Search from over 60,000 research works

Advanced Search

Impact of the North Atlantic Oscillation on transatlantic flight routes and clear-air turbulence

[thumbnail of jamc-d-15-0261%2E1.pdf]
Preview
jamc-d-15-0261%2E1.pdf - Published Version (1MB) | Preview
[thumbnail of JAMC-D-15-0261_R2.fnl.7-35.pdf]
Preview
JAMC-D-15-0261_R2.fnl.7-35.pdf - Accepted Version (3MB) | Preview
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Kim, J.-H., Chan, W. N., Sridhar, B., Sharman, R. D., Williams, P. D. orcid id iconORCID: https://orcid.org/0000-0002-9713-9820 and Strahan, M. (2016) Impact of the North Atlantic Oscillation on transatlantic flight routes and clear-air turbulence. Journal of Applied Meteorology and Climatology, 55 (3). pp. 763-771. ISSN 1558-8432 doi: 10.1175/JAMC-D-15-0261.1

Abstract/Summary

The variation of wind-optimal transatlantic flight routes and their turbulence potential is investigated to understand how upper-level winds and large-scale flow patterns can affect the efficiency and safety of long-haul flights. In this study, the wind-optimal routes (WORs) that minimize the total flight time by considering wind variations are modeled for flights between John F. Kennedy International Airport (JFK) in New York, New York, and Heathrow Airport (LHR) in London, United Kingdom, during two distinct winter periods of abnormally high and low phases of North Atlantic Oscillation (NAO) teleconnection patterns. Eastbound WORs approximate the JFK–LHR great circle (GC) route following northerly shifted jets in the +NAO period. Those WORs deviate southward following southerly shifted jets during the −NAO period, because eastbound WORs fly closely to the prevailing westerly jets to maximize tailwinds. Westbound WORs, however, spread meridionally to avoid the jets near the GC in the +NAO period to minimize headwinds. In the −NAO period, westbound WORs are north of the GC because of the southerly shifted jets. Consequently, eastbound WORs are faster but have higher probabilities of encountering clear-air turbulence than westbound ones, because eastbound WORs are close to the jet streams, especially near the cyclonic shear side of the jets in the northern (southern) part of the GC in the +NAO (−NAO) period. This study suggests how predicted teleconnection weather patterns can be used for long-haul strategic flight planning, ultimately contributing to minimizing aviation’s impact on the environment

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/59457
Item Type Article
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > NCAS
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher American Meteorological Society
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar