In situ aerosol-size distributions and clear-column radiative closure during ACE-2

被引:86
|
作者
Collins, DR
Jonsson, HH
Seinfeld, JH
Flagan, RC
Gassó, S
Hegg, DA
Russell, PB
Schmid, B
Livingston, JM
Öström, E
Noone, KJ
Russell, LM
Putaud, JP
机构
[1] CALTECH, Pasadena, CA 91125 USA
[2] USN, Postgrad Sch, Monterey, CA USA
[3] Univ Washington, Seattle, WA 98195 USA
[4] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA
[5] Bay Area Environm Res Inst, San Francisco, CA USA
[6] SRI Int, Menlo Park, CA 94025 USA
[7] Stockholm Univ, S-10691 Stockholm, Sweden
[8] Princeton Univ, Princeton, NJ 08544 USA
[9] Joint Res Ctr, Ispra, Italy
关键词
D O I
10.1034/j.1600-0889.2000.00008.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
As part of the second Aerosol Characterization Experiment (ACE-2) during June and July of 1997, aerosol-size distributions were measured on board the CIRPAS Pelican aircraft through the use of a DMA and 2 OPCs. During the campaign, the boundary-layer aerosol typically possessed characteristics representative of a background marine aerosol or a continentally influenced aerosol, while the free-tropospheric aerosol was characterized by the presence or absence of a Saharan dust layer. A range of radiative closure comparisons were made using the data obtained during vertical profiles flown on 4 missions. Of particular interest here are the comparisons made between the optical properties as determined through the use of measured aerosol-size distributions and those measured directly by an airborne 14-wavelength sunphotometer and 3 nephelometers. Variations in the relative humidity associated with each of the direct measurements required consideration of the hygroscopic properties of the aerosol for size-distribution-based calculations. Simultaneous comparison with such a wide range of directly-measured optical parameters not only offers evidence of the validity of the physicochemical description of the aerosol when closure is achieved, but also provides insight into potential sources of error when some or all of the comparisons result in disagreement. Agreement between the derived and directly-measured optical properties varied for different measurements and for different cases. Averaged over the 4 case studies, the derived extinction coefficient at 525 nm exceeded that measured by the sunphotometer by 2.5% in the clean boundary layer, but underestimated measurements by 13% during pollution events. For measurements within the free troposphere, the mean derived extinction coefficient was 3.3% and 17% less than that measured by the sunphotometer during dusty and non-dusty conditions, respectively. Likewise, averaged discrepancies between the derived and measured scattering coefficient were -9.6%, +4.7%, +17%, and -41% for measurements within the clean boundary layer, polluted boundary layer, free troposphere with a dust layer, and free troposphere without a dust layer, respectively. Each of these quantities, as well as the majority of the > 100 individual comparisons from which they were averaged, were within estimated uncertainties.
引用
收藏
页码:498 / 525
页数:28
相关论文
共 50 条
  • [1] An overview of the ACE-2 clear sky column closure experiment (CLEARCOLUMN)
    Russell, PB
    Heintzenberg, J
    TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02) : 463 - 483
  • [2] Point and column aerosol radiative closure during ACE 1: Effects of particle shape and size
    Fridlind, AM
    Jacobson, MZ
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D3)
  • [3] Clear-column radiative closure during ACE-Asia: Comparison of multiwavelength extinction derived from particle size and composition with results from Sun photometry
    Wang, J
    Flagan, RC
    Seinfeld, JH
    Jonsson, HH
    Collins, DR
    Russell, PB
    Schmid, B
    Redemann, J
    Livingston, JM
    Gao, S
    Hegg, DA
    Welton, EJ
    Bates, D
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D23)
  • [4] ON DISTINGUISHING BETWEEN 2 AEROSOL-SIZE DISTRIBUTIONS
    COOPER, DW
    AEROSOL SCIENCE AND TECHNOLOGY, 1992, 16 (03) : 205 - 206
  • [5] Clear-column closure studies of aerosols and water vapor aboard the NCAR C-130 during ACE-Asia, 2001
    Redemann, J
    Masonis, SJ
    Schmid, B
    Anderson, TL
    Russell, PB
    Livingston, JM
    Dubovik, O
    Clarke, AD
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D23)
  • [6] Size-segregated chemical, gravimetric and number distribution-derived mass closure of the aerosol in Sagres, Portugal during ACE-2
    Neusüss, C
    Weise, D
    Birmili, W
    Wex, H
    Wiedensohler, A
    Covert, DS
    TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02) : 169 - 184
  • [7] AEROSOL-SIZE DISTRIBUTIONS IN ARCTIC HAZE DURING THE POLAR SUNRISE EXPERIMENT 1992
    STAEBLER, RM
    DENHARTOG, G
    GEORGI, B
    DUSTERDIEK, T
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D12) : 25429 - 25437
  • [8] The chemical composition of the size-segregated atmospheric aerosol in Sagres (Portugal) during ACE-2
    Neusüß, C.
    Thomas, A.
    Gerlach, B.
    Gnauk, T.
    Brüggemann, E.
    Herrmann, H.
    Journal of Aerosol Science, 1998, 29 (SUPPL.2):
  • [9] Aerosol optical properties at Sagres, Portugal during ACE-2
    Carrico, CM
    Rood, MJ
    Ogren, JA
    Neusüss, C
    Wiedensohler, A
    Heintzenberg, J
    TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02): : 694 - 715
  • [10] Vertical profiles of aerosol scattering and absorption measured in situ during the North Atlantic Aerosol Characterization Experiment (ACE-2)
    Öström, E
    Noone, KJ
    TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02): : 526 - 545