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##### Cited by 50 publications
(61 citation statements)
##### References 83 publications
(61 reference statements)
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“…However, we must be cautious with their application to the turbulent convective-scale regime (cf. Lauritzen et al 2011). Although some successful turbulent applications may be found in the literature, semiLagrangian schemes work most efficiently for a relatively laminar flow.…”
Section: Data Assimilationmentioning
confidence: 99%
“…However, we must be cautious with their application to the turbulent convective-scale regime (cf. Lauritzen et al 2011). Although some successful turbulent applications may be found in the literature, semiLagrangian schemes work most efficiently for a relatively laminar flow.…”
Section: Data Assimilationmentioning
confidence: 99%
“…A number of desirable properties for numerical schemes solving the continuity and other prognostic equations have been identified (e.g., Rasch and Williamson, 1990;Schär and Smolarkiewicz, 1996;Lin and Rood, 1996;Jöckel et al, 2001;Lauritzen et al, 2011). These deal with 1.…”
Section: Desirable Propertiesmentioning
confidence: 99%
“…Horizontal tracer mass fluxes are derived using the horizontal wind field. The vertical velocity ω FFSL used in the FFSL tracer transport is derived from the continuity equation for the tracer from the horizontal tracer mass fluxes for individual model grid boxes (Lin, 2004;Lauritzen et al, 2011). This vertical velocity ω FFSL differs from the vertical velocity ω spec deduced from the wind field, since different advection schemes are used for the air-mass density and for trace gases: the spectral advection is used for air-mass density, whereas the grid-pointbased FFSL transport is used for the tracers.…”
Section: Kinematic Vertical Velocitymentioning
confidence: 99%
“…The internal grid in the FFSL transport module differs from the η-grid in ECHAM5: it is variable in the vertical dimension and fixed in the horizontal dimensions. This concept is denoted as "vertically Lagrangian" (Lin, 2004) or "floating Lagrangian vertical coordinate" (Lauritzen et al, 2011). In each advection time step, horizontal mass fluxes through the lateral boundaries are calculated for each grid box.…”
Section: Kinematic Vertical Velocitymentioning
confidence: 99%