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- Hard_rime abstract "Hard rime is a white ice that forms when the water droplets in fog freeze to the outer surfaces of objects. It is often seen on trees atop mountains and ridges in winter, when low-hanging clouds cause freezing fog. This fog freezes to the windward (wind-facing) side of tree branches, buildings, or any other solid objects, usually with high wind velocities and air temperatures between −2 and −8 °C (28.4 and 17.6 °F). Hard rime formations are difficult to shake off; they have a comb-like appearance, unlike soft rime, which looks feathery or spiky, or clear ice, which looks homogeneous and transparent.Scientists at meteorologically extreme places such as Mount Washington in New Hampshire often have to break huge chunks of hard rime off weather equipment, in order to keep anemometers and other measuring instruments operating.Rime ice can accumulate on the leading edges and control surfaces of aircraft operating in certain meteorological conditions.Meteorologists distinguish between three basic types of ice forming on vertical and horizontal surfaces by deposition of supercooled water droplets. Of course there are also intermediate formations.Soft rime is less dense than hard rime and is milky and crystalline, like sugar. Soft rime appears similar to hoar frost.Hard rime is somewhat less milky, especially if it is not heavy.Clear ice is transparent and homogeneous and resembles ice-cube ice in appearance. Its amorphous, dense structure helps it cling tenaciously to any surface on which it forms. Both rime types are less dense than clear ice and cling less tenaciously, therefore damage due to rime is generally minor compared to clear ice.Glaze ice is similar in appearance to clear ice but it is the result of a completely different process, occurring during freezing rain or drizzle.These three types occur also when ice forms on the surface of an aircraft when it flies through a cloud made of supercooled water liquid droplets. Rime ice is the least dense, milky ice is intermediate and clear ice is the most dense. Dense ice can spoil lift and may have a catastrophic effect on an airborne aircraft.".
- Hard_rime thumbnail Rime_ice.jpg?width=300.
- Hard_rime wikiPageExternalLink search?id=hard-rime1.
- Hard_rime wikiPageExternalLink Rime.htm.
- Hard_rime wikiPageID "429587".
- Hard_rime wikiPageRevisionID "589964081".
- Hard_rime hasPhotoCollection Hard_rime.
- Hard_rime subject Category:Precipitation.
- Hard_rime subject Category:Snow_or_ice_weather_phenomena.
- Hard_rime subject Category:Water_ice.
- Hard_rime type Phenomenon100034213.
- Hard_rime type PhysicalEntity100001930.
- Hard_rime type Process100029677.
- Hard_rime type SnowOrIceWeatherPhenomena.
- Hard_rime comment "Hard rime is a white ice that forms when the water droplets in fog freeze to the outer surfaces of objects. It is often seen on trees atop mountains and ridges in winter, when low-hanging clouds cause freezing fog. This fog freezes to the windward (wind-facing) side of tree branches, buildings, or any other solid objects, usually with high wind velocities and air temperatures between −2 and −8 °C (28.4 and 17.6 °F).".
- Hard_rime label "Calabrosa".
- Hard_rime label "Cencellada dura".
- Hard_rime label "Givre".
- Hard_rime label "Hard rime".
- Hard_rime label "Raueis".
- Hard_rime label "Rijp".
- Hard_rime label "Sincelo".
- Hard_rime label "Szadź".
- Hard_rime label "Изморозь".
- Hard_rime label "雾凇".
- Hard_rime label "霧氷".
- Hard_rime sameAs Raueis.
- Hard_rime sameAs Cencellada_dura.
- Hard_rime sameAs Givre.
- Hard_rime sameAs Calabrosa.
- Hard_rime sameAs 霧氷.
- Hard_rime sameAs 상고대.
- Hard_rime sameAs Rijp.
- Hard_rime sameAs Szadź.
- Hard_rime sameAs Sincelo.
- Hard_rime sameAs m.027hxx.
- Hard_rime sameAs Q131099.
- Hard_rime sameAs Q131099.
- Hard_rime sameAs Hard_rime.
- Hard_rime wasDerivedFrom Hard_rime?oldid=589964081.
- Hard_rime depiction Rime_ice.jpg.
- Hard_rime isPrimaryTopicOf Hard_rime.
