Inflow (meteorology)
Inflow is the flow of a fluid into a large collection of that fluid.[1] In meteorology, inflow normally means the influx (entry) of warmth and moisture from air within the Earth's atmosphere into storm systems. Extratropical cyclones are created by inflow focused along their cold front and warm fronts. Tropical cyclones need a large inflow of warmth and moisture from warm oceans to become very powerful, mainly within the lowest 1 kilometre (0.62 mi) of the atmosphere. Once the thunderstorms and their associated tornadoes do not get the flow of warm and moist air, the storms begin to dissipate.
Inflow (meteorology) Media
Airflow in and around a supercell with the inflow at the base on right.
Hurricane Isabel (2003) as seen from the International Space Station.
Structure of a tropical cyclone with inflow in red.
A weather map of an extratropical cyclone affecting Great Britain and Ireland. The "L" symbol denotes the center of the "low", and the occluded, cold, and warm frontal boundaries are depicted.
Related pages
References
- ↑ Glossary of Meteorology (June 2000). "Inflow". American Meteorological Society. Archived from the original on 2011-06-06. Retrieved 2009-11-22.
