Editing Sublimation (phase transition) (section)

===Water===
[[Snow]] and [[ice]] sublime gradually at temperatures below the solid-liquid boundary (melting point) (generally 0&nbsp;°C), and at partial pressures below the triple point pressure of {{convert|612|Pa|atm|abbr=on}}, at a low rate.<ref>{{cite journal |last=Fassnacht |first=S. R. |year=2004 |title=Estimating Alter-shielded gauge snowfall undercatch, snowpack sublimation, and blowing snow transport at six sites in the coterminous USA |journal=Hydrol. Process. |doi=10.1002/hyp.5806 |bibcode=2004HyPr...18.3481F |volume=18 |issue=18 |pages=3481–3492|s2cid=129927018 }}</ref> In [[freeze-drying]], the material to be dehydrated is frozen and its water is allowed to sublime under reduced pressure or vacuum. The loss of snow from a [[snowfield]] during a cold spell is often caused by sunshine acting directly on the upper layers of the snow. Sublimation of ice is a factor to the erosive wear of [[glacier ice]], known as [[ablation]] in [[glaciology]].<ref>{{Cite web |url=http://amsglossary.allenpress.com/glossary/search?p=1&query=ablation&submit=Search |title=''Glossary of Meteorology'' |access-date=2010-07-05 |archive-url=https://web.archive.org/web/20110917232831/http://amsglossary.allenpress.com/glossary/search?p=1&query=ablation&submit=Search |archive-date=2011-09-17 |url-status=dead }}</ref>