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Hi @jbarr444, Multiplicity is unitless, it conveys the number of particles represented by a super droplet. We compute the surface flux only for the particles that cross the bottom boundary of the domain, not for all the particles in the bottom cell, the relevant code is here: Then, it is summed and normalised wrt area of the column base here:As noted in #708, we are actually missing unit tests for the above code, help welcome! |
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Hi @slayoo,
Can you explain how PySDM calculates surface precipitation in the 1D environment? I'm trying to split the precipitation into contributions from radius bins, but the total is ending up anywhere within one order of magnitude off from what the 'surface precipitation' product reports. I'm simply summing up 4/3 * pi * r**3 * multiplicity * v(r) / dz in the 0 height bin. v(r) is stokes drag and I'm assuming multiplicity has units # per unit area (?) I also tried summing the volume of particles that are less than height v(r)*dt, then dividing by dt, but that does similarly.
Thanks,
Jason
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