Jet Streams

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Contents
  1. Overview
  2. History
  3. Design & Specifications
  4. Operations
  5. See also
  6. References

Overview

Jet streams are fast-flowing, narrow air currents found in the atmosphere, generally located near the altitude of the tropopause and flowing as westerly winds from west to east around the globe. Both the Northern and Southern Hemispheres have a polar jet stream circling their respective polar vortex at around 30,000 feet above sea level, typically traveling around 110 mph, though speeds can be considerably faster under certain conditions. Jet streams have a major practical impact on aviation, since flights traveling with the jet stream can gain substantial speed and fuel savings, while flights traveling against it face longer flight times and higher fuel burn. Airlines and flight planners routinely factor jet stream position and strength into route planning, sometimes choosing longer great-circle paths specifically to take advantage of favorable jet stream tailwinds.

History

Jet streams were first identified by researchers in the early-to-mid 20th century, though their existence wasn't widely understood or confirmed until high-altitude military aircraft during World War II began encountering unexpectedly strong headwinds and tailwinds at cruise altitude. Post-war meteorological research through the 1940s and 1950s mapped jet stream behavior more precisely, establishing the now-standard understanding of polar and subtropical jet streams circling each hemisphere. Commercial aviation began systematically factoring jet stream position into flight planning from the 1950s and 1960s onward, as airlines recognized the substantial fuel and time savings available from routing flights to take advantage of favorable jet stream tailwinds. Modern flight planning systems continue to incorporate real-time and forecast jet stream data, and the practical fuel-saving benefits first recognized in the mid-20th century remain just as relevant to airline route planning today.

Design & Specifications

Jet streams form as narrow, fast-moving air currents near the tropopause, driven by temperature differences between air masses at that altitude.

Operations

Airlines and dispatchers factor jet stream position into route planning, seeking tailwind benefit on eastbound flights and avoiding excessive headwind penalty westbound.

See also

References

Jet Streams
Jet Streams
Photo: NOAA — Public Domain, via Wikimedia Commons
CategoryNavigation, Meteorology & Rules
TypeFast-flowing upper-atmosphere air current
Typical Speed~110 mph
DirectionWest to east
Aviation ImpactMajor fuel/time factor