Subgrid-scale process: Difference between revisions
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<div class="definition"><div class="short_definition">Atmospheric processes that cannot be adequately resolved within a [[numerical simulation]].</div><br/> <div class="paragraph">Examples can include [[turbulent fluxes]], [[phase changes]] of water, chemical reactions, and [[radiative flux divergence]]. Such processes are often parameterized in numerical integrations and even neglected in some applications. <br/>''See'' [[parameterization]], [[convective adjustment]], [[Mellor–Yamada parameterization]], [[shallow convection parameterization]].</div><br/> </div> | <div class="definition"><div class="short_definition">Atmospheric processes that cannot be adequately resolved within a [[numerical simulation|numerical simulation]].</div><br/> <div class="paragraph">Examples can include [[turbulent flux|turbulent fluxes]], [[phase changes]] of water, chemical reactions, and [[radiative flux divergence]]. Such processes are often parameterized in numerical integrations and even neglected in some applications. <br/>''See'' [[parameterization]], [[convective adjustment]], [[Mellor–Yamada parameterization|Mellor–Yamada parameterization]], [[shallow convection parameterization]].</div><br/> </div> | ||
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Latest revision as of 17:00, 25 April 2012
subgrid-scale process
Atmospheric processes that cannot be adequately resolved within a numerical simulation.
Examples can include turbulent fluxes, phase changes of water, chemical reactions, and radiative flux divergence. Such processes are often parameterized in numerical integrations and even neglected in some applications.
See parameterization, convective adjustment, Mellor–Yamada parameterization, shallow convection parameterization.
See parameterization, convective adjustment, Mellor–Yamada parameterization, shallow convection parameterization.