Thirty years of in situ stratospheric aerosol size distribution measurements from Laramie, Wyoming (41°N), using balloon-borne instruments -: art. no. 4167

被引:190
作者
Deshler, T [1 ]
Hervig, ME
Hofmann, DJ
Rosen, JM
Liley, JB
机构
[1] Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA
[2] GATS Inc, Driggs, ID 83422 USA
[3] Natl Ocean & Atmospher Adm, Boulder, CO 80305 USA
[4] Natl Inst Water & Atmospher Res, Lauder, Central Otago, New Zealand
[5] Univ Wyoming, Dept Phys & Astron, Laramie, WY 82071 USA
关键词
stratospheric aerosol size distributions; volcanic stratospheric aerosol; background stratospheric aerosol; in situ aerosol size distribution measurements; optical particle counters; balloonborne aerosol measurements;
D O I
10.1029/2002JD002514
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Vertical profiles of size-resolved aerosol concentrations above Laramie, Wyoming (41degreesN), have been measured for the past thirty years, 1971-2001. During this period, two somewhat different optical particle counters have been used to measure particles with radii greater than or equal to0.15 mum, whereas the instrument to measure condensation nuclei (CN) has not changed significantly since the late 1970s. The two optical particle counters measure aerosols greater than or equal to0.15, 0.25 mum and aerosols greater than or equal to0.15-2.0 mum in twelve size classes. These measurements have concentration (N) uncertainties proportional to +/-N-0.5, but with a minimum of +/-10%. Sizing uncertainties are about +/-10%. The impact of these uncertainties on size distribution fitting parameters and aerosol moments are approximately +/-30% and +/-40%. The long-term record from these measurements indicates that volcanoes have controlled stratospheric aerosol abundance for 20 of the past 30 years. The present period, beginning in 1997, represents the longest volcanically quiescent period in the record. These and other measurements clearly show that stratospheric aerosol are now in a background state, a state rarely occurring in recent times, and that this background state is not significantly different than observations in 1979. Aerosol volumes and surface areas, inferred from size distributions fit to the measurements, are compared with SAGE II satellite estimates of surface area and volume. For volume the measurements are in agreement within measurement error throughout the record. For surface area there is good agreement for a volcanic aerosol laden stratosphere, but for background aerosol conditions the SAGE II estimates are about 40% less than the in situ measurements. Present aerosol surface areas are similar to1.0 (0.6) mum(2) cm(-3) in the 15-20 (20-25) km layer based on in situ measurements. The Laramie size distribution record is now available to the community over the internet.
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页数:13
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共 100 条
  • [91] Major optical depth perturbations to the stratosphere from volcanic eruptions: Pyrheliometric period, 1881-1960
    Stothers, RB
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D2) : 3901 - 3920
  • [92] Balloon-borne optical counter for in situ aerosol measurements
    Sugita, T
    Kondo, Y
    Koike, M
    Kanada, M
    Toriyama, N
    Nakajima, H
    Deshler, T
    Imasu, R
    [J]. JOURNAL OF ATMOSPHERIC CHEMISTRY, 1999, 32 (01) : 183 - 204
  • [93] A comparison of the stratospheric aerosol background periods of 1979 and 1989-1991
    Thomason, LW
    Kent, GS
    Trepte, CR
    Poole, LR
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D3) : 3611 - 3616
  • [94] A global climatology of stratospheric aerosol surface area density deduced from stratospheric aerosol and gas experiment II measurements: 1984-1994
    Thomason, LW
    Poole, LR
    Deshler, T
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D7) : 8967 - 8976
  • [95] USE OF STRATOSPHERIC AEROSOL PROPERTIES AS DIAGNOSTICS OF ANTARCTIC VORTEX PROCESSES
    THOMASON, LW
    POOLE, LR
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1993, 98 (D12) : 23003 - 23012
  • [96] HETEROGENEOUS INTERACTIONS OF CHLORINE NITRATE, HYDROGEN-CHLORIDE, AND NITRIC-ACID WITH SULFURIC-ACID SURFACES AT STRATOSPHERIC TEMPERATURES
    TOLBERT, MA
    ROSSI, MJ
    GOLDEN, DM
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1988, 15 (08) : 847 - 850
  • [97] Twomey S., 1977, Introduction to the Mathematics of inversion in remote sensing and indirect measurements
  • [98] SAGE-II AEROSOL DATA VALIDATION BASED ON RETRIEVED AEROSOL MODEL SIZE DISTRIBUTION FROM SAGE-II AEROSOL MEASUREMENTS
    WANG, PH
    MCCORMICK, MP
    MCMASTER, LR
    CHU, WP
    SWISSLER, TJ
    OSBORN, MT
    RUSSELL, PB
    OBERBECK, VR
    LIVINGSTON, J
    ROSEN, JM
    HOFMANN, DJ
    GRAMS, GW
    FULLER, WH
    YUE, GK
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1989, 94 (D6): : 8381 - 8393
  • [99] REMOVAL OF STRATOSPHERIC O-3 BY RADICALS - IN-SITU MEASUREMENTS OF OH, HO2, NO, NO2, CLO, AND BRO
    WENNBERG, PO
    COHEN, RC
    STIMPFLE, RM
    KOPLOW, JP
    ANDERSON, JG
    SALAWITCH, RJ
    FAHEY, DW
    WOODBRIDGE, EL
    KEIM, ER
    GAO, RS
    WEBSTER, CR
    MAY, RD
    TOOHEY, DW
    AVALLONE, LM
    PROFFITT, MH
    LOEWENSTEIN, M
    PODOLSKE, JR
    CHAN, KR
    WOFSY, SC
    [J]. SCIENCE, 1994, 266 (5184) : 398 - 404
  • [100] ZHAO R, 1996, THESIS U WYO LARAMIE