Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

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Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea Andrew J. Pershing University of Maine/ Gulf of Maine Research Institute Charles H. Greene Cornell University

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Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea. Andrew J. Pershing University of Maine/ Gulf of Maine Research Institute. Charles H. Greene Cornell University. Collaborators. Outline. Project goals Results Future plans. Goals. - PowerPoint PPT Presentation

Transcript of Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Page 1: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Andrew J. PershingUniversity of Maine/

Gulf of Maine Research Institute

Charles H. GreeneCornell University

Page 2: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Collaborators

Ted Durbin URICharles Flagg SUNY Stony BrookSirpa Häkkinen NASA GoddardErica Head BIODave Mountain NEFSCPeter Smith BIO

Page 3: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Outline

• Project goals• Results• Future plans

Page 4: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Goals

• Characterize interannual variability in physical and biological conditions in GOM/GB– Retrospective approach

• Identify drivers of variability– Focus on remote climate forcing

• Compare GOM with nearby regions– Scotian Shelf, MAB

Page 5: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Gulf of Maine Regime ShiftAutumn Phytoplankton

Small Copepods

Herring

• Hallmarks– Abrupt shift in 1990,

reversal in 2001– Multiple trophic

levels– Strongest in autumn

Page 6: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Possible Mechanism

Reduced surface salinity

Bigger fall bloom

Increased copepodreproduction

(e.g. Durbin et al. 2003*)

Surface Salinity

Autumn Phytoplankton

*MEPS 254:81-100

Page 7: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Salinity and Fall Stratification

• 1D Mixing Model• Salty (1986) and

Fresh (1998) initial TS-profiles

• 1980-1999 NCEP forcing

Page 8: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Possible Mechanism

Page 9: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Impact of ShiftSmall Copepods Calanus

finmarchicus

• Increase in small copepods, including Calanus copepodites• Decrease in adult Calanus

Page 10: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Impact of ShiftSmall Copepods Calanus

finmarchicus

Herring Right Whale Calves

Page 11: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Impact of Shift

Page 12: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Herring-Copepod Interactions

• Fall-winter: larval herring– Inefficient feeding

• Summer: adults– Efficient feeding

Page 13: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

PhytoplanktonFreshwater

Page 14: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

PhytoplanktonFreshwater

Page 15: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Discussion

• Importance of fall-winter period– Spring has dominated research

(e.g. GLOBEC) in NW Atlantic• Spring bloom, spawning of cod

and haddock– CPR data suggests that there is

considerable variability in fall• Fall ecosystem changes can

persist throughout the year

Fall phytoplankton

Haddock recruitment

Page 16: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

1990s Freshening

1990-1994 1995-1999

Salinity Change in the N. Atlantic

Figure courtesy of Tim Boyer, NOAA

• Gulf of Maine freshening part of larger pattern extending into Labrador Sea– Non-local processes can influence Gulf of Maine

Page 17: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

1990s Freshening

• Freshwater in early 1990s traced to Arctic– NAO+ winds in late 1980s pushed

Arctic ice out– Increased outflow through

Canadian Archipelago

Page 18: Marine Ecosystem Responses to Climate-Associated Remote Forcing from the Labrador Sea

Future Work

• CAFÉ Gulf of Maine Workshop III– Theme: Arctic Influences on NW Atlantic Shelf Ecosystems– November 7-8, GMRI, Portland, ME

• Compare Gulf of Maine with Mid-Atlantic Bight– Oleander CPR data set