| appearance as argument number 1 |
|
| (documentation FohnWind EnglishLanguage "A FohnWind is a type of dry, relatively warm downslope wind in the lee of a mountain range. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes. As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes.[Wikipedia]") | Weather.kif 2184-2188 | |
| (subclass FohnWind Wind) | Weather.kif 2183-2183 | Fohn wind is a subclass of wind |
| appearance as argument number 2 |
|
|
| (names "Foehn" FohnWind) | Weather.kif 2191-2191 | Fohn wind has &ames$"name" "Foehn" |
| (names "Föhn" FohnWind) | Weather.kif 2190-2190 | Fohn wind has &ames$"name" "Föhn" |
| (relatedInternalConcept KatabaticWind FohnWind) | Weather.kif 2514-2514 | Katabatic wind is internally related to Fohn wind |
| (subclass InteriorChinookWind FohnWind) | Weather.kif 2170-2170 | Interior chinook wind is a subclass of Fohn wind |
| (subclass ZondaWind FohnWind) | Weather.kif 2214-2214 | Zonda wind is a subclass of Fohn wind |
| (termFormat EnglishLanguage FohnWind "Fohn wind") | Weather.kif 2189-2189 | Zonda wind is a subclass of Fohn wind |
| antecedent |
|
|
| (=> (and (instance ?W FohnWind) (eventLocated ?W ?A) (instance ?A GeographicArea) (instance ?M MountainRange)) (orientation ?A ?M Downwind)) |
Weather.kif 2202-2208 |
|
| (=> (and (instance ?W FohnWind) (path ?W ?P) (origin ?W ?H) (destination ?W ?L) (beforeOnPath ?H ?L ?P ?W)) (orientation ?L ?H Downhill)) |
Weather.kif 2193-2200 |
|
| (=> (instance ?W FohnWind) (property ?W Dry)) |
Weather.kif 2210-2212 |
|
Show full definition with tree view
Show simplified definition (without tree view)
Show simplified definition (with tree view)
|
|
Sigma web home Suggested Upper Merged Ontology (SUMO) web home
Sigma version 3.0 is open source software produced by Articulate Software and its partners