A new Chemical Lagrangian Model of the Stratosphere (CLaMS) 1. Formulation of advection and mixing

By D. McKenna, P. Konopka, J. Grooß, G. Günther, R. Müller, R. Spang, D. Offermann, Y. Orsolini. 2002

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Impact of the vertical velocity scheme on modeling transport in the tropical tropopause layer (2010, methodology): “[21] For the trajectory calculations we use the trajectory program CLaMS-TRAJ which is part of the Lagrangian chemical transport model CLaMS [McKenna et al., 2002; Konopka et al., 2007].”
Mixing and ozone loss in the 1999–2000 Arctic vortex: Simulations with the three‐dimensional Chemical Lagrangian Model of the Stratosphere (CLaMS) (2004, methodology): “While the purely advective transport is completely reversible, the regridding procedure that is driven by the deformations in the flow, defines the amount of irreversibility (i.e., mixing) affecting the transport of the chemical constituents [McKenna et al., 2002b].”
Horizontal water vapor transport in the lower stratosphere from subtropics to high latitudes during boreal summer (2013, methodology): “[12] The CLaMS model [e.g., McKenna et al., 2002a, 2002b; Konopka et al., 2007] is a Lagrangian chemistry transport model, based on three-dimensional forward trajectories describing the motion of air parcels, denoted CLaMS air parcels in the following.”