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Biological Time Series Observations in the Pacific Arctic Region. Jacqueline M. Grebmeier 1 and Sue E. Moore 2 1 Chesapeake Biological Laboratory, University of Maryland Center for Environmental Science (UMCES), Solomons, Maryland, USA 2 NOAA/Science & Technology, PMEL, Seattle, WA, USA.
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Biological Time Series Observations in the Pacific Arctic Region Jacqueline M. Grebmeier1 and Sue E. Moore2 1Chesapeake Biological Laboratory, University of Maryland Center for Environmental Science (UMCES), Solomons, Maryland, USA 2NOAA/Science & Technology, PMEL, Seattle, WA, USA 20 May 2009 “NOAA Day on the Hill” Cannon Senate Building Washington, DC
Talk Outline Ecosystem studies in the Pacific-influenced Arctic waters Case studies as indicators of biological change Development of “Distributed Biological Observatory” concept to track ecosystem change with climate warming in the Arctic
Rich benthic communities on the western side of the Bering/Chukchi Sea system • carbon export through the water column to the benthos supports a rich benthic infaunal system in the the Bering and Chukchi ecosystem • “foot prints” of high benthic biomass on the shallow continental shelves regions are areas of high pelagic-benthic coupling and export of carbon to sediments [Grebmeier et al. 2006]
MARINE MAMMALS & SEA ICEMoore and Huntington. 2008. Ecological Applications
Gray Whales as Ecosystem Sentinels:‘Weight of Evidence’ • One-week delay in southbound migration timing, coincident with NPAC regime shift (Rugh et al. 2001) • Calving rates positively correlated with ice-free Chirikov Basin (Perryman et al. 2002) • Absence of feeding GW in Chirikov Basin,coincident with decline in benthic infauna (Moore et al. 2003) • Feeding whales year-round near Kodiak(Moore et al. 2007) • Calls detected year-round near Barrow(Stafford et al.2007) • Shorter residency in breeding lagoons (Urban & Swartz 2008*) Moore. 2008. J. of Mammalogy
Chirikov Basin, Northern Bering Sea in the 1980s • high amphipod populations in sediments • large population of migrating gray whales suction up mud to feed on benthic amphipods Gray whale sightings [movie]
Time-series sites Chirikov Basin: Drop in Benthic Productivity in 1990s • Highsmith and Coyle (1992) report evidence of 30% amphipod production downturn from 1986-88 • decline of ampeliscid amphipod biomass at 4 time series stations (Moore et al. 2003); subsequently supported at more stations in the region (Coyle et al. 2007) • LeBoeuf et al. 2002 suggest this amphipod decline in the Chirikov Basin as causal to gray whale mortalities • Shift gray whales north of Bering Strait; normally prefer feeding in ice-free areas
Salmon & pollock migration moving northward with seawater warming [Moss et al. 2009] [courtesy Jack Helle/NOAA] Pink salmon Pollock • NOAA Bering-Aleutian Salmon International Survey (BASIS)survey 2007: pink and chum salmon in Chukchi Sea with warming seawater • increased sea water temperature positive influence on growth rates • 2007 maximum sea ice retreat on record; increase open water habitat • 2000 to 2004 increased surface seawater temperature northward • influenced northward migration of pink salmon and pollock
RUSALCA (Russian-American Long-term Census of the Arctic) and C30 (Canada’s Three Oceans) working in Pacific sector of Arctic C3O RUSALCA 2009
Distributed Biological Observatory Concept • Based on two recent NOAA lead and co-sponsored workshops: • 6-8 May 2009 “Biological Response to Sea Ice Reduction in the Pacific Arctic Region”, PMEL/NOAA, Seattle, WA • 13-15 May 2009 “Bering Strait Observations Workshop”, University of Washington Center for Sustainable Forestry (Pack Forest), Eatonville, WA • recommend 3 distributed biological observatory regions for standard measurements and focused time-series studies as part of a national and international network • NOAA continuing contributions to biological observations within US SEARCH (Study of Environmental Arctic Change) program, specifically RUSALCA)
Passive Acoustic ObservatoriesviaLong-term recorders since 1999 2006
Call Detection Rate(s) & Seasonal Surprises Gulf of Alaska Blue whale – blue Fin whale - red Sperm whale - green W. Beaufort Sea Gray whale – calls detected over-winter [Stafford et al. 2007a&b]
Bering Strait Environmental Observatory: Passive Acoustics • Provide real-time call detections to local people, educators & scientists • Track phenology of arctic and sub-arctic marine mammals in ecosystem context • Measure noise from natural and anthropogenic sources Fin whale Killer whale Gray whale