Mesoscale numerical investigations of air traffic emissions over the North Atlantic during SONEX flight 8: A case study

被引:3
作者
Bieberbach, G
Fuelberg, HE [1 ]
Thompson, AM
Schmitt, A
Hannan, JR
Gregory, GL
Kondo, Y
Knabb, RD
Sachse, GW
Talbot, RW
机构
[1] Florida State Univ, Dept Meteorol, Tallahassee, FL 32306 USA
[2] NASA, Langley Res Ctr, Hampton, VA 23681 USA
[3] Nagoya Univ, Solar Terr Environm Lab, Aichi 442, Japan
[4] Deutsch Zentrum Luft & Raumfahrt, Abt Verkehrsforsch, D-51147 Cologne, Germany
[5] Univ New Hampshire, Inst Study Earth Oceans & Space, Durham, NH 03824 USA
[6] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
关键词
D O I
10.1029/1999JD901036
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Chemical data from flight 8 of NASA's Subsonic Assessment (SASS) Ozone and Nitrogen Oxide Experiment (SONEX) exhibited signatures consistent with aircraft emissions, stratospheric air, and surface-based pollution. These signatures are examined in detail: focusing on the broad aircraft emission signatures that are several hundred kilometers in length. A mesoscale meteorological model provides high-resolution wind data that are used to calculate backward trajectories arriving at locations along the flight track. These trajectories are compared to aircraft locations in the North Atlantic Flight Corridor (NAFC) over a 27-33 hour period. Time series of flight level NO and the number of trajectory/aircraft encounters within the NAFC show excellent agreement. Trajectories arriving within the stratospheric and surface-based pollution regions are found to experience very few aircraft encounters. Conversely, there are many trajectory/aircraft encounters within the two chemical signatures corresponding to aircraft emissions. Even many detailed fluctuations of NO within the two aircraft signature regions correspond to similar fluctuations in aircraft encountered. These NO spikes are due to the superposition of 14 to 25 aircraft plumes transported to the DC-8 flight track during the previous 33 hours. Results confirm that aircraft emissions were responsible for two chemical signatures observed during SONEX flight 8. They also indicate that high-resolution meteorological modeling, when coupled with detailed aircraft location data, is useful for understanding chemical signatures from aircraft emissions at scales of several hundred kilometers.
引用
收藏
页码:3821 / 3832
页数:12
相关论文
共 51 条
[1]  
ANTHES RA, 1977, MON WEATHER REV, V105, P270, DOI 10.1175/1520-0493(1977)105<0270:ACPSUA>2.0.CO
[2]  
2
[3]  
Arakawa A., 1977, Methods of Computational Physics, V17, P173, DOI [10.1016/B978-0-12-460817-7.50009-4, DOI 10.1016/B978-0-12-460817-7.50009-4]
[4]   MEASUREMENTS OF JET AIRCRAFT EMISSIONS AT CRUISE ALTITUDE-I - THE ODD-NITROGEN GASES NO, NO2, HNO2 AND HNO3 [J].
ARNOLD, F ;
SCHEID, J ;
STILP, T ;
SCHLAGER, H ;
REINHARDT, ME .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (24) :2421-2424
[5]   THE EFFECT OF AIRCRAFT EMISSIONS ON TROPOSPHERIC OZONE IN THE NORTHERN-HEMISPHERE [J].
BECK, JP ;
REEVES, CE ;
DELEEUW, FAAM ;
PENKETT, SA .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1992, 26 (01) :17-29
[6]  
BENGTSSON L, 1985, B AM METEOROL SOC, V66, P1133
[7]   Chemical characteristics of air from differing source regions during the Pacific Exploratory Mission-Tropics A (PEM-Tropics A) [J].
Board, AS ;
Fuelberg, HE ;
Gregory, GL ;
Heikes, BG ;
Schultz, MG ;
Blake, DR ;
Dibb, JE ;
Sandholm, ST ;
Talbot, RW .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D13) :16181-16196
[8]   Atmospheric impact of NOx emissions by subsonic aircraft: A three-dimensional model study [J].
Brasseur, GP ;
Muller, JF ;
Granier, C .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D1) :1423-1428
[9]   A general model of how fire emissions and chemistry produce African/oceanic plumes (O-3, CO, PAN, smoke) in TRACE A [J].
Chatfield, RB ;
Vastano, JA ;
Singh, HB ;
Sachse, G .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D19) :24279-24306
[10]  
DOTY KG, 1993, MON WEATHER REV, V121, P387, DOI 10.1175/1520-0493(1993)121<0387:SOTCTT>2.0.CO