the jet stream
A "front" is the interface between two air masses of different temperature.
Polar air masses are cooler than tropical air masses because they originate from high-latitude regions closer to the poles, where temperatures are generally colder. Conversely, tropical air masses originate from low-latitude regions near the equator, where temperatures are generally warmer. This temperature difference between the two regions accounts for the inherent temperature contrast between polar and tropical air masses.
the continental air is found in high temperature regions. the maritime air is found in low temperature regions.
Density differences is usually what would keep air masses separate.
Air currents are caused by the sun's uneven heating of the earth, Water Currents (mostly known as Ocean Currents) are generated by wind, density differs in water masses causes by temperature and salinity variations,gravity, and also events such as earthquakes
Jet Stream
Differences of atmospheric pressures or differences of temperatures of adjacent air masses.
air masses with different characteristics such as temperature and humidity do not usually mix. so when two different air masses meet a boundary forms between them.
A front, or boundary between two air masses, is typically characterized by clouds and precipitation. The amount and type of precipitation typically depends on the temperature and moisture difference between the two air masses. Generally speaking, stronger temperature/moisture differences mean more clouds and precipitation.
When two masses that have a difference in air pressure meets they will create a storm front. When the differences in air pressure between the two masses increase the severity of the storm created will intensify.
The wind is the movement of air masses due the differences in air pressure or air temperature.
The wind is the movement of air masses due the differences in air pressure or air temperature.
two air masses with large differences in the air pressure are near one another. what weather conditions will most likely exist between the two air masses
Continentality: the relationship between land masses (continents) and ocean bodies and the differences in temperature that are produced. Areas located in the interior of a continent are more likely to have greater temperature ranges and possibly drier conditions compared to maritime locations (land next to ocean). Because solar radiation heats land faster than water, Continentality causes greater extremes in both temperature and precipitation the farther inland an area is. This causes localized as well as global effects on weather patterns
global winds
A "front" is the interface between two air masses of different temperature.
Tides are caused by the gravitational attraction of the Moon. The tides interact with the continental plates to form currents, which can also be created or altered by temperature differences in the sea. Winds are caused by the motion of air masses when the atmosphere is heated by the Sun, or cooled by colder land and ice surfaces. Air masses are also steered by the spinning of the Earth.