z-logo
open-access-imgOpen Access
Measurements of excess O 3 , CO 2 , CO, CH 4 , C 2 H 4 , C 2 H 2 , HCN, NO, NH 3 , HCOOH, CH 3 COOH, HCHO, and CH 3 OH in 1997 Alaskan biomass burning plumes by airborne Fourier transform infrared spectroscopy (AFTIR)
Author(s) -
Goode Jon G.,
Yokelson Robert J.,
Ward Darold E.,
Susott Ronald A.,
Babbitt Ronald E.,
Davies Mary Ann,
Hao Wei Min
Publication year - 2000
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2000jd900287
Subject(s) - carbon monoxide , formaldehyde , trace gas , formic acid , plume , analytical chemistry (journal) , methanol , carbon dioxide , ozone , mixing ratio , nitrogen dioxide , chemistry , environmental chemistry , meteorology , physics , catalysis , biochemistry , chromatography , organic chemistry
We used an airborne Fourier transform infrared spectrometer (AFTIR), coupled to a flow‐through, air‐sampling cell, on a King Air B‐90 to make in situ trace gas measurements in isolated smoke plumes from four, large, boreal zone wildfires in interior Alaska during June 1997. AFTIR spectra acquired near the source of the smoke plumes yielded excess mixing ratios for 13 of the most common trace gases: water, carbon dioxide, carbon monoxide, methane, nitric oxide, formaldehyde, acetic acid, formic acid, methanol, ethylene, acetylene, ammonia and hydrogen cyanide. Emission ratios to carbon monoxide for formaldehyde, acetic acid, and methanol were 2.2±0.4%, 1.3±0.4%, and 1.4±0.1%, respectively. For each oxygenated organic compound, a single linear equation fits our emission factors from Alaska, North Carolina, and laboratory fires as a function of modified combustion efficiency (MCE). A linear equation for predicting the NH 3 /NO x emission ratio as a function of MCE fits our Alaskan AFTIR results and those from many other studies. AFTIR spectra collected in downwind smoke that had aged 2.2±1 hours in the upper, early plume yielded ΔO 3 /ΔCO ratios of 7.9±2.4% resulting from O 3 production rates of ∼50 ppbv h −1 . The ΔNH 3 /ΔCO ratio in another plume decreased to 1/ e of its initial value in ∼2.5 hours. A set of average emission ratios and emission factors for fires in Alaskan boreal forests is derived. We estimate that the 1997 Alaskan fires emitted 46±11 Tg of CO 2 .

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom