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Thunderstorms but with Fire!


How would tectonics behave on a two continent planet?Fire Resistant FloraFire Resistant FaunaSurface temperature of a icy rogue planetA world with a moon orbiting much closer than oursExoplanetary Review: Acid RainOn the viability of living balloonsPlanetary tidal locking causing asymetrical water distribution






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2












$begingroup$


The planet is huge roughly four times the size of earth, with lots of hydrogen in its atmosphere (group A water in Hydrogen out, B water out.) it is also very humid. what do I do to have giant Storms in the sky with Fire instead of thunder? What would these storms look like?










share|improve this question









New contributor



WindWelder is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
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  • 2




    $begingroup$
    They probably look like the whole atmosphere igniting in a catastrophic firestorm.
    $endgroup$
    – Starfish Prime
    8 hours ago










  • $begingroup$
    If they breath hydrogen in and out they are not using it for breathing, like we do with nitrogen
    $endgroup$
    – L.Dutch
    8 hours ago

















2












$begingroup$


The planet is huge roughly four times the size of earth, with lots of hydrogen in its atmosphere (group A water in Hydrogen out, B water out.) it is also very humid. what do I do to have giant Storms in the sky with Fire instead of thunder? What would these storms look like?










share|improve this question









New contributor



WindWelder is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.






$endgroup$









  • 2




    $begingroup$
    They probably look like the whole atmosphere igniting in a catastrophic firestorm.
    $endgroup$
    – Starfish Prime
    8 hours ago










  • $begingroup$
    If they breath hydrogen in and out they are not using it for breathing, like we do with nitrogen
    $endgroup$
    – L.Dutch
    8 hours ago













2












2








2





$begingroup$


The planet is huge roughly four times the size of earth, with lots of hydrogen in its atmosphere (group A water in Hydrogen out, B water out.) it is also very humid. what do I do to have giant Storms in the sky with Fire instead of thunder? What would these storms look like?










share|improve this question









New contributor



WindWelder is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.






$endgroup$




The planet is huge roughly four times the size of earth, with lots of hydrogen in its atmosphere (group A water in Hydrogen out, B water out.) it is also very humid. what do I do to have giant Storms in the sky with Fire instead of thunder? What would these storms look like?







science-based planets environment climate






share|improve this question









New contributor



WindWelder is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.










share|improve this question









New contributor



WindWelder is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.








share|improve this question




share|improve this question








edited 2 hours ago







WindWelder













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asked 9 hours ago









WindWelderWindWelder

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New contributor



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Check out our Code of Conduct.




New contributor




WindWelder is a new contributor to this site. Take care in asking for clarification, commenting, and answering.
Check out our Code of Conduct.












  • 2




    $begingroup$
    They probably look like the whole atmosphere igniting in a catastrophic firestorm.
    $endgroup$
    – Starfish Prime
    8 hours ago










  • $begingroup$
    If they breath hydrogen in and out they are not using it for breathing, like we do with nitrogen
    $endgroup$
    – L.Dutch
    8 hours ago












  • 2




    $begingroup$
    They probably look like the whole atmosphere igniting in a catastrophic firestorm.
    $endgroup$
    – Starfish Prime
    8 hours ago










  • $begingroup$
    If they breath hydrogen in and out they are not using it for breathing, like we do with nitrogen
    $endgroup$
    – L.Dutch
    8 hours ago







2




2




$begingroup$
They probably look like the whole atmosphere igniting in a catastrophic firestorm.
$endgroup$
– Starfish Prime
8 hours ago




$begingroup$
They probably look like the whole atmosphere igniting in a catastrophic firestorm.
$endgroup$
– Starfish Prime
8 hours ago












$begingroup$
If they breath hydrogen in and out they are not using it for breathing, like we do with nitrogen
$endgroup$
– L.Dutch
8 hours ago




$begingroup$
If they breath hydrogen in and out they are not using it for breathing, like we do with nitrogen
$endgroup$
– L.Dutch
8 hours ago










2 Answers
2






active

oldest

votes


















3














$begingroup$

[Handwavium explanation]



Without Oxygen, you will have a hard time burning the hydrogen to create a fire.
Since you do not mention the composition of atmosphere, one possible way you can achieve the Firestorm could be via a sudden outburst of oxygen in the atmosphere leading to the right conditions, which are otherwise absent.



This could be due to geological events disturbing internal rock formations storing oxygen - which got formed in the first place due to microbial activity decomposing water into Hydrogen and oxygen. Now, you want this firestorm to take the place of thunder. The regular thunder is produced by interaction of clouds. Instead, you can use a cyclone - they can easily span 400-700kms. This gives you something like a firenado, which you can modify to support taking the oxygen to the upper reaches of the cyclone, where it interacts with hydrogen to lighten up



Another property you could utilize here is that oxygen is much heavier than hydrogen, so they both would be at different altitudes in the atmosphere. So, by using a geological/climatic phenomena that brings the two in contact - say via heating up of surface by sun's rays, variations of walker cycle etc, you can then lighten them up.






share|improve this answer









$endgroup$






















    2














    $begingroup$

    Flame cloud deflagrations.



    1. The surface of your world is mostly reduced gases: hydrogen, water, maybe some ammonia, methane.


    2. On the surface the humidity and fog shields life from most solar radiation. In the higher atmosphere, energetic rays from your sun cause photodissociation of molecules. The main effect of this is to strip oxygen out of water, producing molecular oxygen (O2) and ozone (O3-). These are high enough in altitude to be low concentrations and it is cold up there, so these reactive oxygen species can accumulate without reacting away.


    3: During your storms there is atmospheric mixing. Oxygen rich gases from the upper atmosphere are pulled down into denser regions. They come into contact with hydrogen gas. When concentrations are right and there is a spark, the oxygen and hydrogen combine energetically.



    In these circumstances there would be an excess of hydrogen and a relatively small amount of oxygen. The result would be a slow moving wave of flame, or deflagration.



    deflagration



    https://www.youtube.com/watch?v=6gkblppESHA&t=6s




    A balloon filled with 100% hydrogen is ignited with a small flame. As
    the flame ignites the hydrogen gas, it combines with oxygen in the
    surrounding air. A large, but relatively slowly moving ball of fire is
    created. This is called a deflagration.




    Depicted is the deflagration - the supersonic one is next and it is an explosion, not a sweet flame cloud.



    These are your clouds of fire. Flame is hot gas and so would rise. An initial fireball would spread laterally according to air currents. In still conditions it could form a spreading, rising ring of fire as oxygen is exhausted in the center. Very big rings would just look like a wall of flame moving across the sky, curling and rising as it went.



    H2+O2-> 2 H2O. The result of these flame clouds is water vapor. This would condense in the upper atmosphere and serve to nucleate raindrops. I could imaging that under conditions of atmospheric turnover, a storm begins with flame clouds of this sort which in turn start the rain. Once the rain starts in earnest few additional flame clouds form.






    share|improve this answer









    $endgroup$
















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      2 Answers
      2






      active

      oldest

      votes








      2 Answers
      2






      active

      oldest

      votes









      active

      oldest

      votes






      active

      oldest

      votes









      3














      $begingroup$

      [Handwavium explanation]



      Without Oxygen, you will have a hard time burning the hydrogen to create a fire.
      Since you do not mention the composition of atmosphere, one possible way you can achieve the Firestorm could be via a sudden outburst of oxygen in the atmosphere leading to the right conditions, which are otherwise absent.



      This could be due to geological events disturbing internal rock formations storing oxygen - which got formed in the first place due to microbial activity decomposing water into Hydrogen and oxygen. Now, you want this firestorm to take the place of thunder. The regular thunder is produced by interaction of clouds. Instead, you can use a cyclone - they can easily span 400-700kms. This gives you something like a firenado, which you can modify to support taking the oxygen to the upper reaches of the cyclone, where it interacts with hydrogen to lighten up



      Another property you could utilize here is that oxygen is much heavier than hydrogen, so they both would be at different altitudes in the atmosphere. So, by using a geological/climatic phenomena that brings the two in contact - say via heating up of surface by sun's rays, variations of walker cycle etc, you can then lighten them up.






      share|improve this answer









      $endgroup$



















        3














        $begingroup$

        [Handwavium explanation]



        Without Oxygen, you will have a hard time burning the hydrogen to create a fire.
        Since you do not mention the composition of atmosphere, one possible way you can achieve the Firestorm could be via a sudden outburst of oxygen in the atmosphere leading to the right conditions, which are otherwise absent.



        This could be due to geological events disturbing internal rock formations storing oxygen - which got formed in the first place due to microbial activity decomposing water into Hydrogen and oxygen. Now, you want this firestorm to take the place of thunder. The regular thunder is produced by interaction of clouds. Instead, you can use a cyclone - they can easily span 400-700kms. This gives you something like a firenado, which you can modify to support taking the oxygen to the upper reaches of the cyclone, where it interacts with hydrogen to lighten up



        Another property you could utilize here is that oxygen is much heavier than hydrogen, so they both would be at different altitudes in the atmosphere. So, by using a geological/climatic phenomena that brings the two in contact - say via heating up of surface by sun's rays, variations of walker cycle etc, you can then lighten them up.






        share|improve this answer









        $endgroup$

















          3














          3










          3







          $begingroup$

          [Handwavium explanation]



          Without Oxygen, you will have a hard time burning the hydrogen to create a fire.
          Since you do not mention the composition of atmosphere, one possible way you can achieve the Firestorm could be via a sudden outburst of oxygen in the atmosphere leading to the right conditions, which are otherwise absent.



          This could be due to geological events disturbing internal rock formations storing oxygen - which got formed in the first place due to microbial activity decomposing water into Hydrogen and oxygen. Now, you want this firestorm to take the place of thunder. The regular thunder is produced by interaction of clouds. Instead, you can use a cyclone - they can easily span 400-700kms. This gives you something like a firenado, which you can modify to support taking the oxygen to the upper reaches of the cyclone, where it interacts with hydrogen to lighten up



          Another property you could utilize here is that oxygen is much heavier than hydrogen, so they both would be at different altitudes in the atmosphere. So, by using a geological/climatic phenomena that brings the two in contact - say via heating up of surface by sun's rays, variations of walker cycle etc, you can then lighten them up.






          share|improve this answer









          $endgroup$



          [Handwavium explanation]



          Without Oxygen, you will have a hard time burning the hydrogen to create a fire.
          Since you do not mention the composition of atmosphere, one possible way you can achieve the Firestorm could be via a sudden outburst of oxygen in the atmosphere leading to the right conditions, which are otherwise absent.



          This could be due to geological events disturbing internal rock formations storing oxygen - which got formed in the first place due to microbial activity decomposing water into Hydrogen and oxygen. Now, you want this firestorm to take the place of thunder. The regular thunder is produced by interaction of clouds. Instead, you can use a cyclone - they can easily span 400-700kms. This gives you something like a firenado, which you can modify to support taking the oxygen to the upper reaches of the cyclone, where it interacts with hydrogen to lighten up



          Another property you could utilize here is that oxygen is much heavier than hydrogen, so they both would be at different altitudes in the atmosphere. So, by using a geological/climatic phenomena that brings the two in contact - say via heating up of surface by sun's rays, variations of walker cycle etc, you can then lighten them up.







          share|improve this answer












          share|improve this answer



          share|improve this answer










          answered 8 hours ago









          mu 無mu 無

          9253 silver badges7 bronze badges




          9253 silver badges7 bronze badges


























              2














              $begingroup$

              Flame cloud deflagrations.



              1. The surface of your world is mostly reduced gases: hydrogen, water, maybe some ammonia, methane.


              2. On the surface the humidity and fog shields life from most solar radiation. In the higher atmosphere, energetic rays from your sun cause photodissociation of molecules. The main effect of this is to strip oxygen out of water, producing molecular oxygen (O2) and ozone (O3-). These are high enough in altitude to be low concentrations and it is cold up there, so these reactive oxygen species can accumulate without reacting away.


              3: During your storms there is atmospheric mixing. Oxygen rich gases from the upper atmosphere are pulled down into denser regions. They come into contact with hydrogen gas. When concentrations are right and there is a spark, the oxygen and hydrogen combine energetically.



              In these circumstances there would be an excess of hydrogen and a relatively small amount of oxygen. The result would be a slow moving wave of flame, or deflagration.



              deflagration



              https://www.youtube.com/watch?v=6gkblppESHA&t=6s




              A balloon filled with 100% hydrogen is ignited with a small flame. As
              the flame ignites the hydrogen gas, it combines with oxygen in the
              surrounding air. A large, but relatively slowly moving ball of fire is
              created. This is called a deflagration.




              Depicted is the deflagration - the supersonic one is next and it is an explosion, not a sweet flame cloud.



              These are your clouds of fire. Flame is hot gas and so would rise. An initial fireball would spread laterally according to air currents. In still conditions it could form a spreading, rising ring of fire as oxygen is exhausted in the center. Very big rings would just look like a wall of flame moving across the sky, curling and rising as it went.



              H2+O2-> 2 H2O. The result of these flame clouds is water vapor. This would condense in the upper atmosphere and serve to nucleate raindrops. I could imaging that under conditions of atmospheric turnover, a storm begins with flame clouds of this sort which in turn start the rain. Once the rain starts in earnest few additional flame clouds form.






              share|improve this answer









              $endgroup$



















                2














                $begingroup$

                Flame cloud deflagrations.



                1. The surface of your world is mostly reduced gases: hydrogen, water, maybe some ammonia, methane.


                2. On the surface the humidity and fog shields life from most solar radiation. In the higher atmosphere, energetic rays from your sun cause photodissociation of molecules. The main effect of this is to strip oxygen out of water, producing molecular oxygen (O2) and ozone (O3-). These are high enough in altitude to be low concentrations and it is cold up there, so these reactive oxygen species can accumulate without reacting away.


                3: During your storms there is atmospheric mixing. Oxygen rich gases from the upper atmosphere are pulled down into denser regions. They come into contact with hydrogen gas. When concentrations are right and there is a spark, the oxygen and hydrogen combine energetically.



                In these circumstances there would be an excess of hydrogen and a relatively small amount of oxygen. The result would be a slow moving wave of flame, or deflagration.



                deflagration



                https://www.youtube.com/watch?v=6gkblppESHA&t=6s




                A balloon filled with 100% hydrogen is ignited with a small flame. As
                the flame ignites the hydrogen gas, it combines with oxygen in the
                surrounding air. A large, but relatively slowly moving ball of fire is
                created. This is called a deflagration.




                Depicted is the deflagration - the supersonic one is next and it is an explosion, not a sweet flame cloud.



                These are your clouds of fire. Flame is hot gas and so would rise. An initial fireball would spread laterally according to air currents. In still conditions it could form a spreading, rising ring of fire as oxygen is exhausted in the center. Very big rings would just look like a wall of flame moving across the sky, curling and rising as it went.



                H2+O2-> 2 H2O. The result of these flame clouds is water vapor. This would condense in the upper atmosphere and serve to nucleate raindrops. I could imaging that under conditions of atmospheric turnover, a storm begins with flame clouds of this sort which in turn start the rain. Once the rain starts in earnest few additional flame clouds form.






                share|improve this answer









                $endgroup$

















                  2














                  2










                  2







                  $begingroup$

                  Flame cloud deflagrations.



                  1. The surface of your world is mostly reduced gases: hydrogen, water, maybe some ammonia, methane.


                  2. On the surface the humidity and fog shields life from most solar radiation. In the higher atmosphere, energetic rays from your sun cause photodissociation of molecules. The main effect of this is to strip oxygen out of water, producing molecular oxygen (O2) and ozone (O3-). These are high enough in altitude to be low concentrations and it is cold up there, so these reactive oxygen species can accumulate without reacting away.


                  3: During your storms there is atmospheric mixing. Oxygen rich gases from the upper atmosphere are pulled down into denser regions. They come into contact with hydrogen gas. When concentrations are right and there is a spark, the oxygen and hydrogen combine energetically.



                  In these circumstances there would be an excess of hydrogen and a relatively small amount of oxygen. The result would be a slow moving wave of flame, or deflagration.



                  deflagration



                  https://www.youtube.com/watch?v=6gkblppESHA&t=6s




                  A balloon filled with 100% hydrogen is ignited with a small flame. As
                  the flame ignites the hydrogen gas, it combines with oxygen in the
                  surrounding air. A large, but relatively slowly moving ball of fire is
                  created. This is called a deflagration.




                  Depicted is the deflagration - the supersonic one is next and it is an explosion, not a sweet flame cloud.



                  These are your clouds of fire. Flame is hot gas and so would rise. An initial fireball would spread laterally according to air currents. In still conditions it could form a spreading, rising ring of fire as oxygen is exhausted in the center. Very big rings would just look like a wall of flame moving across the sky, curling and rising as it went.



                  H2+O2-> 2 H2O. The result of these flame clouds is water vapor. This would condense in the upper atmosphere and serve to nucleate raindrops. I could imaging that under conditions of atmospheric turnover, a storm begins with flame clouds of this sort which in turn start the rain. Once the rain starts in earnest few additional flame clouds form.






                  share|improve this answer









                  $endgroup$



                  Flame cloud deflagrations.



                  1. The surface of your world is mostly reduced gases: hydrogen, water, maybe some ammonia, methane.


                  2. On the surface the humidity and fog shields life from most solar radiation. In the higher atmosphere, energetic rays from your sun cause photodissociation of molecules. The main effect of this is to strip oxygen out of water, producing molecular oxygen (O2) and ozone (O3-). These are high enough in altitude to be low concentrations and it is cold up there, so these reactive oxygen species can accumulate without reacting away.


                  3: During your storms there is atmospheric mixing. Oxygen rich gases from the upper atmosphere are pulled down into denser regions. They come into contact with hydrogen gas. When concentrations are right and there is a spark, the oxygen and hydrogen combine energetically.



                  In these circumstances there would be an excess of hydrogen and a relatively small amount of oxygen. The result would be a slow moving wave of flame, or deflagration.



                  deflagration



                  https://www.youtube.com/watch?v=6gkblppESHA&t=6s




                  A balloon filled with 100% hydrogen is ignited with a small flame. As
                  the flame ignites the hydrogen gas, it combines with oxygen in the
                  surrounding air. A large, but relatively slowly moving ball of fire is
                  created. This is called a deflagration.




                  Depicted is the deflagration - the supersonic one is next and it is an explosion, not a sweet flame cloud.



                  These are your clouds of fire. Flame is hot gas and so would rise. An initial fireball would spread laterally according to air currents. In still conditions it could form a spreading, rising ring of fire as oxygen is exhausted in the center. Very big rings would just look like a wall of flame moving across the sky, curling and rising as it went.



                  H2+O2-> 2 H2O. The result of these flame clouds is water vapor. This would condense in the upper atmosphere and serve to nucleate raindrops. I could imaging that under conditions of atmospheric turnover, a storm begins with flame clouds of this sort which in turn start the rain. Once the rain starts in earnest few additional flame clouds form.







                  share|improve this answer












                  share|improve this answer



                  share|improve this answer










                  answered 8 hours ago









                  WillkWillk

                  140k34 gold badges263 silver badges582 bronze badges




                  140k34 gold badges263 silver badges582 bronze badges
























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