Difference between revisions of "Template:Westarctica.wiki:Today's featured article"

 
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Her Ladyship, the '''[[Countess of Benton]]''', Deborah McHenry, is the mother of [[Grand Duke Travis]], and a member of the [[Peerage of Westarctica]]. The Countess was invested as a Dame Commander in the [[Order of the Snowflake]] at the same time she received her title. The Countess is an active part of [[Westarctica]], having represented the nation during the [[2017 - State visit in Scone|2017 State Visit to the Kingdom of Scone]]. She is also a frequent participant in Westarctica's Citizen's Group on Facebook where she has welcomed most new guests as a representative of the [[Grand Duke of Westarctica|Grand Duke]].
'''[[Drift ice]]''' is the sea ice of the [[Southern Ocean]]. It extends far north in winter and retreats almost to the coastline each summer. Sea ice is frozen seawater that is usually less than a few meters thick. This is in contrast to [[Ice shelf|ice shelves]], which are formed by glaciers, float in the sea, and are up to a kilometer thick. There are two subdivisions of sea ice: fast ice, which is attached to land; and ice floes, which are not.


Her Ladyship joined the official Westarctica delegation to [[MicroCon 2019]] in Hamilton, Ontario. Prior to the beginning of the conference, Countess Deborah was invested as a Dame in the [[Order of the Orca]], and debuted her new regalia during the evening awards banquet. In August 2019, Deborah was commissioned as a lieutenant in the Naval Detachment of the [[Westarctican Royal Guards]]. After completing a shakedown cruise on the Susquehanna River, Her Ladyship served as communications officer in training on board the USS ''Don Quixote'' during [[Exercise: Westarctic Chill]] with [[Slabovia]].
Sea ice in the Southern Ocean melts from the bottom instead of from the surface like Arctic ice because it is covered in snow. As a result, melt ponds are rarely observed. On average, [[Antarctica|Antarctic]] sea ice is younger, thinner, warmer, saltier, and more mobile than Arctic sea ice. Due to its inaccessibility, it is not as well-studied as Arctic ice.


'''([[Countess of Benton|Full Article...]])'''
'''([[Drift ice|Full Article...]])'''

Latest revision as of 16:39, 25 October 2024

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Drift ice is the sea ice of the Southern Ocean. It extends far north in winter and retreats almost to the coastline each summer. Sea ice is frozen seawater that is usually less than a few meters thick. This is in contrast to ice shelves, which are formed by glaciers, float in the sea, and are up to a kilometer thick. There are two subdivisions of sea ice: fast ice, which is attached to land; and ice floes, which are not.

Sea ice in the Southern Ocean melts from the bottom instead of from the surface like Arctic ice because it is covered in snow. As a result, melt ponds are rarely observed. On average, Antarctic sea ice is younger, thinner, warmer, saltier, and more mobile than Arctic sea ice. Due to its inaccessibility, it is not as well-studied as Arctic ice.

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