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[jbovlaste] Re: from core to exosphere



On Tue, Aug 11, 2009 at 7:33 PM, tijlan<jbotijlan@gmail.com> wrote:

  Huh?  Why moi in all the following?  Also, despite the fact that
your definitions are generic, your notes only refer to the Earth (in
regards to the altitudes, etc.).  And if only Earth has them, why do
the even need the X2, x3 places?

>
> flemomvacri (troposphere)
> $f_1=v_1$ is the troposphere (the lowest layer of atmosphere) of
> planet/moon $v_2$, of composition $x_3$.
> Notes: From 0 to 17 km in altitude. The Earth's troposphere contains
> approximately 75 percent of the atmosphere's mass and 99 percent of
> its water vapor and aerosols. Cf. {vacri}.
>
> dukmomvacri (stratosphere)
> $d_1=v_1$ is the stratosphere (the second layer of atmosphere) of
> planet/moon $v_2$, of composition $x_3$.
> Notes: From 17 to 50 km in altitude. It is stratified in temperature,
> with warmer layers higher up and cooler layers farther down. This is
> in contrast to the troposphere. Cf. {vacri}.

???  How can an atmosphere be emotionally wrought?  If you looking for
physical turmoil, perhaps you should be looking at se jilca or kalsa?

>
> mijmomvacri (mesosphere)
> $m_1=v_1$ is the mesosphere (the third layer of atmosphere) of
> planet/moon $v_2$, of composition $x_3$.
> Notes: From 50 to 85 in altitude. Cf. {vacri}.
>
> glamomvacri (thermosphere)
> $g_1=v_1$ is the thermosphere (the fourth layer of atmosphere) of
> planet/moon $v_2$, of composition $x_3$.
> Notes: From 85 to over 640 km in altitude. The highly diluted gas in
> this layer can reach 2,500 °C (4532°F) during the day. Cf. {vacri}.
>
> barmomvacri (exosphere)
> $b_1=v_1$ is the exosphere (the uppermost layer of atmosphere) of
> planet/moon $v_2$, of composition $x_3$.
> Notes: From 500-1000 up to 10,000 km in altitude. In the exosphere, an
> upward travelling molecule can escape to space if it is moving fast
> enough to attain escape velocity; otherwise it will be pulled back to
> the celestial body by gravity. Cf. {vacri}.
>
         --gejyspa