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Lewis, C. V. W. (Dartmouth), D. R. Lynch (Dartmouth), M. J. Fogarty (Chesapeake Biological Laboratory), and D. Mountain (NMFS - Woods Hole)
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| Tar file of sample source. <\td><\tr> |
Simulation |
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General Information
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(2/18/99) Population modelling (ASLO Results):
Idealized model with following parameters:
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| (2/18/99) Sources and Sinks (ASLO Results): Larvae were initiated on September 1 throughout the model domain and transported for 40 days in the top 25 meter flow. The distribution of the source and settlement regions were calculated as the percentage of the individuals at a given location that either originated from (settlement) or settled in (source) a given closed area. This can also be thought of as the probability that an adult at a given location originated from the closed area (sink map) and the probability that a larvae from a given region will settle into a given closed area (source map). |
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| (12/1/98) Top 25 meter Flow: Larvae spawn on September 1 and travel for 40 days, with no dispersion. Larvae in water deeper than 200 m are killed. This cycle is repeated for 10 years. |
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| (12/1/98) Top 25 meter Flow: Larvae spawn on September 1 and travel for 40 days, with a 10 cm/s velocity variance. Larvae in water deeper than 200 m are killed. This cycle is repeated for 10 years. |
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| (5/7/98) Depth averaged Flow: Particles are seeded within each of the regions every 60 days (simulating spawning on Jan. 1, Mar. 1, May 1, Jul. 1, Sep. 1, and Nov. 1) and allowed to diffuse (dispersal velocity variance =10 cm/s)and advect for 60 days. The particles are released in a two-dimensional flowfield consisting of the average horizontal velocity over the entire water column |
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(5/7/98) Top 25 meter Flow: Particles are seeded within each of
the regions every 60 days (Jan. 1, Mar. 1, May 1, Jul. 1, Sep. 1, and
Nov. 1) and allowed to diffuse (dispersal velocity variance = 10 cm/s)
and advect for 60 days. The particles are released in a
two-dimensional flowfield consisting of the average horizontal
velocity over the top 25 meters of the water column, and is thus
subject to the faster surface currents as well as notable surface
convergence and divergence.
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