Formaldehyde methods comparison in the remote lower troposphere during the Mauna Loa photochemistry experiment 2

被引:39
|
作者
Heikes, B
McCully, B
Zhou, X
Lee, YN
Mopper, K
Chen, X
Mackay, G
Karecki, D
Schiff, H
Campos, T
Atlas, E
机构
[1] BROOKHAVEN NATL LAB, DIV ENVIRONM CHEM, UPTON, NY 11973 USA
[2] WASHINGTON STATE UNIV, DEPT CHEM, PULLMAN, WA 99164 USA
[3] UNISEARCH ASSOCIATES INC, CONCORD, ON, CANADA
[4] NATL CTR ATMOSPHER RES, BOULDER, CO 80307 USA
关键词
D O I
10.1029/96JD00550
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Five methods for the measurement of CH2O vapor were compared under remote tropospheric conditions. The techniques included an aqueous-scrubber enzyme fluorescence method (URIcoil), TDLAS (UNI), 2,4-dinitrophenylhydrazine (DNPH) impregnated-cartridges (BNL/WSUcart), an aqueous-scrubber DNPH mettled (BNL/WSUcoil), and an unpublished aqueous-scrubber immobilized-enzyme fluorescence method (NCARbound). This was part of the Mauna Loa Observatory Photochemistry Experiment 2 (MLOPEX 2) which was performed in four similar to 30-day intensives. In MLOPEX 2a (fall 1991), the URIcoil technique indicated higher concentrations relative to the BNL/WSUcoil which were higher than UNI. The limited number of NCARbound measurements for MLOPEX 2a were greater than the other measurements and least reliable. During MLOPEX 2b (winter 1992), URIcoil, UNI, BNL/WSUcoil, and NCAR-bound gave comparable measurements of CH2O with the latter again being consistently higher than the first three methods and its performance and reliability was improved over MLOPEX 2a. URIcoil and BNL/WSUcoil were comparable in MLOPEX 2c (spring 1992) and 2d (summer 1992), whereas, BNL/WSUcart was consistently higher than both for these intensives. The major source of difference between techniques was ascribed to variations in the analytical-procedural field blanks. Calibration differences were the most likely cause of URIcoil being higher than BNL/WSUcoil and BNL/WSUcoil being higher than UNI during MLOPEX 2a. Lower free troposphere median concentrations were between 100 and 150 ppt for all seasons and without a seasonal trend. These values were a factor of 2 to 3 lower than model estimates for this study site and were in keeping with earlier work.
引用
收藏
页码:14741 / 14755
页数:15
相关论文
共 50 条
  • [41] Global water vapour distribution in the upper troposphere and lower stratosphere during CRISTA 2
    Schaeler, B.
    Offermann, D.
    Kuell, V.
    Jarisch, M.
    ADVANCES IN SPACE RESEARCH, 2009, 43 (01) : 65 - 73
  • [42] Comparison of in situ N2O and CH4 measurements in the upper troposphere and lower stratosphere during STRAT and POLARIS
    Hurst, DF
    Dutton, GS
    Romashkin, PA
    Elkins, JW
    Herman, RL
    Moyer, EJ
    Scott, DC
    May, RD
    Webster, CR
    Grecu, J
    Loewenstein, M
    Podolske, JR
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D15) : 19811 - 19822
  • [43] COMPARISON OF 2 SAMPLING METHODS FOR DETERMINING FORMALDEHYDE CONCENTRATIONS IN WORKPLACE AIR
    KUCHENBECKER, D
    GRAU, H
    SCHAFFERNICHT, H
    STAUB REINHALTUNG DER LUFT, 1993, 53 (04): : 143 - 145
  • [44] COMPARISON OF THREE DIFFERENT METHODS FOR BREATHING MEASURE DURING A PSYCHOPHYSIOLOGICAL EXPERIMENT
    Cardoso, Thiago Lopes
    Soares, Rita Alves
    Garcia, Mirtes Pereira
    Caetano, Frederico Jandre
    Giannella-Neto, Antonio
    PSYCHOPHYSIOLOGY, 2011, 48 : S67 - S67
  • [45] Estimate of bias in Aura TES HDO/H2O profiles from comparison of TES and in situ HDO/H2O measurements at the Mauna Loa observatory
    Worden, J.
    Noone, D.
    Galewsky, J.
    Bailey, A.
    Bowman, K.
    Brown, D.
    Hurley, J.
    Kulawik, S.
    Lee, J.
    Strong, M.
    ATMOSPHERIC CHEMISTRY AND PHYSICS, 2011, 11 (09) : 4491 - 4503
  • [46] Measurement of HO2NO2 in the free troposphere during the intercontinental chemical transport experiment -: North America 2004
    Kim, S.
    Huey, L. G.
    Stickel, R. E.
    Tanner, D. J.
    Crawford, J. H.
    Olson, J. R.
    Chen, G.
    Brune, W. H.
    Ren, X.
    Lesher, R.
    Wooldridge, P. J.
    Bertram, T. H.
    Perring, A.
    Cohen, R. C.
    Lefer, B. L.
    Shetter, R. E.
    Avery, M.
    Diskin, G.
    Sokolik, I.
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2007, 112 (D12)
  • [47] Aerosol particle chemical characteristics measured from aircraft in the lower troposphere during ACE-2
    Schmeling, M
    Russell, LM
    Erlick, C
    Collins, DR
    Jonsson, H
    Wang, Q
    Kregsamer, P
    Streli, C
    TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02): : 185 - 200
  • [48] MEASUREMENT OF FORMALDEHYDE AND ACETALDEHYDE USING 2,4-DINITROPHENYLHYDRAZINE-IMPREGNATED CARTRIDGES DURING THE CARBONACEOUS SPECIES METHODS COMPARISON STUDY
    FUNG, K
    WRIGHT, B
    AEROSOL SCIENCE AND TECHNOLOGY, 1990, 12 (01) : 44 - 48
  • [49] COMPARISON OF 2 METHODS OF PERFORMING THELLIER-EXPERIMENT (OR, HOW THELLIER EXPERIMENT SHOULD NOT BE DONE)
    LEVI, S
    JOURNAL OF GEOMAGNETISM AND GEOELECTRICITY, 1975, 27 (03): : 245 - 255
  • [50] Lidar observations of the middle atmospheric thermal tides and comparison with the High Resolution Doppler Imager and Global Scale Wave Model 2.: October observations at Mauna Loa (19.5°N)
    Leblanc, T
    McDermid, IS
    Ortland, DA
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D10) : 11931 - 11938