Concept information
اصطلاح مرجح
باد یخچالی
نوع
-
http://www.irandoc.ac.ir/onto/irandoc-meta/Concept
مفهوم اعم
تعاریف
- A shallow gravity wind, along the icy surface of a glacier, caused by the temperature difference between the air in contact with the glacier and free air at the same altitude. The glacier wind does not reverse itself diurnally as do mountain and valley winds, but it reaches its maximum intensity in the early afternoon. The glacier wind is characterized by strongly turbulent flow. See katabatic wind.
منسوخ
- false
در زبان های دیگر
-
English
URI
http://www.irandoc.acir/onto/irandoc/SWEETT16178
{{label}}
{{#each values }} {{! loop through ConceptPropertyValue objects }}
{{#if prefLabel }}
{{/if}}
{{/each}}
{{#if notation }}{{ notation }} {{/if}}{{ prefLabel }}
{{#ifDifferentLabelLang lang }} ({{ lang }}){{/ifDifferentLabelLang}}
{{#if vocabName }}
{{ vocabName }}
{{/if}}