Research Article Eulerian-Eulerian Simulation of Particle ...
Effect of eddy transport and blocking on migration …...swimming ability Simple box%ocean ! ...
Transcript of Effect of eddy transport and blocking on migration …...swimming ability Simple box%ocean ! ...
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Sachihiko ITOH and Takashige SUGIMOTO
Effect of eddy transport and blocking on migration
of small pelagic fishes
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Subtropical and subarctic gyres
!a" SST #°C$
!b" SSS #psu.$
!c" Dynamic height !2000%db" #m$
!d" Sea surface chlorophyll #µg/l$
!Data from World Ocean Atlas 2001"
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Meridional migration of pelagic fishes in the Western North Pacific
Spawning area!Over%wintering" Feeding area
Upper%layer oceanic/fishery condition
Kuroshio region
Oyashio region
Southern coastal area
Northern coastal area
Kuroshio%OyashioTransition region
25N
35N
30N
40N
50N
45N
130E 140E 150E 160E 170E sardine
anchovy
mackerels
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Pelagic fishes in the Transition Region
SardineImportance of juvenile mortality !Watanabe et al. 1995" Temperature criticality!Noto and Yasuda, 1999"
Kuroshio Extensio! hypothesis
Anchovy Faster growth more survival!Takahashi, 2001"
Mackerels Largest young fish abundance in frontal areas !Kuroda et al, 1997"
Importance of fronts
Importance of migration phaseSchool concentration at fronts
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Eddies and fronts for small pelagic fishes
High productivity and plankton convergence !Uda, 1960"Blocking migration !Uda, 1960"Transport/diffusion/retention
Modeling approach of this studyExamine basic processes of eddies and fronts on the northward migration of fishes with small swimming abilitySimple box%ocean ! <=> realistic simulation"Migratory eulerian tracer
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Wind%driven double%gyre ocean circulation model
2000%km x 2000%km closed flat domain
Idealized wind stress and heating/cooling amplitudes
360%days period forcing!begins from spring"
Physical model
Schematic diagram of model domain
2000m
0m
2000km
2000km
logarithmic 9 levels
zonally homogeneouswind stress amplitude
10km x 10km grid
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Direction northward
Speed limited by temperature gradient
Migratory eulerian tracer
†
∂N∂t
=
†
-u∂N∂x
- v ∂N∂y
- w ∂N∂z
†
+ AH∂ 2N∂x 2 +
∂ 2N∂y 2
Ê
Ë Á
ˆ
¯ ˜
†
- umig∂N∂x
- vmig∂N∂y
tendency physical advection physical diffusion migration
†
umig = 0, vmig £ 0.1 m/s
†
¢ T y +vmigDt - ¢ T £ aDt
†
a = 0.05 [°C/day]
Migration
†
umig, vmig( )
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Tracer input
at the beginningof the seasonal cycle !Spring"in 30m depth, 17°C latitude along the western boundary
Three sets of 100 days calculation
Settings and cases
30m temp. at Day 0 of the 1st year
(a) Standard
(b) Windy winter (c) Calm winter
0km
1000
1000
-1000
-1000
0km
0km 1000 20000km 1000 2000
0
1
2
Day 0, 100
SpringS F W SS S F W
(b)(a)
(c)
Heating/coolingamplitude
Wind stressamplitude
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Basic cases
Standard -500
500
0km
0km 500 0km 500 0km 500 0km 500 0km 500
No migration !Passive" -500
500
0km
0km 500 0km 500 0km 500 0km 500 0km 500
No blocking !constantmigration" -500
500
0km
0km 500 0km 500 0km 500 0km 500 0km 500
Day 20 Day 40 Day 60 Day 80 Day 100
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Change of wind in winter
1st year 2nd year 3rd year
Windy winter
Constant wind stress amplitude
! Standard "
Calm winter
0 km
-500
500
0 km 1000
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Average movement and temperature history
-500km
-250km
0km
250km
0km 250km 500km 750km
BasicWindy winterCalm winter
0km 250km 500km 750km
BasicWindy winterCalm winter
0km 250km 500km 750km
BasicWindy winterCalm winter
Day 0
Day 10Day 50
Day 100
Day 0
Day 10 Day 50
Day 100
Day 10
Day 50
Day 100Average movement
1st year 2nd year 3rd year
-1.5
-1.0
-0.5
0°C
0 days 20 40 60 80 100
Std. 1
Std. 2Std. 3
Wnd. 1Wnd. 2Wnd. 3
Clm. 1Clm. 2
Clm. 3
Average environmentaltemperature history
km
[°C]
Std. 1
Std. 2
Std. 3
Wnd. 1Wnd. 2
Wnd. 3
Clm. 1
Clm. 2Clm. 3
Average temperature filed
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Latitudinally different waters and migration strategy
!c" !d"
SSC #µg/l$ climatology !World Ocean Atlas 2001"
SST #°C$ snapshots by a simulation!Earth simulator center"
!a" !b"
Dynamic confluence
Shelf break
Cross-gyre migration
Along-shoremigration
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Eddy transport and blocking of migratory tracer
Concentration at the ridge of water intrusions
Influences of warm eddy activity to the migration path and temperature history
Meridional migration in the W.N.Pacific
Required to sustain large population
Utilizing eddy%intruding dynamic confluence
Summary
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Thank you
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Parameters examination
Cases X ± s.d. !km" Y ± s.d. !km" T ± s.d. !°C"
Standard 580 ± 243 571 ± 292 %1.3 ± 3.6
Vmig ≤ 0.20 m/s 605 ± 225 758 ± 373 %1.8 ± 3.4
Vmig ≤ 0.05 m/s 390 ± 159 378 ± 186 %0.4 ± 3.6
a = 0.10 °C 580 ± 216 768 ± 294 %1.8 ± 3.6
a = 0.025 °C 513 ± 266 436 ± 265 %0.6 ± 3.5
No heating 582 ± 249 545 ± 275 %3.2 ± 2.8
Average distance and increase/decrease of environmental temperature of tracer at Day 100 from the initial