Comparisons of box model calculations and measurements of formaldehyde from the 1997 North Atlantic Regional Experiment -: art. no. 4060

被引:31
作者
Frost, GJ
Fried, A
Lee, YN
Wert, B
Henry, B
Drummond, JR
Evans, MJ
Fehsenfeld, FC
Goldan, PD
Holloway, JS
Hübler, G
Jakoubek, R
Jobson, BT
Knapp, K
Kuster, WC
Roberts, J
Rudolph, J
Ryerson, TB
Stohl, A
Stroud, C
Sueper, DT
Trainer, M
Williams, J
机构
[1] NOAA, Aeron Lab, Boulder, CO 80303 USA
[2] Univ Toronto, Dept Phys, Toronto, ON M5S 1A1, Canada
[3] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
[4] NCAR, Div Atmospher Chem, Boulder, CO 80305 USA
[5] Pacific NW Natl Lab, Richland, WA 99352 USA
[6] Penn State Univ, Dept Chem, York, PA 17403 USA
[7] Brookhaven Natl Lab, Environm Chem Div, Upton, NY 11973 USA
[8] York Univ, Dept Chem, Ctr Atmospher Chem, N York, ON M3J 1P3, Canada
[9] Tech Univ Munich, Lehrstuhl Bioklimatol & Immissionsforsch, D-85354 Munich, Germany
[10] Max Planck Inst Chem, Abt Chem Atmosphare, D-55020 Mainz, Germany
[11] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[12] Univ Colorado, Dept Chem, Boulder, CO 80309 USA
关键词
formaldehyde; photochemical modeling; aircraft measurements; North Atlantic troposphere;
D O I
10.1029/2001JD000896
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] Formaldehyde (CH2O) measurements from two independent instruments are compared with photochemical box model calculations. The measurements were made on the National Oceanic and Atmospheric Administration P-3 aircraft as part of the 1997 North Atlantic Regional Experiment (NARE 97). The data set considered here consists of air masses sampled between 0 and 8 km over the North Atlantic Ocean which do not show recent influence from emissions or transport. These air masses therefore should be in photochemical steady state with respect to CH2O when constrained by the other P-3 measurements, and methane oxidation was expected to be the predominant source of CH2O in these air masses. For this data set both instruments measured identical CH2O concentrations to within 40 parts per trillion by volume (pptv) on average over the 0-800 pptv range, although differences larger than the combined 2 total uncertainty estimates were observed between the two instruments in 11% of the data. Both instruments produced higher CH2O concentrations than the model in more than 90% of this data set, with a median measured-modeled [CH2O] difference of 0.13 or 0.18 ppbv (depending on the instrument), or about a factor of 2. Such large differences cannot be accounted for by varying model input parameters within their respective uncertainty ranges. After examining the possible reasons for the model-measurement discrepancy, we conclude that there are probably one or more additional unknown sources of CH2O in the North Atlantic troposphere.
引用
收藏
页码:15 / 1
页数:12
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