Explore: Convergence (meteorology)

A convergence zone in meteorology is a region in the atmosphere where two prevailing flows meet and interact, usually resulting in distinctive weather

of the air mass. The movement of the monsoon trough, or Intertropical Convergence Zone, brings rainy seasons to savannah climes. The urban heat island

significance of wind field convergence in tropical weather production in the 1940s and 1950s, the term Intertropical Convergence Zone (ITCZ) was then applied

In meteorology, a low-pressure area (LPA), low area or low is a region where the atmospheric pressure is lower than that of surrounding locations. It

front, or the Intertropical Convergence Zone. When located within a monsoon region, this zone of low pressure and wind convergence is also known as the monsoon

Glossary of Meteorology (2009). "South Atlantic convergence zone". American Meteorological Society. Retrieved 2009-06-05. Glossary of Meteorology (2009).

In meteorology, the synoptic scale (also called the large scale or cyclonic scale) is a horizontal length scale of the order of 1,000 km (620 mi) or more

In meteorology, a cloud is an aerosol consisting of a visible mass of miniature liquid droplets, ice crystals, or other particles, suspended in the atmosphere

of the low. The convergence line ahead of the low became known as either the steering line or the warm front. The trailing convergence zone was referred

In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls from clouds due to gravitational pull. The main