Quote:
Originally Posted by Ed's Mountain
I'm not sure a definition based strictly on temperature and precipitation thresholds is sufficient.
To me, a tropical climate is one that is continuously under the influence of synoptic-scale tropical systems. That is to say, the weather is determined by entities such as trade winds, the ICTZ, etc., and it is immune to extra-tropical phenomena such as cold fronts and wave cyclones.
As such I could see a wide variety of different temperature and precipitation regimes being fully tropical.
|
I like this approach, which is closer to the option C, “
A low latitude climate above a specific precipitation threshold, no matter the temperature”. In such case, the necessary influence of the ITCZ translates into at least a significant amount of precipitation, whereas diversity of elevation can provide a wide range of temperatures.
Under this precept, we can say that any place devoid of tropical convergence has not a tropical climate (i.e. any hot desert, which is ruled by the subtropical highs), whereas any place who does have tropical influence during the high-sun season but its influenced by extratropical convergence the rest of the year has not a tropical climate either (i.e. the Eastern side of landmasses just above the tropics).
So tropical climates branch off in two directions: dry
subtropical climates ("west side" climates) and wet
subtropical climates ("east side" climates).