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'''[[Baron of Bastanchury]]''' is a [[courtesy title]] held by the ruler of the Barony of Bastanchury. It was originally a subordinate title held by [[Grand Duke Travis]] when he was King of [[Colony of Calsahara|Calsahara]], however, he granted the title as a courtesy to Westarctica's new [[Minister of Information]] in March 2018 to recognize the latter's previous support of Calsahara. It is one of only two peerage titles in the [[Nobility of Calsahara]] that is not held by Grand Duke Travis.
'''[[Drift ice|Antarctic sea 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. 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.


The Baron has been an extremely active member of the [[Royal Council]] and was responsible for designing Westarctica's first paper currency, the [[Ice mark]]. His Lordship was appointed to the position of [[Commissioner of the Treasury]] with responsibility for managing the [[Central Bank of Westarctica]] on behalf of the Crown, and [[Captain-General of Calsahara]]. His Lordship served as Minister of Information for just over a year from 2018 - 2019, when he was transferred to the post of [[Minister of Commerce]] to oversee [[Westarctica|Westarctica's]] retail product offerings.
Westarctica's sea ice cover is highly seasonal, with very little ice in the austral summer, expanding to an area roughly equal to that of mainland [[Westarctica]] in the winter. It peaks during September, which marks the end of austral winter, and retreats to a minimum in February.


'''([[Baron of Bastanchury|Full Article...]])'''
'''([[Drift ice|Full Article...]])'''

Revision as of 01:55, 25 November 2019

Kontio tow.jpg

Antarctic sea 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.

Westarctica's sea ice cover is highly seasonal, with very little ice in the austral summer, expanding to an area roughly equal to that of mainland Westarctica in the winter. It peaks during September, which marks the end of austral winter, and retreats to a minimum in February.

(Full Article...)