Bergeron Classification of Air Masses
The Bergeron classification is the most widely accepted form of air mass classification.. Air mass classification involves three letters. The first letter describes its moisture properties, with c used for continental air masses (dry) and m for maritime air masses (moist). The second letter describes the thermal characteristic of its source region: T for tropical, P for polar, A for arctic or Antarctic, M for monsoon, E for equatorial, and S for superior air (dry air formed by significant upward motion in the atmosphere). The third letter is used to designate the stability of the atmosphere. If the air mass is colder than the ground below it, it is labeled k. If the air mass is warmer than the ground below it, it is labeled w. Fronts separate air masses of different types or origins, and are located along troughs of lower pressure.
Read more about this topic: Weather Fronts
Famous quotes containing the words air and/or masses:
“At length, having come up fifty rods off, he uttered one of those prolonged howls, as if calling on the god of loons to aid him, and immediately there came a wind from the east and rippled the surface, and filled the whole air with misty rain, and I was impressed as if it were the prayer of the loon answered, and his god was angry with me; and so I left him disappearing far away on the tumultuous surface.”
—Henry David Thoreau (1817–1862)
“The masses of the sea
The masses of the sea under
The masses of the infant-bearing sea
Erupt, fountain, and enter to utter for ever
Glory glory glory
The sundering ultimate kingdom of genesis’ thunder.”
—Dylan Thomas (1914–1953)