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simone-silvestri avatar simone-silvestri commented on July 28, 2024

I decided to use a piecewise cubic function for the wind stress (and salinity flux). I guess we could use a parabolic one also

from oceanscalingtests.jl.

navidcy avatar navidcy commented on July 28, 2024

Is it constant values in between?

from oceanscalingtests.jl.

glwagner avatar glwagner commented on July 28, 2024

How about

τ₀ * (cos(3π * φ/Δφ) - exp(-φ^2 / 2Δφₑ^2))

?

from oceanscalingtests.jl.

navidcy avatar navidcy commented on July 28, 2024

I think that should work. Perhaps we should ensure that wind stress goes to zero at the North-South latitudinal boundaries otherwise you get Kelvin waves and circulation at the boundaries.

from oceanscalingtests.jl.

glwagner avatar glwagner commented on July 28, 2024

Ah nice. Then Δφ is the total latitudinal extent of the domain. Δφₑ is the width of the equatorial bump, typically about 10 degrees latitude. We can also add a parameter to express the relative magnitude of the equatorial bump.

from oceanscalingtests.jl.

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