The North Atlantic Organized Track Structure
The first point to note about the North Atlantic air traffic system is the diurnal pattern of flow. This is strongly tidal, with westbound flow predominant during daylight hours and eastbound flow overnight. There is some traffic which flows against the main stream, particularly during the day, but...
Published in: | Journal of Navigation |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1982
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0373463300021883 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0373463300021883 |
id |
crcambridgeupr:10.1017/s0373463300021883 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0373463300021883 2024-03-03T08:46:58+00:00 The North Atlantic Organized Track Structure Attwooll, V. W. 1982 http://dx.doi.org/10.1017/s0373463300021883 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0373463300021883 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Navigation volume 35, issue 3, page 497-499 ISSN 0373-4633 1469-7785 Ocean Engineering Oceanography journal-article 1982 crcambridgeupr https://doi.org/10.1017/s0373463300021883 2024-02-08T08:46:15Z The first point to note about the North Atlantic air traffic system is the diurnal pattern of flow. This is strongly tidal, with westbound flow predominant during daylight hours and eastbound flow overnight. There is some traffic which flows against the main stream, particularly during the day, but the strong tendency for one-way traffic results from the difference in local times on opposite sides of the ocean, together with the transit times of flight at current speeds. This means that the general pattern will probably persist, unless and until aircraft speeds change radically. Article in Journal/Newspaper North Atlantic Cambridge University Press Journal of Navigation 35 3 497 499 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Ocean Engineering Oceanography |
spellingShingle |
Ocean Engineering Oceanography Attwooll, V. W. The North Atlantic Organized Track Structure |
topic_facet |
Ocean Engineering Oceanography |
description |
The first point to note about the North Atlantic air traffic system is the diurnal pattern of flow. This is strongly tidal, with westbound flow predominant during daylight hours and eastbound flow overnight. There is some traffic which flows against the main stream, particularly during the day, but the strong tendency for one-way traffic results from the difference in local times on opposite sides of the ocean, together with the transit times of flight at current speeds. This means that the general pattern will probably persist, unless and until aircraft speeds change radically. |
format |
Article in Journal/Newspaper |
author |
Attwooll, V. W. |
author_facet |
Attwooll, V. W. |
author_sort |
Attwooll, V. W. |
title |
The North Atlantic Organized Track Structure |
title_short |
The North Atlantic Organized Track Structure |
title_full |
The North Atlantic Organized Track Structure |
title_fullStr |
The North Atlantic Organized Track Structure |
title_full_unstemmed |
The North Atlantic Organized Track Structure |
title_sort |
north atlantic organized track structure |
publisher |
Cambridge University Press (CUP) |
publishDate |
1982 |
url |
http://dx.doi.org/10.1017/s0373463300021883 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0373463300021883 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Journal of Navigation volume 35, issue 3, page 497-499 ISSN 0373-4633 1469-7785 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0373463300021883 |
container_title |
Journal of Navigation |
container_volume |
35 |
container_issue |
3 |
container_start_page |
497 |
op_container_end_page |
499 |
_version_ |
1792503102012653568 |