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MLS Scientific Publication Scientific Themes: Atmospheric composition, Atmospheric dynamics, Biomass burning, Methyl Cyanide, Convection, Remote Sounding. Enhancements in lower stratospheric CH 3 CN observed by the Upper Atmosphere Research Satellite Microwave Limb Sounder following boreal forest fires. Nathaniel J. Livesey, Michael D. Fromm, Joe W. Waters, Gloria L. Manney, Michelle L. Santee, and William G. Read. J. Geophys. Res., 109 (D06308), doi:10.1029/2003JD004055, 2004 First author: Nathaniel J. Livesey, [email protected], +1 818 354 4214. Summary 100 hPa 25 August 1992 60W 70W 80W 90W 100W 20N 30N 40N 400 600 800 1000 1200 1400 CH 3 CN / pptv Figure 2 (subset): Observed enhance- ment in lower stratospheric CH 3 CN ob- served by MLS. Typical values at these altitudes are around 30 pptv. This paper describes the observation and interpretation of an unusual enhance- ment in lower stratospheric CH 3 CN (methyl cyanide, also known as acetoni- trile) off the coast of Florida over the period 25–30 August 1992 made by the Microwave Limb Sounder (MLS) on the Upper Atmosphere Research Satellite (UARS). The enhancement appeared suddenly in the MLS data on 25 August, after which it was carried westward, consistent with trajectory calculations, and dispersed. The paper discusses three theories for the possible origin of the event. The first two (a link to a failed rocket launch, and a link to the earlier eruption of Mount Spurr in Alaska) are ruled out. The strongest hypothesis for the origin of the enhancement relates it to a boreal forest fire near Boise Idaho. Biomass burning is known to be the dominant source of CH 3 CN in the atmosphere. During this period MLS made no observations north of 34 N, so the region of the fire was unobserved, and it is impossible to tell from the MLS data alone the true extent of the enhancement. The Total Ozone Mapping Spectrometer (TOMS) aerosol observations for the days preceding the fire show a sudden significant enhancement, extending over much of the United States and Canada on 22 August. The paper suggests that this enhancement represents smoke and soot from the Boise fires. A study of the wind fields indicates that this aerosol enhancement must have been located in the lower stratosphere. 21-Aug 22-Aug 23-Aug 24-Aug 60W 70W 80W 90W 100W 110W 120W 130W 140W 40N 50N 60N 19 20 21 22 23 August 1992 Figure 8: TOMS aerosol enhancements prior to the MLS CH 3 CN enhancement. The enhancement seen on 22 August is thought to be due to forest fires in Boise Idaho at the time (features over the Pacific on 19, 20 and 21 August are related to the Mount Spurr eruption on 18 August). The red lines in- dicate backward trajectories from the location and time first enhanced MLS CH 3 CN at 100 hPa shown above. The paper proposes that polluted air in the region of the forest fire was transported to the lower stratosphere by convec- tive activity associated with a strong series of thunderstorms in the region. Image data from the Advanced Very High Reso- lution Radiometer (AVHRR) show both the smoke associated with the fires and, later, clouds associated with strong thunder- storms whose tops are at the tropopause. Observations of such enhancement events are not unprece- dented, though so far only a handful or so of similar events have been documented in the literature. The understanding of the nature, frequency and importance of these events is still in its early stages. No other events of comparable magnitude are seen in the multi-year MLS data. However many tropopause penetration events may go unobserved by MLS as they are not associated with heavily polluted air.

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Page 1: MLS Scientic Publication Scientic Themes: Atmospheric …mls.jpl.nasa.gov/joe/onepagesummary-ch3cnevent.pdf · MLS Scientic Publication Scientic Themes: Atmospheric composition, Atmospheric

MLS Scientific PublicationScientific Themes: Atmospheric composition, Atmospheric dynamics, Biomass burning,

Methyl Cyanide, Convection, Remote Sounding.

Enhancements in lower stratospheric CH3CN observed by the Upper Atmosphere Research SatelliteMicrowave Limb Sounder following boreal forest fires.Nathaniel J. Livesey, Michael D. Fromm, Joe W. Waters, Gloria L. Manney, Michelle L. Santee, andWilliam G. Read.J. Geophys. Res., 109 (D06308), doi:10.1029/2003JD004055, 2004First author: Nathaniel J. Livesey, [email protected], +1 818 354 4214.

Summary

100 hPa

25 August 1992

60W70W80W90W100W

20N

30N

40N

68 hPa

25 August 1992

60W70W80W90W100W

20N

30N

40N

26 August 1992

60W70W80W90W100W

20N

30N

40N

26 August 1992

60W70W80W90W100W

20N

30N

40N

27 August 1992

60W70W80W90W100W

20N

30N

40N

27 August 1992

60W70W80W90W100W

20N

30N

40N

28 August 1992

60W70W80W90W100W

20N

30N

40N

28 August 1992

60W70W80W90W100W

20N

30N

40N

29 August 1992

60W70W80W90W100W

20N

30N

40N

29 August 1992

60W70W80W90W100W

20N

30N

40N

30 August 1992

60W70W80W90W100W

20N

30N

40N

30 August 1992

60W70W80W90W100W

20N

30N

40N

400 600 800 1000 1200 1400 CH3CN / pptv

100 hPa

25 August 1992

60W70W80W90W100W

20N

30N

40N

68 hPa

25 August 1992

60W70W80W90W100W

20N

30N

40N

26 August 1992

60W70W80W90W100W

20N

30N

40N

26 August 1992

60W70W80W90W100W

20N

30N

40N

27 August 1992

60W70W80W90W100W

20N

30N

40N

27 August 1992

60W70W80W90W100W

20N

30N

40N

28 August 1992

60W70W80W90W100W

20N

30N

40N

28 August 1992

60W70W80W90W100W

20N

30N

40N

29 August 1992

60W70W80W90W100W

20N

30N

40N

29 August 1992

60W70W80W90W100W

20N

30N

40N

30 August 1992

60W70W80W90W100W

20N

30N

40N

30 August 1992

60W70W80W90W100W

20N

30N

40N

400 600 800 1000 1200 1400 CH3CN / pptv

Figure 2 (subset): Observed enhance-ment in lower stratospheric CH3CN ob-served by MLS. Typical values at thesealtitudes are around 30 pptv.

This paper describes the observation and interpretation of an unusual enhance-ment in lower stratospheric CH3CN (methyl cyanide, also known as acetoni-trile) off the coast of Florida over the period 25–30 August 1992 made by theMicrowave Limb Sounder (MLS) on the Upper Atmosphere Research Satellite(UARS). The enhancement appeared suddenly in the MLS data on 25 August,after which it was carried westward, consistent with trajectory calculations, anddispersed.

The paper discusses three theories for the possible origin of the event. Thefirst two (a link to a failed rocket launch, and a link to the earlier eruption ofMount Spurr in Alaska) are ruled out. The strongest hypothesis for the originof the enhancement relates it to a boreal forest fire near Boise Idaho. Biomassburning is known to be the dominant source of CH3CN in the atmosphere.During this period MLS made no observations north of 34◦N, so the region ofthe fire was unobserved, and it is impossible to tell from the MLS data alonethe true extent of the enhancement.

The Total Ozone Mapping Spectrometer (TOMS) aerosol observations forthe days preceding the fire show a sudden significant enhancement, extending over much of the United States andCanada on 22 August. The paper suggests that this enhancement represents smoke and soot from the Boise fires. Astudy of the wind fields indicates that this aerosol enhancement must have been located in the lower stratosphere.

21-Aug

22-Aug23-Aug

24-Aug

60W70W80W90W100W110W120W130W140W

40N

50N

60N

19 20 21 22 23August 1992

Figure 8: TOMS aerosol enhancements prior to the MLSCH3CN enhancement. The enhancement seen on 22 Augustis thought to be due to forest fires in Boise Idaho at the time(features over the Pacific on 19, 20 and 21 August are relatedto the Mount Spurr eruption on 18 August). The red lines in-dicate backward trajectories from the location and time firstenhanced MLS CH3CN at 100 hPa shown above.

The paper proposes that polluted air in the region of theforest fire was transported to the lower stratosphere by convec-tive activity associated with a strong series of thunderstormsin the region. Image data from the Advanced Very High Reso-lution Radiometer (AVHRR) show both the smoke associatedwith the fires and, later, clouds associated with strong thunder-storms whose tops are at the tropopause.

Observations of such enhancement events are not unprece-dented, though so far only a handful or so of similar eventshave been documented in the literature. The understanding ofthe nature, frequency and importance of these events is still inits early stages. No other events of comparable magnitude areseen in the multi-year MLS data. However many tropopausepenetration events may go unobserved by MLS as they are notassociated with heavily polluted air.