Eta vertical coordinate: Difference between revisions
From Glossary of Meteorology
imported>Perlwikibot (Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == eta vertical coordinate == </div> <div class="definition"><div class="short_definition">A v...") |
imported>Perlwikibot No edit summary |
||
Line 9: | Line 9: | ||
</div> | </div> | ||
<div class="definition"><div class="short_definition">A vertical coordinate for atmospheric models defined with a steplike representation of [[topography]], having mountains formed of [[grid]] boxes of the [[model]].</div><br/> <div class="paragraph">The vertical coordinate surfaces are quasi-horizontal, intersecting model mountains or forming their nearly horizontal upper sides. It is defined by <div class="display-formula"><blockquote>[[File:ams2001glos-Ee62.gif|link=|center|ams2001glos-Ee62]]</blockquote></div> where ''p'' is [[pressure]]; the subscripts ''T'' and ''S'' stand for the top and the ground surface values of the [[model atmosphere]], respectively; ''z'' is geometric height; and ''p''<sub>''ref''</sub>(''z'') is a suitably defined reference pressure as a function of ''z''. The ground surface heights ''z''<sub>''S''</sub> are permitted to take only a discrete set of values, those of elevations at which the interfaces of the chosen model layers are located when pressure is equal to the reference pressure ''p''<sub>''ref''</sub>(''z''). The | <div class="definition"><div class="short_definition">A vertical coordinate for atmospheric models defined with a steplike representation of [[topography]], having mountains formed of [[grid]] boxes of the [[model]].</div><br/> <div class="paragraph">The vertical coordinate surfaces are quasi-horizontal, intersecting model mountains or forming their nearly horizontal upper sides. It is defined by <div class="display-formula"><blockquote>[[File:ams2001glos-Ee62.gif|link=|center|ams2001glos-Ee62]]</blockquote></div> where ''p'' is [[pressure]]; the subscripts ''T'' and ''S'' stand for the top and the ground surface values of the [[model atmosphere]], respectively; ''z'' is geometric height; and ''p''<sub>''ref''</sub>(''z'') is a suitably defined reference pressure as a function of ''z''. The ground surface heights ''z''<sub>''S''</sub> are permitted to take only a discrete set of values, those of elevations at which the interfaces of the chosen model layers are located when pressure is equal to the reference pressure ''p''<sub>''ref''</sub>(''z''). The "Eta Model" using the eta coordinate became the primary short-range operational forecasting model of the U.S. National Weather Service in 1993. <br/>''See'' [[sigma vertical coordinate]], [[isentropic vertical coordinate]], [[hybrid vertical coordinate]], [[vertical coordinate system]].</div><br/> </div> | ||
</div> | </div> | ||
Latest revision as of 14:11, 20 February 2012
eta vertical coordinate
A vertical coordinate for atmospheric models defined with a steplike representation of topography, having mountains formed of grid boxes of the model.
The vertical coordinate surfaces are quasi-horizontal, intersecting model mountains or forming their nearly horizontal upper sides. It is defined by where p is pressure; the subscripts T and S stand for the top and the ground surface values of the model atmosphere, respectively; z is geometric height; and pref(z) is a suitably defined reference pressure as a function of z. The ground surface heights zS are permitted to take only a discrete set of values, those of elevations at which the interfaces of the chosen model layers are located when pressure is equal to the reference pressure pref(z). The "Eta Model" using the eta coordinate became the primary short-range operational forecasting model of the U.S. National Weather Service in 1993.
See sigma vertical coordinate, isentropic vertical coordinate, hybrid vertical coordinate, vertical coordinate system.
See sigma vertical coordinate, isentropic vertical coordinate, hybrid vertical coordinate, vertical coordinate system.