Yukimarimo
Yukimarimo are balls of fine frost formed at low temperatures on the Antarctic plateau during weak wind conditions. Yukimarimo were discovered in 1995 at Dome Fuji by the 36th Japanese Antarctic Research Expedition (JARE-36) at temperatures of -59 to -72 C. [Ref 1] [Ref 2] Electrostatic attraction between ice crystals explains the formation of yukimarimo at these low temperatures.[Ref 3]
Name
Yukimarimo were named by T. Kameda on JARE-36 in 1995. "Yuki" means snow in Japanese, and "marimo" is a ball-like growth of water algae which the yukimarimo resemble.
Formation
During a storm on the antarctic plateau the humidity is higher than normal. After a storm, the temperature rapidly drops and and due to the excess humidity, hoarfrost forms on the surface of the snow. At these low temperatures, electrostatic attraction between the rapidly formed ice crystals is high due to growth charging during formation. When a light wind blows after the formation of this hoarfrost, the hoarfrost breaks apart and the frost crystals clump together and stick due to the high electrostatic attraction and tumble across the snow in a manner similar to tumbleweeds. [Ref 3]
- Photos of yukimarimo taken by winterover Keith Vanderlinde at dawn 2008 at the South Pole while wintering over for the South Pole Telescope.
-
-
Commercial Products
To celebrate the discovery of the yukimarimo, a line of cookies were manufactured in Japan. They are available at a few stores in Japan and online[1].
References
- ^
T. Kameda , H. Yoshimi, N. Azuma and H. Motoyama (1999). "Observation of "yukimarimo" on the snow surface of the inland plateau, Antarctic ice sheet". Journal of Glaciology. 45 (150): 394–396.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - ^ T. Kameda (2007). "Discovery and reunion with yukimarimo" (PDF). Seppyo (Journal of Japanese Society of Snow and Ice). 69 (3): 403–407.
- ^ a b J. Nelson and M. Baker (2003). "Charging of ice-vapor interfaces" (PDF). Atmospheric Chemistry and Physics Discussions. 3: 41–73.