Asia Tropical Weather Locales.

Due to the location of the Southern Asian regions nearer the equator and the lack of a temperature gradient there exists in south Asia a large consistent area of heated land masses and sea surface waters known as the Tropical regions. As the temperature gradient lacks in the southern area no weather fronts form and weather is created via tropical weather anomolies.

• Weak mid level troughs.
• Convective systems.
• Tropical disturbances.
• Monsoon systems.
• Trough inversions.

This creates a weather pattern built on the tropical disturbance and monsoonal patterns of which torrential rains, quick forming storms, and formidable Typhoons and the lesser cousin the Tropical Storm may sprout in the southern Asia areas.

In heatwaves Hot Dry weather or Hot Humid weather may be experienced as the large equatorial area provides a region adept at Solar Heating. The heated water temperature and evaporation of sea areas also assists in creating weather in weak trough regions or tropical low pressure centers helped by wind transportation and regular tropical weather patterns.