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Ocean-scale modelling of Calanus finmarchicus
Douglas Speirs Acknowledgments: Bill Gurney (Strathclyde) Mike Heath (FRS Aberdeen) Simon Wood (Glasgow University) SOC, PML, SAHFOS, US-GLOBEC
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Calanus finmarchicus – a marine copepod
Up to 90% of copepod biomass throughout the sub-arctic North Atlantic. Important prey species for fish in both shelf and ocean ecosystems. Extensive database from field surveys and laboratory experiments. 2 mm
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The life-cycle of Calanus finmarchicus
Omnivorous, but feeds mainly on phytoplankton. x1000 difference in body weight between eggs and adults. Stage duration strongly dependent on temperature Naupliar survival strongly dependent on food. Reproduction & growth in upper layers (<200m). Overwinters in a resting state at depths of m.
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Coupling Life-Cycle to Physical Oceanography
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Calanus abundance and Circulation
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The modelling challenge
The Challenge Physiologically and spatially explicit demographic model Ocean-basin scale – advection plus diffusion Hypothesis tests require wide parameter exploration Need exceptional computational efficiency The Solution Focus on Calanus (physical and biotic environment as given) Separate computation of physical and biological components Discrete-time approach ( 104 speed-up relative to Lagrangian ensemble)
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A Calanus-focussed model
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The Biological Model Development rate a function of temperature and food Diapause entry from end C5 Fixed fraction of each generation enter diapause Diapause exit photoperiod cued Surface mortality increases with biomass and temperature
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Yearly Population Cycle
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Continuous Plankton Recorder Surveys
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Test Data – Time Series & CPR
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Water column integrated abundance of overwintering C4 and C5 C
Water column integrated abundance of overwintering C4 and C5 C. finmarchicus C5
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Time Series Test Gulf of Maine OWS Mike surface C5-C6 diapause C5
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Diapauser Survey Test
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CPR Test observed predicted Jan./Feb. May/Jun. Jul./Aug.
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August Sea Temperature at 20m
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The Impact of Transport
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Domain Connectivity Year 1 Year 3 Year 6
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Travels of the Great Salinity Anomaly
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Conclusions Fractional diapause entry Diapause entry late in C5
Photoperiod-cued diapause exit Temperature-dependent mortality Limited impact of transport High domain connectivity Ocean-scale population model feasible Numerical efficiency is key
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Washout of a non-developing population from Gulf of Maine
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Boundary effects on C5-C6 seasonal cycle
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Gulf of Maine Export
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Invasion of Gulf of Maine
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Future Prospects Tests on independent data sets
(UK-GLOBEC Irminger Sea data) Automated parameter optimization Hindcasting of decadal trends Nested models for shelf regions Coupled target species - ecosystem models
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1958-1999 average surface abundance of C
average surface abundance of C. finmarchicus (stage C5 and CVI) 1996-onwards Calanus abundance map compiled from data supplied by SAHFOS to NERCMarine Productivity project GR2/2749 and the EU-TASC project
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Annual Mean Temperature & Food
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Overwintering depths in various regions...
C5
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Geographical focus of Marine Productivity and other Calanus-centric programmes during the 1990’s..
Multi-national programmes: EU-ICOS EU-TASC National programmes: UK, Norway, Germany, Denmark, Iceland, Canada, USA NERC Marine Productivity Calanus abundance map compiled from data supplied by SAHFOS to NERCMarine Productivity project GR2/2749 and the EU-TASC project
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C5’s & phytoplankton carbon at OWSM
Diapause occurs at end of C5 stage Fixed fraction of each generation
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