20.01.2013 Aufrufe

Forschung und wissenschaftliches Rechnen - Beiträge zum - GWDG

Forschung und wissenschaftliches Rechnen - Beiträge zum - GWDG

Forschung und wissenschaftliches Rechnen - Beiträge zum - GWDG

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automatic time step control. Although computationally more demanding, the<br />

latter are best suited for the most difficult stiffness problems e.g. associated<br />

with multiphase chemistry. For each individual application, it is necessary to<br />

balance the advantages and disadvantages regarding efficiency, stability, accuracy,<br />

and precision. We fo<strong>und</strong> that for most of our chemical mechanisms,<br />

the Rosenbrock solvers of 2nd or 3rd order (ros2 and ros3) work best. However,<br />

we stress that it may be necessary to test other solvers as well (e.g.<br />

radau5) to achieve the best performance for a given set of equations. Fortunately,<br />

switching between solvers is easy with KPP and does not require<br />

any reprogramming of the chemistry scheme. The selection of a chemical<br />

equation set and a numerical solver is shown in Fig. 6.<br />

4.16 OFFLEM<br />

MAINTAINER: Patrick Jöckel<br />

DESCRIPTION: This submodel reads input data from files for two-dimensional<br />

emission fluxes (i.e. surface emissions in molecules/(m 2 s)) and threedimensional<br />

emission fluxes (aircraft emissions in molecules/(m 3 s)) and updates<br />

the tracer tendencies (gridpoint- and Lagrangian) accordingly.<br />

4.17 ONLEM<br />

MAINTAINER: Astrid Kerkweg<br />

CONTRIBUTIONS: Yves Balkanski (LSCE), Ina Tegen (MPI-BG), Philip<br />

Stier (MPI-MET), Sylvia Kloster (MPI-MET), Laurens Ganzeveld, Michael<br />

Schulz (LSCE)<br />

DESCRIPTION: This submodel calculates two-dimensional emission fluxes<br />

for gas-phase tracers (i.e. surface emissions in molecules/(m 2 s)) and updates<br />

the tracer tendencies accordingly. In addition, aerosol source functions are<br />

calculated.<br />

4.18 PSC<br />

MAINTAINER: Joachim Buchholz<br />

ORIGINAL CODE: Ken Carslaw, Stefanie Meilinger, Joachim Buchholz<br />

DESCRIPTION: The Polar Stratospheric Cloud (PSC) submodel simulates<br />

micro-physical processes that lead to the formation of super-cooled ternary<br />

solutions (STS), nitric acid trihydrate (NAT), and ice particles in the polar<br />

stratosphere as well as heterogeneous chemical reactions of halogens and<br />

dinitrogen pentoxide on liquid and solid aerosol particles. Denitrification and<br />

dehydration due to sedimenting solid PSC particles are calculated for each<br />

grid box depending on particle size, pressure and temperature.<br />

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