Difference between revisions of "Very Thin Atmosphere"

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[[ATM-2-T5-Fan-Andy-Bigwood 22-Oct-2019a.jpg|right]]
 
A [[Very Thin Atmosphere]] is a type of [[atmosphere]] which requires a [[respirator]].  
 
A [[Very Thin Atmosphere]] is a type of [[atmosphere]] which requires a [[respirator]].  
 
* The atmosphere has a pressure of 0.1 to 0.42 atmospheres, which requires the use of a [[respirator]] to ensure sufficient oxygen.
 
* The atmosphere has a pressure of 0.1 to 0.42 atmospheres, which requires the use of a [[respirator]] to ensure sufficient oxygen.
  
== Description (Specifications) ==
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== Description ([[Specifications]]) ==
 
An [[atmosphere]] rated as Very Thin has a mean [[Atmospheric Pressure|surface pressure]] ranging from 0.10 [[Atmospheric Pressure|atm]] to 0.42 [[Atmospheric Pressure|atm]].
 
An [[atmosphere]] rated as Very Thin has a mean [[Atmospheric Pressure|surface pressure]] ranging from 0.10 [[Atmospheric Pressure|atm]] to 0.42 [[Atmospheric Pressure|atm]].
  
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== History & Background (Dossier) ==
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== History & Background ([[Dossier]]) ==
 
At altitudes above 4,000 [[meter]]s on [[Terra]], such as most of the Tibetan plateau, the oxygen content in every breath full drops almost to 50%, whilst above 7,000 [[meter]]s (the peaks of the Himalaya mountains) the lack of available oxygen reaches lethal levels. This extreme altitude on the 'roof of the world' is equivalent to the [[IISS]] Scout Code atmosphere of Very Thin. For most explorers, [[respirator]]s or [[oxygen mask]]s will be required in this type of [[environment]]. {{Page cite|name=The Universal World Profile|page=14}}
 
At altitudes above 4,000 [[meter]]s on [[Terra]], such as most of the Tibetan plateau, the oxygen content in every breath full drops almost to 50%, whilst above 7,000 [[meter]]s (the peaks of the Himalaya mountains) the lack of available oxygen reaches lethal levels. This extreme altitude on the 'roof of the world' is equivalent to the [[IISS]] Scout Code atmosphere of Very Thin. For most explorers, [[respirator]]s or [[oxygen mask]]s will be required in this type of [[environment]]. {{Page cite|name=The Universal World Profile|page=14}}
  
== References & contributors (Sources) ==
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== References & contributors ([[Sources]]) ==
 
{{Intermediate}}
 
{{Intermediate}}
 
{{Sources
 
{{Sources
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|S9= {{Ludography cite|name=T5 Core Rules|page=409}}
 
|S9= {{Ludography cite|name=T5 Core Rules|page=409}}
 
|S10= {{Ludography cite|name=The Universal World Profile|page=TBD}}
 
|S10= {{Ludography cite|name=The Universal World Profile|page=TBD}}
|S11= Author & Contributor: Lord (Marquis) and Master of Sophontology [[User:Maksim-Smelchak|Maksim-Smelchak]] of the [[Ministry of Science]]
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|S11= [[Traveller Wiki Editorial Team]]
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|S12= Author & Contributor: Lord (Marquis) and Master of Sophontology [[Maksim-Smelchak]] of the [[Ministry of Science]]  
 
}}
 
}}
 
  
 
{{LEN|Atmosphere|Planetology}}
 
{{LEN|Atmosphere|Planetology}}

Revision as of 21:27, 22 October 2019

right A Very Thin Atmosphere is a type of atmosphere which requires a respirator.

  • The atmosphere has a pressure of 0.1 to 0.42 atmospheres, which requires the use of a respirator to ensure sufficient oxygen.

Description (Specifications)

An atmosphere rated as Very Thin has a mean surface pressure ranging from 0.10 atm to 0.42 atm.

Surface Pressure & Water Properties

Surface Pressure & Water Properties
Surface
pressure
Boiling point
of water
0.10 atm 45.5°C
0.25 atm 65°C
0.42 atm 77.5°C

History & Background (Dossier)

At altitudes above 4,000 meters on Terra, such as most of the Tibetan plateau, the oxygen content in every breath full drops almost to 50%, whilst above 7,000 meters (the peaks of the Himalaya mountains) the lack of available oxygen reaches lethal levels. This extreme altitude on the 'roof of the world' is equivalent to the IISS Scout Code atmosphere of Very Thin. For most explorers, respirators or oxygen masks will be required in this type of environment. [1]

References & contributors (Sources)

This list of sources was used by the Traveller Wiki Editorial Team and individual contributors to compose this article. Copyrighted material is used under license from Mongoose Publishing or by permission of the author. The page history lists all of the contributions.