Pangolin v1.0, a conservative 2-D advection model towards large-scale parallel calculation

0Citations
Citations of this article
5Readers
Mendeley users who have this article in their library.

Abstract

To exploit the possibilities of parallel computers, we designed a large-scale bidimensional atmospheric advection model named Pangolin. As the basis for a future chemistry-transport model, a finite-volume approach for advection was chosen to ensure mass preservation and to ease parallelization. To overcome the pole restriction on time steps for a regular latitude-longitude grid, Pangolin uses a quasi-area-preserving reduced latitude-longitude grid. The features of the regular grid are exploited to reduce the memory footprint and enable effective parallel performances. In addition, a custom domain decomposition algorithm is presented. To assess the validity of the advection scheme, its results are compared with state-of-the-art models on algebraic test cases. Finally, parallel performances are shown in terms of strong scaling and confirm the efficient scalability up to a few hundred cores.

Figures

  • Figure 1. Van Leer scheme for positive (left) and negative (right) winds. The distribution of the tracer is shown as a linear distribution (broken line). The grey area is the quantity of tracer passing through the interface during a time step.
  • Figure 2. Grid used in Pangolin with 20 latitudes: orthographic projection (left) and Robinson projection, with the six identical zones highlighted (right).
  • Figure 4. Discretization for zonal and meridional winds (u and v, respectively) and tracer mixing ratio q.
  • Figure 3. Number of cells for the grid used by Pangolin on one hemisphere with 90 latitudes (solid line). The truncated and “exact” version are shown as dotted and dashed lines, respectively. {
  • Figure 5. Meridional interfaces (bold lines) and fluxes (arrows) for cell (i,j).
  • Table 1. For a given resolution at the Equator, we compare the total number of cells of each model nmodel vs. the total number of cells of Pangolin npangolin.
  • Figure 6. Zonal interpolation to compute the meridional gradient of q ′ ij .
  • Table 2. Summary of the models used as a comparison: name, implementation grid, the total number of cells vs. Pangolin, and the time scheme.

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Cite

CITATION STYLE

APA

Praga, A., Cariolle, D., & Giraud, L. (2015). Pangolin v1.0, a conservative 2-D advection model towards large-scale parallel calculation. Geoscientific Model Development, 8(2), 205–220. https://doi.org/10.5194/gmd-8-205-2015

Readers over time

‘15‘19‘2200.751.52.253

Readers' Seniority

Tooltip

PhD / Post grad / Masters / Doc 3

60%

Researcher 2

40%

Readers' Discipline

Tooltip

Earth and Planetary Sciences 3

60%

Medicine and Dentistry 1

20%

Computer Science 1

20%

Save time finding and organizing research with Mendeley

Sign up for free
0