It will be shown later that the scale height, H, is proportional totemperature, T. For an average temperature of 255 K, the scaleheight is 7.5 km assuming an isothermal atmosphere. If the sunheats up the air over Florida so that it is 10 K warmer than theair over the surrounding oceans, before any breezes have a chanceto move the air, what will be the difference in pressure at theground?
What will be the difference in pressure at 10 km altitude? What will happen next in this situation?