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Modeling secondary production in the Norwegian Sea with a fully

coupled model system

Solfrid Sætre Hjøllo, Geir Huse and Morten Skogen

ICES Annual Science Conference.

Nantes, France, September 2010 Paper L:09

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• Background and motivation

• Coupled model system

• Model upset and parameterizations

• Trophic coupling and impacts of various drivers

• Summary and future plans –towards

NORWECOM.E2E

(3)

Need: an integrated system of models that describe the

ecosystem function with focus on processes of importance to harvestable stocks

From Skjoldal et al. 2004

(4)

Coupled model system

OCEAN MODEL

C. FINMARCHICUS IBM

Phytoplankton distribution Predator field

3D field of current, temperature, turbulence PHYTO-

PLANKTON MODEL NORWECOM

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DIA FLA NIT

PHO SiS SIL

DETN DETP

SIL

PHO

NIT OXY

OXY OXY

O

2

OXY Stress

Stress

BURIED

DETP N2

DETN

DETN DETP

SIL SiS NIT PHO

NORWECOM

Skogen & Søiland (1998), Skogen et al (2007)

Prognostic variables: Primary production (diatoms, flagellates),

nutrients (inorganic nitrogen, phosphorus,

silicate), oxygen, detrituis, biogenic silicia,

light in water column, suspended matter

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DIA FLA NIT

PHO SiS SIL

DETN DETP

SIL

PHO

NIT OXY

OXY OXY

O

2

OXY Stress

Stress

BURIED

DETP N2

DETN

DETN DETP

SIL SiS NIT PHO

NORWECOM

Skogen & Søiland (1998), Skogen et al (2007)

Forcing by: light, temperature, nutrients

(river+atmosphere), algae death

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DIA FLA NIT

PHO SiS SIL

DETN DETP

SIL

PHO

NIT OXY

OXY OXY

O

2

OXY Stress

Stress

BURIED

DETP N2

DETN

DETN DETP

SIL SiS NIT PHO

NORWECOM

Skogen & Søiland (1998), Skogen et al (2007)

Processes included: respiration,

regeneration of nutrients, self shading,

turbidity, sedimentation, resuspension,

denitrification, detritus (N and P) and

diatom skeletals (Si), oxygen

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Individual-based model (IBM) Calanus-model

From http://pulse.unh.edu/

Feeding: functional response, type 2 (Campbell 2001)

Growth: bioenergetics (Carlotti &

Wolf 1998)

Reproduction: mature adults above weight and fat thresholds, in mixed layer

Vertical movement: dvm, annual cycle

Horizontal movement: by currents

Structural weight Fat content 3D Position Stage

Individual number

WUD AFD

OWD

VM1W +VM2 if C5 before AFD=> mature

else allocate to fat

if fat/soma > FSRdescend to OWD

Time Depth

..

Huse et al (in prep)

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Calanus mortality

1. Geographical limitations (Nordic Seas)

2. Stage specific weight limitations (i.e.starvation)

3. Age and spawning stress limitations (< 400 days and <800 eggs) 4. Invertebrate predation parameterized (not year specific)

1. day/night dependent

2. geographically uniform & exponentially decying in upper 1000m

5. Predation from pelagic fish parameterized (not year specific)

1. preysize and daylight dependent

2. geographically uniform & restricted to upper 600m

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Model upset

• Physical forcing for year 1997

• NORWECOM initialization

• Typical winter values of Atlantic water for nutrients (12.0,5,5 and 0.8 uM inorganic nitrogen,silicate and phosphoros)

• Small amounts of algae (0.10mgNm-3)

• 200 mgN/m2/year added from the atmosphere

• CALANUS initialization

• 50.000 super individuals with influence ratio of 4 gridcells

• ”Standard” initial C. Finmarchicus distribution

• ~1011 C5 individuals distributed on 50.000 super individuals

• Strctural weight 80µg, fat level 40µg; total mass: 17 mill tonn C

• Overwintering depth 300-1100m

• Diapause termination : Feb 10 –April 9

1000 ind m-2

”Standard” initial C5 distribution from test run

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Model performance

Initial no of calanus

(overwintering C5) 100*fold increased, slightly elevated at end of simulation

Biomass ~stable

No of super-individuals

elevated; increased computer time 

C5 nauplii copepodites

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Calanus Finmarchicus copepodite abundance

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Initial: 0-100.000 ind/m2

Apr-July: peak values of 400.000 ind m-2, 40.000 ind m-2 C6

Overwintering population: 0-100.000 ind m-2, in Atlantic Water zone

Mid April - Mid-July

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Geographical distribution of a) annual production and b) mean of daily top to bottom biomass. Unit is [gC/m2]. Below panels the same quantities integrated within the Norwegian Sea.

PB ratio:

Annual production/mean summer biomass = 6.3

Biomass:

~10 gC m-2

Norw Sea: 8 mill tonnes C Observed estimate

Skjoldal et al (2004) : 7 mill tonnes C

Production:

~60 gCm-2

Norw Sea: 34 mill tonnes C

Observed estimate Skjoldal et al (2004) : 42 mill tonnes C,

assuming PB-ratio of 6

(15)

Trophic coupling through Calanus mortality

Geographical limitations Starvation

Age and spawning stress Invertebrate predation

Fish

(16)

Diapause termination

WUD early:

production weakly increased in Atlantic Water zone/coastal waters;

otherwise reduced.

Biomass increase in Atlantic Water zone, reduced elsewhere.

WUD late:

production decreased in coastal waters, increased elsewhere

Biomass reduced in coastal/Atlantic Water zone, increased elsewhere WUD light dependent:

production pattern as for WUD early

Biomass weakly increased in

northern coastal/Atlantic Water zone, decreased elsewhere

EARLY LATE MIXED

- 12% +3% - 11%

+2% - 5% - 4%

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Summary

• Coupled model system for the Norwegian Sea implemented and running

• ~50.000 calanus super-individuals sufficient

• Stable biomass development; multi-year simulations possible

• Two way coupling between different trophic levels

• Stock collapse due to food limitations within one year possible

• Diapause termination changes production more & different than biomass

• Towards end-to-end modelling:

NORWECOM.E2E is a suitable model tool to study ecosystem dynamics

• Flexible module system allows easy inclusion of new species

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NORWECOM.E2E future plans

OCEAN MODEL ROMS

PHYTOPLANKTON MODEL

NORWECOM

C. Finmarchicus C. Glacialis

C. Hypoboreus C. Helgolandicus Krill

Phytoplankton distribution

Herring, blue whiting, mackerel

Mesopelagic fish and Gonatus

Marine mammals Fish larvea...

Zooplankton distribution Predator field

Predator field

3D field of current, temperature, turbulence

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NORWECOM.E2E future plans

OCEAN MODEL ROMS

PHYTOPLANKTON MODEL

NORWECOM

C. Finmarchicus C. Glacialis

C. Hypoboreus C. Helgolandicus Krill

Phytoplankton distribution

Herring, blue whiting, mackerel

Mesopelagic fish and Gonatus

Marine mammals Fish larvea...

Zooplankton distribution Predator field

Predator field

3D field of current, temperature, turbulence

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