areas. understanding identifying priorities, absent 3), lack will limit utility future assessments. Although expected lower carrying capacity ice-dependent species, currently recovering [George 2015], sport hunting [Schliebe 2006]) previously insufficiently managed prior 2000 West Greenland [Witting Born 2013]). short term, recovery previous overexploitation could mask reductions loss. addition, productivity could, period, offset potential result transient term increases (Quakenbush St Lawrence Estuary Cook Inlet beluga) show cessation harvesting (Wade 2012). modern world, rare wild mammals, particular top predators, support well-being communities, do. subspecies hunted commercially. Thus, intertwined renewable resource. responsibility resides federal state government agencies partners representing communities. Many under regional, national, agreements share decision-making power framework harvests supported national laws U.S. Protection Act, Nunavut Land Claims Agreement). comprehensive list, examples Alaska Native working United States Beluga Committee, Eskimo Commission, Walrus Nanuuq Ice Seal Committee. Inuvialuit Fisheries Joint Management Committee; Wildlife Boards Nunavut, Nunavik, Nunatsiavut; Polar Bear Administrative Chukotka (Russia), Associations Hunters (KNAPK) Association Traditional Chukotka, respectively, cooperate agencies. Furthermore, Greenland, carried local composed mainly ethnic Inuit. highly mobile undertake movements, resulting half 1) ranging regional boundaries, quantify movement poor. transboundary requires collaboration. Currently, bears joint commissions Canada Greenland; Russia) information shared Inupiat-Inuvialuit Agreement Canadian Technical Committee (also Greenland). Scientific narwhals though Canada–Greenland Narwhal-Beluga NAMMCO. receive advice NAMMCO, catch Russia, States, set IWC. Advice coordinated Council Exploration Seas Organization. It well established declining every month monthly areal capture timing annual influence feeding, AMMs. therefore This meaningful approach other metrics appropriate 1979-2013, 17 days/decade 25 consistent findings Stammerjohn (2012), who methods similar ours, Stroeve (2014), detection liquid water surface snow obtain melt onset freezing regions. addition extent, thickness decreased substantially (Schweiger Continuation induce (Notz 2009) possibly weather anomalies warm strong storm) impact thin correlation transition 2) manifestation ice-albedo feedback, extra heat absorbed ocean during early must released into atmosphere before begin form. direct indirect comprehensively (2008a) (2011). Loss affected survival (Regehr Pinniped pup related breakup young need sufficient suckling weaning (Øigard 2010; Absence Pacific calf crushing at crowded haul-out sites (Jay Physical properties, roughness depth (which decreasing [Webster 2014]), suitability lairs (Furgal 1996; Iacozza Ferguson 2014). Timing linked accessibility foraging production bloom ultimately influences (Carmack Wassmann 2006). Indirect consequences overlap new predators competitors. Finally, both ability humans access them fraction takes place near edge affecting abate immediate future. At present, there agreement reduce emissions gasses, unabated versus aggressive mitigation scenarios substantively diverge until least years fixed regardless efforts greenhouse-gas emissions. reduction solution mitigating long-term warming, scientists, managers, conservationists, industry, communities dependent prepare deal Accordingly, conservation. Maintaining increasing governmental entities key component face climate-induced viability (see "Human Use" section). culture people throughout (Born Comanagement directly involve resource vested interest it. They lead community participation minimizing human–polar conflicts), collection traditional knowledge, compliance restrictions, identification science priorities opportunities scientific sampling. Arctic, activities benefits prohibitively expensive otherwise infeasible involvement. Future require balancing needs declines There scientifically incremental balance social If loss, responsible percentage [Runge 2009; 2015]) hold unlikely accelerate environmentally driven declines. either updated periodically conservative levels. precautionary warranted populations, whereby increasingly risk-averse applied decline size resilience. Given fast pace how respond, flexible adaptive critical. articulation goals targets. users managers reducing human-caused disturbance removals, harvests, one mechanisms (but necessarily offset) Species exhibit variable space (Post 2009, Moritz variation characteristics ice), species' move favorable habitats, phenotypic behavioral plasticity, genetic traits bolster managing scales 2012) should incorporated predictive plans. contrasting climate. Chukchi southern rates 2), body condition reproductive parameters historic values region, declined (Rode Samples subsistence-harvested northern 2000s indicate vital better 1960s 1970s 2011), 1992 2011 (Harwood seals, observed attributed productivity. whale shown growth concurrent Both Bering-Chukchi-Beaufort (BCB) low whaling >3%/year, theoretical maximum (Wiig Givens time, BCB improved 1989 (George 2015), extensive productive Though showing recent changes, forecasts next 50–100 (Wang Overland serious threats Models forecast century Amstrup Udevitz 2013) inform prescribe term. Part challenge broad resolutions frames. Pitfalls making decisions coarse-resolution missed opportunities, sustainable latter risk alienating stakeholders compromising efforts. that, possible, consider risks coarse fine scales. monitored determine scale. Measuring trend, indicator status, demographic analysis reproduction survival), elusive distribution AMMs, acquiring realistic; thus, develop samples provides opportunity, collaboration suite age maturity, pregnancy rate, condition, pollution, contaminant loads) serve broader indicators. Other feasible monitor sensing observation Gulland analyzed together regular areas, reasonable strategy. Long-term provided foundation Western Hudson Bay Southern [Stirling 2010]) conjunction hunters, amounts cost. Successful Department Fish Game's Bio-monitoring Program Slope Borough's sampling program Harvest biosampling successfully conducted Canada. plans drafted whales, 2008b; Simpkins Vongraven 2014), systematically implemented. factors insufficient funding, organization will, awareness plans, absence major economic incentives cooperation biodiversity often projects span agency interests authority. rigorous, any work outlined plan while concurrently performing focused necessary meet needs. With physical barrier interchange disappearing (Heide-Jørgensen complicates emphasizes analyses. On level, moving Assessment CAFF Program. range states preparing action auspices 1973 Bears. An example successful Ocean Antarctic

Language: Английский

CryoSat‐2 estimates of Arctic sea ice thickness and volume DOI

Seymour W. Laxon,

Katharine Giles,

A. Ridout

et al.

Geophysical Research Letters, Journal Year: 2013, Volume and Issue: 40(4), P. 732 - 737

Published: Feb. 20, 2013

Satellite records show a decline in ice extent over more than three decades, with record minimum September 2012. Results from the Pan‐Arctic Ice‐Ocean Modelling and Assimilation system (PIOMAS) suggest that has been accompanied by volume, but this not confirmed data. Using new data European Space Agency CryoSat‐2 (CS‐2) mission, validated situ data, we generate estimates of volume for winters 2010/11 2011/12. We compare these current PIOMAS earlier (2003–8) National Aeronautics Administration ICESat mission. Between periods, autumn declined 4291 km 3 winter 1479 . This exceeds central Arctic model 2644 autumn, is less 2091 winter, between two time periods.

Language: Английский

Citations

801

Changes in Arctic melt season and implications for sea ice loss DOI Creative Commons
Julienne Strœve, T. Markus, Linette Boisvert

et al.

Geophysical Research Letters, Journal Year: 2014, Volume and Issue: 41(4), P. 1216 - 1225

Published: Feb. 5, 2014

Abstract The Arctic‐wide melt season has lengthened at a rate of 5 days decade −1 from 1979 to 2013, dominated by later autumn freezeup within the Kara, Laptev, East Siberian, Chukchi, and Beaufort seas between 6 11 . While onset trends are generally smaller, timing large influence on total amount solar energy absorbed during summer. additional heat stored in upper ocean approximately 752 MJ m −2 last increases sea surface temperatures 0.5 1.5 °C largely explains observed delays Arctic Ocean's adjacent seas. Cumulative anomalies radiation May through September for most recent pentad locally exceed 300–400 Beaufort, Siberian This extra is equivalent melting 0.97 1.3 ice

Language: Английский

Citations

718

Effects of Arctic Sea Ice Decline on Weather and Climate: A Review DOI Creative Commons
Timo Vihma

Surveys in Geophysics, Journal Year: 2014, Volume and Issue: 35(5), P. 1175 - 1214

Published: March 8, 2014

The areal extent, concentration and thickness of sea ice in the Arctic Ocean adjacent seas have strongly decreased during recent decades, but cold, snow-rich winters been common over mid-latitude land areas since 2005. A review is presented on studies addressing local remote effects decline weather climate. It evident that reduction cover has increased heat flux from ocean to atmosphere autumn early winter. This locally air temperature, moisture, cloud reduced static stability lower troposphere. Several based observations, atmospheric reanalyses, model experiments suggest decline, together with snow Eurasia, favours circulation patterns resembling negative phase North Atlantic Oscillation Oscillation. suggested large-scale pressure include a high which cold Europe northeastern Eurasia. western low eastern America also suggested, favouring advection masses America. Mid-latitude winter is, however, affected by several other factors, generate large inter-annual variability often mask decline. In addition, small sample years loss makes it difficult distinguish directly attributable conditions. that, advancing global warming, continents will no longer be second half twenty-first century. Recent causal links between summer precipitation Europe, Mediterranean, East Asia.

Language: Английский

Citations

687

Arctic sea ice variability and trends, 1979–2010 DOI Creative Commons

D. J. Cavalieri,

Claire L. Parkinson

˜The œcryosphere, Journal Year: 2012, Volume and Issue: 6(4), P. 881 - 889

Published: Aug. 15, 2012

Abstract. Analyses of 32 yr (1979–2010) Arctic sea ice extents and areas derived from satellite passive microwave radiometers are presented for the Northern Hemisphere as a whole nine regions. There is an overall negative yearly trend −51.5 ± 4.1 × 103 km2 yr−1 (−4.1 0.3% decade−1) in extent hemisphere. The trends individual regions all except Bering Sea: −3.9 1.1 (−8.7 2.5% Seas Okhotsk Japan, +0.3 0.8 (+1.2 2.7% Sea, −4.4 0.7 (−5.1 0.9% Hudson Bay, −7.6 1.6 (−8.5 1.8% Baffin Bay/Labrador −0.5 0.3 (−5.9 3.5% Gulf St. Lawrence, −6.5 (−8.6 1.5% Greenland −13.5 2.3 (−9.2 1.6% Kara Barents Seas, −14.6 (−2.1 Ocean, −0.9 0.4 (−1.3 0.5% Canadian Archipelago. Similarly, Sea. On seasonal basis both areas, largest observed summer with next being autumn. Both area vary widely by month depending on region season. For whole, 12 months show minimum magnitude May maximum September, whereas corresponding smaller reach values March September.

Language: Английский

Citations

597

Ecological Consequences of Sea-Ice Decline DOI
Eric Post, Uma S. Bhatt, Cecilia M. Bitz

et al.

Science, Journal Year: 2013, Volume and Issue: 341(6145), P. 519 - 524

Published: Aug. 1, 2013

After a decade with nine of the lowest arctic sea-ice minima on record, including historically low minimum in 2012, we synthesize recent developments study ecological responses to decline. Sea-ice loss emerges as an important driver marine and terrestrial dynamics, influencing productivity, species interactions, population mixing, gene flow, pathogen disease transmission. Major challenges near future include assigning clearer attribution sea ice primary such especially systems, addressing pressures arising from human use coastal near-shore areas diminishes.

Language: Английский

Citations

575

The Met Office Hadley Centre sea ice and sea surface temperature data set, version 2: 1. Sea ice concentrations DOI
Holly Titchner, Nick A Rayner

Journal of Geophysical Research Atmospheres, Journal Year: 2014, Volume and Issue: 119(6), P. 2864 - 2889

Published: Jan. 4, 2014

We present a new version of the sea ice concentration component Met Office Hadley Centre and surface temperature data set, HadISST.2.1.0.0. Passive microwave are combined with historical sources, such as charts, to create global analyses on 1° grid from 1850 2007. Climatology was used when no information about available. Our main aim homogenous set by calculating applying bias adjustments using periods overlaps between different sources used. National Ice Center charts 1995 2007 have been reference achieve this. In particular, large applied passive in both Antarctic Arctic summers. Overall, HadISST.2.1.0.0 contains more than HadISST1.1, higher concentrations, shorter marginal zones, larger extents areas some regions periods. A method for estimating concentrations within pack distance edge has developed evaluated. This only were known or original fields heterogeneous. number discontinuities HadISST1.1 record longer found

Language: Английский

Citations

469

Seasonal and Regional Manifestation of Arctic Sea Ice Loss DOI Creative Commons
Ingrid H. Onarheim, Tor Eldevik, Lars H. Smedsrud

et al.

Journal of Climate, Journal Year: 2018, Volume and Issue: 31(12), P. 4917 - 4932

Published: March 27, 2018

The Arctic Ocean is currently on a fast track toward seasonally ice-free conditions. Although most attention has been the accelerating summer sea ice decline, large changes are also occurring in winter. This study assesses past, present, and possible future change regional Northern Hemisphere extent throughout year by examining concentration based observations back to 1950, including satellite record since 1979. At variability dominate perennial ice-covered Beaufort, Chukchi, East Siberian, Laptev, Kara Seas, with Siberian Sea explaining largest fraction of September loss (22%). Winter occur seas farther south: Barents Sea, Okhotsk, Greenland Baffin Bay, carrying March (27%). distinct regions winter have generally consistent but appear at present be transformation as result rapid all seasons. As become free, will dominated appears first free September. Remaining observed trends, shelf estimated 2020s, south year-round from 2050s.

Language: Английский

Citations

467

Quantifying climate feedbacks in polar regions DOI Creative Commons
Hugues Goosse, Jennifer E. Kay, Kyle C. Armour

et al.

Nature Communications, Journal Year: 2018, Volume and Issue: 9(1)

Published: May 9, 2018

The concept of feedback is key in assessing whether a perturbation to system amplified or damped by mechanisms internal the system. In polar regions, climate dynamics are controlled both radiative and non-radiative interactions between atmosphere, ocean, sea ice, ice sheets land surfaces. Precisely quantifying feedbacks required for process-oriented evaluation models, clear understanding processes responsible changes, reduction uncertainty associated with model projections. This quantification can be performed using simple consistent approach that valid wide range feedbacks, offering opportunity more systematic analyses better changes. Estimating magnitude regions. Here authors propose an inclusive methodology quantify influence all those stimulating observational ensembles.

Language: Английский

Citations

458

On the 2012 record low Arctic sea ice cover: Combined impact of preconditioning and an August storm DOI Open Access
Claire L. Parkinson, Josefino C. Comiso

Geophysical Research Letters, Journal Year: 2013, Volume and Issue: 40(7), P. 1356 - 1361

Published: March 14, 2013

Abstract A new record low Arctic sea ice extent for the satellite era, 3.4 × 10 6 km 2 , was reached on 13 September 2012; and a area, 3.0 same date. Preconditioning through decades of overall reductions made pack more vulnerable to strong storm that entered central in early August 2012. The caused separation an expanse 0.4 melted total, while its removal left main exposed wind waves, facilitating pack's further decay. Future summer storms could lead acceleration decline cover should be carefully monitored.

Language: Английский

Citations

456

A sea ice free summer Arctic within 30 years: An update from CMIP5 models DOI Open Access
Muyin Wang, James E. Overland

Geophysical Research Letters, Journal Year: 2012, Volume and Issue: 39(18)

Published: Aug. 13, 2012

Three years ago we proposed that the summer Arctic would be nearly sea ice free by 2030s; “nearly” is interpreted as extent less than 1.0 million km 2 . We consider this estimate to still valid based on projections of updated climate models (CMIP5) and observational data. Similar previous (CMIP3), CMIP5 shows a wide spread in hindcast projected loss among different models. Further, there no consensus scientific literature for cause such results CMIP3 CMIP5. While model mean extents are closer observations CMIP3, rates reduction most runs slow relative recent observations. All do show due increased anthropogenic forcing pre‐industrial control runs. Applying same technique selection extrapolation approach used our paper, interval range 14 36 years, with median value 28 years. Relative 2007 baseline, suggests 2030s.

Language: Английский

Citations

433