North Atlantic Tracks

North Atlantic Tracks
North Atlantic Tracks for the eastbound crossing on the evening of May 4, 2006

North Atlantic Tracks (NAT) are trans-Atlantic routes that stretch from the northeast of North America to western Europe across the Atlantic Ocean. They ensure aircraft are separated over the ocean, where there is little radar coverage. These heavily-traveled routes are used by aircraft traveling between North America and Europe, flying between the altitudes of 28,500 and 42,000 feet, inclusive. Entrance and movement along these tracks is controlled by special Oceanic Center air traffic controllers to maintain separation between airplanes. The primary purpose of these routes is to provide a Minimum Time Route (MTR). They are aligned in such a way as to minimize any head winds and maximize tail winds impact on the aircraft. This results in much more efficiency by reducing fuel burn and flight time. To make such efficiencies possible, the routes are created daily to take account of the shifting of the winds aloft.

Contents

Route Planning

The specific routing of the tracks are dictated based on a number of factors, the most important being the jetstream - aircraft going to North America from Europe experience headwinds caused by the jetstream. Tracks to Europe use the jetstream to their advantage by routing along the strongest tailwinds. Because of the difference in ground speed caused by the jetstream, westbound flights tend to be longer in duration than their eastbound counterparts. North Atlantic Tracks are published by Shanwick Center (EGGX) and Gander Center (CZQX) in consultation with other adjacent air traffic control agencies and airlines.

Flying the Routes

Prior to departure, airline flight dispatchers/flight operations officers will determine the best track based on destination, aircraft weight, aircraft type, prevailing winds and Air Traffic Control route charges. The aircraft will then contact the Oceanic Center controller before entering oceanic airspace and request the track giving the estimated time of arrival at the entry point. The Oceanic Controllers then calculate the required separation distances between aircraft and issue clearances to the pilots. It may be that the track is not available at that altitude or time so an alternate track or altitude will be assigned. Planes cannot change assigned course or altitude without permission.

Contingency plans exist within the North Atlantic Track system to account for any operational issues that occur. For example, if an aircraft can no longer maintain the speed or altitude it was assigned, the aircraft can move off the track route and fly parallel to its track, but well away from other aircraft. Also, pilots on North Atlantic Tracks are required to inform air traffic control of any deviations in altitude or speed necessitated by avoiding weather, such as thunderstorms or turbulence.

Despite advances in navigation technology, such as GPS and LNAV, errors can and do occur. While typically not dangerous, two aircraft can violate separation requirements. On a busy day, aircraft are spaced approximately 10 minutes apart. With the introduction of TCAS, aircraft traveling along these tracks can monitor the relative position of other aircraft thereby increasing the safety of all track users.

Since there is little radar coverage in the middle of the Atlantic, airplanes must report in as they cross various waypoints along each track, their anticipated crossing time of the next waypoint, and the waypoint after that. These reports enable the Oceanic Controllers to maintain separation between planes. These reports can be made to dispatchers via a satellite communications link (CPDLC) or via High Frequency (HF) radios. In the case of HF reports, each aircraft operates using SELCAL (Selective Calling). The use of SELCAL allows an aircraft crew to be notified of incoming communications even when the aircraft's radio has been muted. Thus, crewmembers need not devote their attention to continuous radio listening. If the aircraft is equipped with Automatic Dependent Surveillance, (ADS-C & ADS-B), voice position reports on HF are no longer necessary, as automatic reports are downlinked. In this case, a SELCAL check only has to be performed when entering the oceanic area and with any change in radio frequency to ensure a working backup system for the event of a datalink failure.

Maximizing Traffic Capacity

Increased aircraft density can be achieved by allowing closer vertical spacing of aircraft through participation in the RVSM program.

Additionally from 10th June 2004 the Strategic Lateral Offset Procedure (SLOP) was introduced to the North Atlantic airspace to reduce the chance of mid-air collision by spreading out aircraft laterally . It reduces the chance of collision for non-normal events such as operational altitude deviation errors and turbulence induced altitude deviations. In essence, the procedure demands that aircraft in North Atlantic airspace fly track centreline or one or two nautical mile offsets to the right of centreline only. However, the choice is left up to the pilot.

The tracks reverse direction twice daily. In the daylight, all traffic on the tracks operates in a westbound flow. At night, the tracks flow eastbound towards Europe. This is done to accommodate traditional airline schedules, with departures from North America to Europe scheduled for departure in the evening thereby allowing passengers to arrive at their destination in the morning. Westbound departures leave Europe mid-day and arrive in North America in the late afternoon. In this manner, a single aircraft can be efficiently utilized by flying to Europe at night and to North America in the day. The tracks are updated daily and their position may alter on the basis of a variety of variable factors, but predominantly due to weather systems.

While the route changes daily, they maintain a series of entrance and exit waypoints which link into the airspace system of North America and Europe. Each route is uniquely identified by a letter of the alphabet. Westbound tracks are indicated with a letter from the start of the alphabet (A, B, C, D, E) and eastbound tracks with a letter from the end (S, T, U, V, W, X, Y). Waypoints on the route are identified by named waypoints (or "fixes") and by the crossing of degrees of latitude and longitude (such as "54/40", indicating 54° latitude, 40° longitude).

The FAA, Nav Canada, NATS and the JAA publish a NOTAM daily with the routes and altitudes to be used in each direction of travel. The current tracks are available online[dead link].

Concorde

Concorde did not travel on the North Atlantic Tracks as it flew to the United States from the United Kingdom and France from a much higher altitude, between 45,000ft and 60,000ft, its relatively high service ceiling. The weather variations at these altitudes were so minor that Concorde followed the same route each day, traveling to and from Europe to North America on fixed tracks. These fixed tracks were known as 'Track Sierra Mike' (SM) and 'Track Sierra Oscar' (SO) for westbound flights and 'Track Sierra November' (SN) for eastbounds. An additional route, 'Track Sierra Papa' (SP), was used for seasonal British Airways flights from London Heathrow to/from Barbados.

See also

External links


Wikimedia Foundation. 2010.

Игры ⚽ Нужна курсовая?

Look at other dictionaries:

  • North Atlantic Tracks — Als North Atlantic Tracks werden die von den zuständigen Funkstationen Shanwick und Gander festgelegten Flugrouten für Linienflüge über den Atlantik bezeichnet. Diese Strecken sichern für Flugzeuge den Überflug des Gebietes ohne permanente… …   Deutsch Wikipedia

  • North Atlantic Tracks — Les North Atlantic Tracks (NAT) ou routes nord Atlantique sont des voies aériennes empruntées par les vols commerciaux qui traversent l Atlantique nord. Elles assurent une séparation entre les avions, au dessus de l océan, là où il n y a pas de… …   Wikipédia en Français

  • North Atlantic tropical cyclone — Tracks of Atlantic tropical cyclones (1851 2005) North Atlantic tropical cyclones usually form in the northern hemisphere summer or fall. Tropical cyclones can be categorized by intensity. Tropical storms have one minute maximum sustained winds… …   Wikipedia

  • North Atlantic Drift (album) — North Atlantic Drift Studio album by Ocean Colour Scene Released July 7 …   Wikipedia

  • North Atlantic oscillation — For the rock band, see North Atlantic Oscillation (band). The North Atlantic oscillation (NAO) is a climatic phenomenon in the North Atlantic Ocean of fluctuations in the difference of atmospheric pressure at sea level between the Icelandic low… …   Wikipedia

  • North Atlantic Track Agreement — The North Atlantic Track Agreement was an agreement in November 1898[1] among 13 passenger steamship companies to use a set series of trans Atlantic routes that stretched from the northeast of North America to western Europe for the Atlantic… …   Wikipedia

  • North America — North American. the northern continent of the Western Hemisphere, extending from Central America to the Arctic Ocean. Highest point, Mt. McKinley, 20,300 ft. (6187 m); lowest, Death Valley, 276 ft. (84 m) below sea level. 400,000,000 including… …   Universalium

  • North Pacific right whale — North Pacific right whale[1] Si …   Wikipedia

  • Atlantic hurricane season — Tracks of all known Atlantic tropical cyclones from 1851 to 2005 For the current season, see 2011 Atlantic hurricane season. The Atlantic hurricane season is the period in a year when hurricanes usually form in the Atlantic Ocean. Tropical… …   Wikipedia

  • Atlantic Avenue–Pacific Street (New York City Subway) — Infobox NYCS name=Atlantic Avenue–Pacific Street accessible=yes bg color=black service=Atlantic Pacific passengers=9.134 million pass year=2006 pass percent=6 connection=LIRR at Flatbush Avenue Access iconAtlantic Avenue–Pacific Street is a New… …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”