The dependence of minimum‐time routes over the North Atlantic on cruise altitude

North Atlantic air traffic is broadly organized into a track system: daily sets of tracks are defined by air traffic control, which are vertically stacked, such that the same set of tracks is used for all flight levels (FLs), regardless of any vertical variations in wind. The present paper uses mini...

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Published in:Meteorological Applications
Main Authors: Mangini, Fabio, Irvine, Emma A., Shine, Keith P., Stringer, Marc A.
Other Authors: Natural Environment Research Council
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2018
Subjects:
Online Access:http://dx.doi.org/10.1002/met.1733
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spelling crwiley:10.1002/met.1733 2024-06-02T08:11:06+00:00 The dependence of minimum‐time routes over the North Atlantic on cruise altitude Mangini, Fabio Irvine, Emma A. Shine, Keith P. Stringer, Marc A. Natural Environment Research Council 2018 http://dx.doi.org/10.1002/met.1733 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fmet.1733 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.1733 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Meteorological Applications volume 25, issue 4, page 655-664 ISSN 1350-4827 1469-8080 journal-article 2018 crwiley https://doi.org/10.1002/met.1733 2024-05-03T11:41:50Z North Atlantic air traffic is broadly organized into a track system: daily sets of tracks are defined by air traffic control, which are vertically stacked, such that the same set of tracks is used for all flight levels (FLs), regardless of any vertical variations in wind. The present paper uses minimum‐time routes, previously shown to be a good proxy for the location of the North Atlantic track system, to understand whether vertical variations in wind speed and direction significantly affect minimum‐time routes optimized at different altitudes. It does so to examine whether (all other factors assumed equal) there is potential for improvements in fuel efficiency. The optimum cruise altitude over the North Atlantic is determined, focusing on the New York–London route. It is found that eastbound routes, which take advantage of the jet stream, are on average faster at 250 hPa (FL340) than at 300 hPa (FL300) or 200 hPa (FL390) by approximately 2 min (compared with the annual mean route time of about 330 min, assuming a true air speed of 250 m/s). For westbound routes, the route time increases with height: aircraft flying at 300 hPa are on average 3 min faster than at higher levels (the annual mean optimum time being about 400 min). These estimates are compared with the time penalty that arises from flying a route optimized at 250 hPa at the other two altitudes. The time penalty is generally less than 1 min compared with the minimum‐time routes calculated at those altitudes. Article in Journal/Newspaper North Atlantic Wiley Online Library Meteorological Applications 25 4 655 664
institution Open Polar
collection Wiley Online Library
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language English
description North Atlantic air traffic is broadly organized into a track system: daily sets of tracks are defined by air traffic control, which are vertically stacked, such that the same set of tracks is used for all flight levels (FLs), regardless of any vertical variations in wind. The present paper uses minimum‐time routes, previously shown to be a good proxy for the location of the North Atlantic track system, to understand whether vertical variations in wind speed and direction significantly affect minimum‐time routes optimized at different altitudes. It does so to examine whether (all other factors assumed equal) there is potential for improvements in fuel efficiency. The optimum cruise altitude over the North Atlantic is determined, focusing on the New York–London route. It is found that eastbound routes, which take advantage of the jet stream, are on average faster at 250 hPa (FL340) than at 300 hPa (FL300) or 200 hPa (FL390) by approximately 2 min (compared with the annual mean route time of about 330 min, assuming a true air speed of 250 m/s). For westbound routes, the route time increases with height: aircraft flying at 300 hPa are on average 3 min faster than at higher levels (the annual mean optimum time being about 400 min). These estimates are compared with the time penalty that arises from flying a route optimized at 250 hPa at the other two altitudes. The time penalty is generally less than 1 min compared with the minimum‐time routes calculated at those altitudes.
author2 Natural Environment Research Council
format Article in Journal/Newspaper
author Mangini, Fabio
Irvine, Emma A.
Shine, Keith P.
Stringer, Marc A.
spellingShingle Mangini, Fabio
Irvine, Emma A.
Shine, Keith P.
Stringer, Marc A.
The dependence of minimum‐time routes over the North Atlantic on cruise altitude
author_facet Mangini, Fabio
Irvine, Emma A.
Shine, Keith P.
Stringer, Marc A.
author_sort Mangini, Fabio
title The dependence of minimum‐time routes over the North Atlantic on cruise altitude
title_short The dependence of minimum‐time routes over the North Atlantic on cruise altitude
title_full The dependence of minimum‐time routes over the North Atlantic on cruise altitude
title_fullStr The dependence of minimum‐time routes over the North Atlantic on cruise altitude
title_full_unstemmed The dependence of minimum‐time routes over the North Atlantic on cruise altitude
title_sort dependence of minimum‐time routes over the north atlantic on cruise altitude
publisher Wiley
publishDate 2018
url http://dx.doi.org/10.1002/met.1733
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fmet.1733
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.1733
genre North Atlantic
genre_facet North Atlantic
op_source Meteorological Applications
volume 25, issue 4, page 655-664
ISSN 1350-4827 1469-8080
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/met.1733
container_title Meteorological Applications
container_volume 25
container_issue 4
container_start_page 655
op_container_end_page 664
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