Thanks for your reply. Of course, there are other major factors that come into play with low pressure area formation such as inertial forces (centrifugal force, Coriolis force) due to conservation of momentum and viscous forces (ground friction, energy cascade in turbulent boundary layer flow). However, these only act on preexisting wind fields. Ultimately, those wind fields are generated solely due to horizontal pressure gradient forces and gravity. Examples are a cold air mass next to a warm air mass or a bubble of hot air surrounded by cold air.
In the first case, the warm air will start to flow on top of the cold air, while the cold air will undercut the warm air mass. In the second case, if heat is suddenly supplied to a pocket of air then its pressure will rise so that it is now higher than the immediate surrounding air. The pressure gradient force then moves the air outward to equalize the pressure difference with the environment. The vertical pressure gradient force is now the same as in the initial situation, but the counteracting gravitational force is lower due to the reduced air density after the expansion of the air parcel. So in this case horizontal pressure gradient forces cause an imbalance between the vertical pressure gradient force and gravity such that the parcel is accelerated upwards. Of course, in reality we don't have perfect air masses or air parcels, but rather all cases in between. The atmospheric equations of motion take this fully into account, however.
These initial horizontal pressure gradients can arise due to differences in solar heating (latitude, time of year, albedo due to snow cover, cloud cover, soil type, dust), sensible heat flux, latent heat flux (dry vs wet soil, ocean), net longwave radiation flux (surface emissivity, greenhouse gases) etc. Of course, preexisting wind fields have a major direct or indirect influence on these processes. However, if we started with an atmosphere at rest then within a few months we would have the weather systems as they are now, while if we started with an atmosphere in motion but no solar heating etc. then this atmosphere would come to rest eventually. So thats why I mainly took into account the primary causes of atmospheric motion.
An observational or modelling study would be required to say anything conclusive about a change in tornado occurrence. However, a difficulty is that motions at the scale of a tornado are not yet resolved in current climate models (even not in current operational models). Alternatively, one could look at the frequency of favorable atmospheric environments for tornadoes as a proxy. And if such a study proves me wrong, I would be the first person to admit it .
Just to be clear, the above post was by no means meant to play down any devastating effects of climate change. Thanks for the recommended book, looks interesting!
In the first case, the warm air will start to flow on top of the cold air, while the cold air will undercut the warm air mass. In the second case, if heat is suddenly supplied to a pocket of air then its pressure will rise so that it is now higher than the immediate surrounding air. The pressure gradient force then moves the air outward to equalize the pressure difference with the environment. The vertical pressure gradient force is now the same as in the initial situation, but the counteracting gravitational force is lower due to the reduced air density after the expansion of the air parcel. So in this case horizontal pressure gradient forces cause an imbalance between the vertical pressure gradient force and gravity such that the parcel is accelerated upwards. Of course, in reality we don't have perfect air masses or air parcels, but rather all cases in between. The atmospheric equations of motion take this fully into account, however.
These initial horizontal pressure gradients can arise due to differences in solar heating (latitude, time of year, albedo due to snow cover, cloud cover, soil type, dust), sensible heat flux, latent heat flux (dry vs wet soil, ocean), net longwave radiation flux (surface emissivity, greenhouse gases) etc. Of course, preexisting wind fields have a major direct or indirect influence on these processes. However, if we started with an atmosphere at rest then within a few months we would have the weather systems as they are now, while if we started with an atmosphere in motion but no solar heating etc. then this atmosphere would come to rest eventually. So thats why I mainly took into account the primary causes of atmospheric motion.
An observational or modelling study would be required to say anything conclusive about a change in tornado occurrence. However, a difficulty is that motions at the scale of a tornado are not yet resolved in current climate models (even not in current operational models). Alternatively, one could look at the frequency of favorable atmospheric environments for tornadoes as a proxy. And if such a study proves me wrong, I would be the first person to admit it .
Just to be clear, the above post was by no means meant to play down any devastating effects of climate change. Thanks for the recommended book, looks interesting!