Hi,
from terrain-based to cloud-based tectonics (wow!), if we observe
phenomena that are comparable in size, outer morphology and apparent
geometry, the next interesting step is to ask: what about the ratio
between 'cloud-rheology' and upper crust behavior?
In other words, analogue models use scale equations to reproduce reliable
fracture patterns. I therefore suppose that clouds, depending on their
altitude, density, humidity, temperature inner anhisotropy, etc.,
suspended as they are in their aerial medium, must have their 'mechanical'
(will climatologists please forgive me..) response to, eg, high-altitude
wind like crustal rocks do with terrestrial tectonics...
Best regards,
Umberto Fracassi
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