A belt of dry hi pressure air
Are formed yes
Roughly 3 degrees per thousand feet
10 K/km (in the troposphere)
* Rising Unstable air * moisture * Air cools with an increasing altitude
convection currents work when heated water cools then goes to the bottom then heats back up
Rising air cools and compresses adiabatically.
Are formed yes
rising air expands then cools and condenses
Either by releasing some of the air it contains or by not applying more heat - as the air cools the balloon descends.
the magma cools on the surface and eventually u get land
Roughly 3 degrees per thousand feet
10 K/km (in the troposphere)
* Rising Unstable air * moisture * Air cools with an increasing altitude
* Rising Unstable air * moisture * Air cools with an increasing altitude
so the poler bears have a place to live in
Rising air contains water vapour which condenses as the air cools with altitude.
Hot air rising and sthen cools and sinks and forms udder like shaped clouds