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

Recent Arctic amplification and extreme mid-latitude weather DOI

Judah Cohen,

James A. Screen, Jason C. Furtado

et al.

Nature Geoscience, Journal Year: 2014, Volume and Issue: 7(9), P. 627 - 637

Published: Aug. 17, 2014

Language: Английский

Citations

2197

Evidence linking Arctic amplification to extreme weather in mid‐latitudes DOI Open Access
Jennifer A. Francis,

Stephen J. Vavrus

Geophysical Research Letters, Journal Year: 2012, Volume and Issue: 39(6)

Published: Feb. 23, 2012

Arctic amplification (AA) – the observed enhanced warming in high northern latitudes relative to hemisphere is evident lower‐tropospheric temperatures and 1000‐to‐500 hPa thicknesses. Daily fields of 500 heights from National Centers for Environmental Prediction Reanalysis are analyzed over N. America Atlantic assess changes north‐south (Rossby) wave characteristics associated with AA relaxation poleward thickness gradients. Two effects identified that each contribute a slower eastward progression Rossby waves upper‐level flow: 1) weakened zonal winds, 2) increased amplitude. These particularly autumn winter consistent sea‐ice loss, but also apparent summer, possibly related earlier snow melt on high‐latitude land. Slower would cause weather patterns mid‐latitudes be more persistent, which may lead an probability extreme events result prolonged conditions, such as drought, flooding, cold spells, heat waves.

Language: Английский

Citations

1652

Trends in Arctic sea ice extent from CMIP5, CMIP3 and observations DOI
Julienne Strœve, V. M. Kattsov, A. P. Barrett

et al.

Geophysical Research Letters, Journal Year: 2012, Volume and Issue: 39(16)

Published: July 26, 2012

The rapid retreat and thinning of the Arctic sea ice cover over past several decades is one most striking manifestations global climate change. Previous research revealed that observed downward trend in September extent exceeded simulated trends from models participating World Climate Research Programme Coupled Model Intercomparison Project Phase 3 (CMIP3). We show here as a group, contributing to CMIP5 are more consistent with observations satellite era (1979–2011). Trends ensemble members nevertheless remain smaller than value. Pointing strong impacts internal variability, 16% member statistically indistinguishable zero. Results do not appear have appreciably reduced uncertainty when seasonally ice‐free Ocean will be realized.

Language: Английский

Citations

1085

The Norwegian Earth System Model, NorESM1-M – Part 1: Description and basic evaluation of the physical climate DOI Creative Commons
Mats Bentsen, Ingo Bethke,

Jens Boldingh Debernard

et al.

Geoscientific model development, Journal Year: 2013, Volume and Issue: 6(3), P. 687 - 720

Published: May 24, 2013

Abstract. The core version of the Norwegian Climate Center's Earth System Model, named NorESM1-M, is presented. NorESM family models are based on Community Model 4 (CCSM4) University Corporation for Atmospheric Research, but differs from latter by, in particular, an isopycnic coordinate ocean model and advanced chemistry–aerosol–cloud–radiation interaction schemes. NorESM1-M has a horizontal resolution approximately 2° atmosphere land components 1° ice components. also available lower (NorESM1-L) that includes prognostic biogeochemical cycling (NorESM1-ME). two configurations not part this paper. Here, first-order assessment stability, mean state internal variability experiments made to CMIP5 Further analysis performance provided accompanying paper (Iversen et al., 2013), presenting corresponding climate response scenario projections with NorESM1-M.

Language: Английский

Citations

983

Global warming releases microplastic legacy frozen in Arctic Sea ice DOI Creative Commons
R. W. Obbard,

Saeed Sadri,

Ying Qi Wong

et al.

Earth s Future, Journal Year: 2014, Volume and Issue: 2(6), P. 315 - 320

Published: May 20, 2014

Abstract When sea ice forms it scavenges and concentrates particulates from the water column, which then become trapped until melts. In recent years, melting has led to record lows in Arctic Sea extent, most September 2012. Global climate models, such as that of Gregory et al. (2002), suggest decline volume (3.4% per decade) will actually exceed something Laxon (2013) have shown supported by satellite data. The extent could release anthropogenic back open ocean not yet been examined. Here we show remote locations contains concentrations microplastics are several orders magnitude greater than those previously reported highly contaminated surface waters, Pacific Gyre. Our findings indicate accumulated far population centers polar represents a major historic global sink man‐made particulates. potential for substantial quantities legacy microplastic contamination be released melts therefore needs evaluated, do physical toxicological effects plastics on marine life.

Language: Английский

Citations

962

The HadGEM2 family of Met Office Unified Model climate configurations DOI Creative Commons
Nicolas Bellouin, W. J. Collins, I. D. Culverwell

et al.

Geoscientific model development, Journal Year: 2011, Volume and Issue: 4(3), P. 723 - 757

Published: Sept. 7, 2011

Abstract. We describe the HadGEM2 family of climate configurations Met Office Unified Model, MetUM. The concept a model "family" comprises range specific incorporating different levels complexity but with common physical framework. includes atmosphere and ocean components, without vertical extension to include well-resolved stratosphere, an Earth-System (ES) component which dynamic vegetation, biology atmospheric chemistry. improvements designed address systematic errors encountered in previous configuration, HadGEM1, namely Northern Hemisphere continental temperature biases tropical sea surface poor variability. Targeting these was crucial order that ES configuration could represent important biogeochemical feedbacks. Detailed descriptions evaluations particular members are included number other publications, discussion here is limited summary overall performance using set metrics compare way various simulate present-day its

Language: Английский

Citations

939

Changing state of Arctic sea ice across all seasons DOI Creative Commons
Julienne Strœve, Dirk Notz

Environmental Research Letters, Journal Year: 2018, Volume and Issue: 13(10), P. 103001 - 103001

Published: Sept. 3, 2018

The decline in the floating sea ice cover Arctic is one of most striking manifestations climate change. In this review, we examine ongoing loss across all seasons. Our analysis based on satellite retrievals, atmospheric reanalysis, climate-model simulations and a literature review. We find that relative to 1981–2010 reference period, recent anomalies spring winter coverage have been more significant than any observed drop summer extent (SIE) throughout period. For example, SIE May November 2016 was almost four standard deviations below these months. Decadal during months has accelerated from −2.4 %/decade 1979 1999 −3.4%/decade 2000 onwards. also regional for given region, seasonal larger closer region outer edge cover. Finally, months, identify robust linear relationship between pan-Arctic total anthropogenic CO2 emissions. annual cycle per ton emissions ranges slightly above 1 m2 3 summer. Based extrapolation trends, Ocean will become sea-ice free August September an additional 800 ± 300 Gt emissions, while it becomes July October 1400

Language: Английский

Citations

923

Arctic sea ice is an important temporal sink and means of transport for microplastic DOI Creative Commons
Ilka Peeken, Sebastian Primpke,

Birte Beyer

et al.

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

Published: April 11, 2018

Microplastics (MP) are recognized as a growing environmental hazard and have been identified far the remote Polar Regions, with particularly high concentrations of microplastics in sea ice. Little is known regarding horizontal variability MP within ice how underlying water body affects composition during growth. Here we show that has no uniform polymer that, depending on growth region drift paths ice, unique patterns can be observed different horizons. Thus even regions such Arctic Ocean, certain indicate presence localized sources. Increasing exploitation resources will likely lead to higher load enhance release areas strong seasonal melt outflow gateways.

Language: Английский

Citations

908

Climate policy implications of nonlinear decline of Arctic land permafrost and other cryosphere elements DOI Creative Commons
Dmitry Yumashev, Chris Hope, Kevin Schaefer

et al.

Nature Communications, Journal Year: 2019, Volume and Issue: 10(1)

Published: April 23, 2019

Arctic feedbacks accelerate climate change through carbon releases from thawing permafrost and higher solar absorption reductions in the surface albedo, following loss of sea ice land snow. Here, we include dynamic emulators complex physical models integrated assessment model PAGE-ICE to explore nonlinear transitions their subsequent impacts on global economy under Paris Agreement scenarios. The feedback is increasingly positive warmer climates, while albedo weakens as snow melt. Combined, these two factors lead significant increases mean discounted economic effect change: +4.0% ($24.8 trillion) 1.5 °C scenario, +5.5% ($33.8 2 +4.8% ($66.9 mitigation levels consistent with current national pledges. Considering makes target marginally more economically attractive than target, although both are statistically equivalent.

Language: Английский

Citations

813

Antarctic sea ice variability and trends, 1979–2010 DOI Creative Commons
Claire L. Parkinson,

D. J. Cavalieri

˜The œcryosphere, Journal Year: 2012, Volume and Issue: 6(4), P. 871 - 880

Published: Aug. 15, 2012

Abstract. In sharp contrast to the decreasing sea ice coverage of Arctic, in Antarctic cover has, on average, expanded since late 1970s. More specifically, satellite passive-microwave data for period November 1978–December 2010 reveal an overall positive trend extents 17 100 ± 2300 km2 yr−1. Much increase, at 13 700 1500 yr−1, has occurred region Ross Sea, with lesser contributions from Weddell Sea and Indian Ocean. One region, that Bellingshausen/Amundsen Seas, (like Arctic) instead experienced significant decreases, extent −8200 1200 When examined through annual cycle over 32-yr 1979–2010, Southern Hemisphere as a whole trends every month, ranging magnitude low 9100 6300 yr−1 February high 24 10 000 May. The Ocean also had each while Seas negative western Pacific mixture trends. Comparing ice-area results ice-extent results, case same sign trend, but magnitudes two differ, some cases these differences allow inferences about corresponding changes concentrations. strong pattern increasing is suggestive atmospheric circulation. This key topic future research.

Language: Английский

Citations

806