ATMOSPHERIC SULFUR-HEXAFLUORIDE - SOURCES, SINKS AND GREENHOUSE WARMING

被引:97
作者
KO, MKW
SZE, ND
WANG, WC
SHIA, G
GOLDMAN, A
MURCRAY, FJ
MURCRAY, DG
RINSLAND, CP
机构
[1] UNIV DENVER, DEPT PHYS, DENVER, CO 80208 USA
[2] NASA, LANGLEY RES CTR, CTR ATMOSPHER SCI, HAMPTON, VA 23681 USA
[3] ALLIED SIGNAL INC, BUFFALO RES LAB, BUFFALO, NY 14210 USA
[4] SUNY Albany, ALBANY, NY 12222 USA
关键词
D O I
10.1029/93JD00228
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Model calculations using estimated reaction rates of sulfur hexafluoride (SF6) with OH and O(1D) indicate that the atmospheric lifetime due to these processes may be very long (25,000 years). An upper limit for the UV cross section would suggest a photolysis lifetime much longer than 1000 years. The possibility of other removal mechanisms are discussed. The estimated lifetimes are consistent with other estimated values based on recent laboratory measurements. There appears to be no known natural source of SF6. An estimate of the current production rate of SF6 is about 5 kt/yr. Based on historical emission rates, we calculated a present-day atmospheric concentrations for SF6 of about 2.5 parts per trillion by volume (pptv) and compared the results with available atmospheric measurements. It is difficult to estimate the atmospheric lifetime of SF6 based on mass balance of the emission rate and observed abundance. There are large uncertainties concerning what portion of the SF6 is released to the atmosphere. Even if the emission rate were precisely known, it would be difficult to distinguish among lifetimes longer than 100 years since the current abundance of SF6 is due to emission in the past three decades. More information on the measured trends over the past decade and observed vertical and latitudinal distributions of SF6 in the lower stratosphere will help to narrow the uncertainty in the lifetime. Based on laboratory-measured IR absorption cross section for SF6, we showed that SF6 is about 3 times more effective as a greenhouse gas compared to CFC 11 on a per molecule basis. However, its effect on atmospheric warming will be minimal because of its very small concentration. We estimated the future concentration of SF6 at 2010 to be 8 and 10 pptv based on two projected emission scenarios. The corresponding equilibrium warming of 0.0035-degrees-C and 0.0043-degrees-C is to be compared with the estimated warming due to CO2 increase of about 0.8-degrees-C in the same period.
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收藏
页码:10499 / 10507
页数:9
相关论文
共 45 条
  • [1] INFRARED SPECTRAL ABSORPTION INTENSITIES IN THE V3 AND V4 REGIONS OF SF6
    BRODBECK, C
    ROSSI, I
    STRAPELIAS, H
    BOUANICH, JP
    [J]. CHEMICAL PHYSICS, 1980, 54 (01) : 1 - 7
  • [2] OCEANIC CONSUMPTION OF CH3CCL3 - IMPLICATIONS FOR TROPOSPHERIC OH
    BUTLER, JH
    ELKINS, JW
    THOMPSON, TM
    HALL, BD
    SWANSON, TH
    KOROPALOV, V
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D12) : 22347 - 22355
  • [4] ATMOSPHERIC CARBON TETRAFLUORIDE - NEARLY INERT-GAS
    CICERONE, RJ
    [J]. SCIENCE, 1979, 206 (4414) : 59 - 61
  • [5] ATMOSPHERIC LIFETIME AND ANNUAL RELEASE ESTIMATES FOR CFCL3 AND CF2CL2 FROM 5 YEARS OF ALE DATA
    CUNNOLD, DM
    PRINN, RG
    RASMUSSEN, RA
    SIMMONDS, PG
    ALYEA, FN
    CARDELINO, CA
    CRAWFORD, AJ
    FRASER, PJ
    ROSEN, RD
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1986, 91 (D10) : 797 - 817
  • [6] THE ATMOSPHERIC LIFETIME EXPERIMENT .3. LIFETIME METHODOLOGY AND APPLICATION TO 3 YEARS OF CFCL3 DATA
    CUNNOLD, DM
    PRINN, RG
    RASMUSSEN, RA
    SIMMONDS, PG
    ALYEA, FN
    CARDELINO, CA
    CRAWFORD, AJ
    FRASER, PJ
    ROSEN, RD
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1983, 88 (NC13) : 8379 - 8400
  • [7] TRACER STUDY OF POLLUTANT TRANSPORT AND DISPERSION IN LOS-ANGELES AREA
    DRIVAS, PJ
    SHAIR, FH
    [J]. ATMOSPHERIC ENVIRONMENT, 1974, 8 (11) : 1155 - 1163
  • [8] THE ABSOLUTE INTENSITIES OF THE BINARY COMBINATION BANDS IN THE INFRARED-SPECTRUM OF SF6
    DUNN, DS
    SCANLON, K
    OVEREND, J
    [J]. SPECTROCHIMICA ACTA PART A-MOLECULAR AND BIOMOLECULAR SPECTROSCOPY, 1982, 38 (08): : 841 - 847
  • [9] FERSHENFELD FC, 1971, J CHEM PHYS, V54, P438
  • [10] MODEL-CALCULATIONS OF THE RELATIVE EFFECTS OF CFCS AND THEIR REPLACEMENTS ON GLOBAL WARMING
    FISHER, DA
    HALES, CH
    WANG, WC
    KO, MKW
    SZE, ND
    [J]. NATURE, 1990, 344 (6266) : 513 - 516