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2.3.4: Warm and cold atmospheres

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    78097
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    For warm and cold days, it is used the so called warm (ISA+5, ISA+10, ISA+15, etc.) and cold (ISA-5, ISA-10, ISA-15, etc.), where the increments (decrements) represent the difference with respect to the 288.15 [K] of an average day.

    Given the new \(T_0\), and given the same pressure at sea level (\(p_0\) does not change), the new density at sea level can be calculated. Then the ISA equation are obtained proceeding in the same manner.


    This page titled 2.3.4: Warm and cold atmospheres is shared under a CC BY-SA 3.0 license and was authored, remixed, and/or curated by Manuel Soler Arnedo via source content that was edited to the style and standards of the LibreTexts platform; a detailed edit history is available upon request.

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