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- Zero-curtain_effect abstract "The zero-curtain effect occurs in cold (particularly periglacial) environments where the phase transition of water to ice is retarded due to latent heat release. The effect is notably found in arctic and alpine permafrost sediments, and occurs where the air temperature falls below 0°C (the freezing point of water) followed by a rapid drop in soil temperature.Because of this effect, the lowering of temperature in moist, cold ground does not happen at a uniform rate. The loss of heat through conduction is reduced when water freezes, and latent heat is released. This heat of fusion is continually released until all the subsurface water has frozen, at which point temperatures can continue to fall.Therefore, for as long as water is available to the system (for example, through cryosuction/capillary action) the temperature of the sediment will remain at a constant temperature.".
- Zero-curtain_effect thumbnail Zero-curtain-effect.svg?width=300.
- Zero-curtain_effect wikiPageID "27554141".
- Zero-curtain_effect wikiPageLength "1857".
- Zero-curtain_effect wikiPageOutDegree "15".
- Zero-curtain_effect wikiPageRevisionID "688096207".
- Zero-curtain_effect wikiPageWikiLink Alpine_climate.
- Zero-curtain_effect wikiPageWikiLink Arctic.
- Zero-curtain_effect wikiPageWikiLink Capillary_action.
- Zero-curtain_effect wikiPageWikiLink Category:Arctic_geography_terminology.
- Zero-curtain_effect wikiPageWikiLink Category:Geomorphology.
- Zero-curtain_effect wikiPageWikiLink Category:Phase_transitions.
- Zero-curtain_effect wikiPageWikiLink Cryosuction.
- Zero-curtain_effect wikiPageWikiLink Ice.
- Zero-curtain_effect wikiPageWikiLink Latent_heat.
- Zero-curtain_effect wikiPageWikiLink Melting_point.
- Zero-curtain_effect wikiPageWikiLink Periglaciation.
- Zero-curtain_effect wikiPageWikiLink Permafrost.
- Zero-curtain_effect wikiPageWikiLink Phase_transition.
- Zero-curtain_effect wikiPageWikiLink Water.
- Zero-curtain_effect wikiPageWikiLink File:Zero-curtain-effect.svg.
- Zero-curtain_effect wikiPageWikiLinkText "Zero-curtain effect".
- Zero-curtain_effect wikiPageUsesTemplate Template:Geomorph-stub.
- Zero-curtain_effect wikiPageUsesTemplate Template:Periglacial_environment.
- Zero-curtain_effect wikiPageUsesTemplate Template:Reflist.
- Zero-curtain_effect subject Category:Arctic_geography_terminology.
- Zero-curtain_effect subject Category:Geomorphology.
- Zero-curtain_effect subject Category:Phase_transitions.
- Zero-curtain_effect hypernym Due.
- Zero-curtain_effect type SportsEvent.
- Zero-curtain_effect type Mechanic.
- Zero-curtain_effect type Process.
- Zero-curtain_effect type Redirect.
- Zero-curtain_effect type Science.
- Zero-curtain_effect type Subfield.
- Zero-curtain_effect type Transition.
- Zero-curtain_effect comment "The zero-curtain effect occurs in cold (particularly periglacial) environments where the phase transition of water to ice is retarded due to latent heat release. The effect is notably found in arctic and alpine permafrost sediments, and occurs where the air temperature falls below 0°C (the freezing point of water) followed by a rapid drop in soil temperature.Because of this effect, the lowering of temperature in moist, cold ground does not happen at a uniform rate.".
- Zero-curtain_effect label "Zero-curtain effect".
- Zero-curtain_effect sameAs Q8069438.
- Zero-curtain_effect sameAs m.0c00dc8.
- Zero-curtain_effect sameAs Q8069438.
- Zero-curtain_effect wasDerivedFrom Zero-curtain_effect?oldid=688096207.
- Zero-curtain_effect depiction Zero-curtain-effect.svg.
- Zero-curtain_effect isPrimaryTopicOf Zero-curtain_effect.