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#advection

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Convection–diffusion equation
The convection-diffusion equation is a more general version of the scalar transport equation. It is a combination of the diffusion and convection (advection) equations. It describes physical phenomena where particles, energy, or other physical quantities are transferred inside a physical system due to two processes: diffusion and convection.
ct=(Dcvc)+R

ct=(Dc)diffusion(vc)advectionconvection+Rdestructioncreation

(Dc) is the contribution of diffusion.
(vc) is the contribution of convection or advection.
R describes the creation or destruction of the quantity.

where
c is the variable of interest.
D is the diffusivity.
v is the velocity field, and
R is the sources or sinks of the quantity c.

Our new paper on modelling the #spatiotemporal dynamics of a beneficial genetic variant is out @eLife.
Muktupavela et al: elifesciences.org/articles/737
Plus a digest highlight here: elifesciences.org/digests/7376

We extend a #diffusion method for inferring the spread of a strongly selected allele, originally developed by Novembre et al. (journals.plos.org/plosbiology/). We now incorporate #ancientDNA and allow for #advection dynamics.

Continued thread

@MPI_Meteo

The most computationally expensive part of such models is the transport (by #advection and #diffusion) of #biogeochemical #tracers (zoo and #phytoplankton #nutrients, organic and inorganic #carbon, etc) with the #ocean #flow.

The more tracers we include to represent the complexity of #ocean biogeochemistry, the slower are the model runs. Same problem arises when the #spatial #resolution of an #ESM increases.

Biogeochemistry models can become a bottleneck in #ESM computations. 2/