TRAJECTORY ANALYSIS OF SOURCE REGIONS INFLUENCING THE SOUTH GREENLAND ICE-SHEET DURING THE DYE-3 GAS AND AEROSOL SAMPLING PROGRAM

被引:39
作者
DAVIDSON, CI
JAFFREZO, JL
SMALL, MJ
SUMMERS, PW
OLSON, MP
BORYS, RD
机构
[1] CNRS,GLACIOL & GEOPHYS ENVIRONNEMENT LAB,F-38402 ST MARTIN DHERES,FRANCE
[2] ATMOSPHER ENVIRONM SERV,DOWNSVIEW M3H 5T4,ON,CANADA
[3] UNIV NEVADA,DESERT RES INST,CTR ATMOSPHER SCI,RENO,NV 89506
来源
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS | 1993年 / 27卷 / 17-18期
基金
美国国家科学基金会;
关键词
DGASP; GREENLAND; TRAJECTORIES; METEOROLOGY; AEROSOLS;
D O I
10.1016/0960-1686(93)90306-J
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Backward air mass trajectories for Dye 3, Greenland (elevation 2.5 km) show source regions that vary with season: the direction of greatest transport distance is from the southwest in fall, west in winter, and northwest in spring; the trajectories in summer do not show a strong preferred direction. Based on 5 d transit times, the trajectories in fall suggest the importance of North America as a potential source region, with occasional trajectories from western Europe, The trajectories in spring, especially in April, suggest Eurasia (transport over the Pole), eastern North America, and western Europe as potential source regions. Less transport of chemical constituents to Dye 3 is expected in summer when transport distances are shorter. Although some long-range transport to Greenland occurs in winter, the stability of the atmosphere over the ice sheet at this time of year is likely to limit the delivery of chemical constituents to the surface. Sources outside of these regions can also influence Dye 3 if transit times longer than 5 d are considered. These results are in contrast to trajectories reported by others for sea-level arctic locations such as Barrow, Alaska and Mould Bay, Canada, where transport over the Pole from Eurasia is responsible for high chemical species concentrations over much of the winter and early spring. Overall, the trajectories are consistent with aerosol chemical data for this time period at Dye 3 reported by several investigators, showing peak concentrations in spring and fall.
引用
收藏
页码:2739 / 2749
页数:11
相关论文
共 59 条
  • [1] [Anonymous], 1980, ANN NY ACAD SCI
  • [2] [Anonymous], 1988, ANN GLACIOL
  • [3] A STATISTICAL TRAJECTORY TECHNIQUE FOR DETERMINING AIR-POLLUTION SOURCE REGIONS
    ASHBAUGH, LL
    [J]. JOURNAL OF THE AIR POLLUTION CONTROL ASSOCIATION, 1983, 33 (11): : 1096 - 1098
  • [4] THE INFLUENCE OF MID-LATITUDINAL POLLUTION SOURCES ON HAZE IN THE CANADIAN ARCTIC
    BARRIE, LA
    HOFF, RM
    DAGGUPATY, SM
    [J]. ATMOSPHERIC ENVIRONMENT, 1981, 15 (08) : 1407 - 1419
  • [5] SEASONAL-VARIATIONS IN THE CONCENTRATION OF BE-10, CL-, NO3-, SO4(2)-, H2O2, PB-210, H-3, MINERAL DUST, AND DELTA-18O IN GREENLAND SNOW
    BEER, J
    FINKEL, RC
    BONANI, G
    GAGGELER, H
    GORLACH, U
    JACOB, P
    KLOCKOW, D
    LANGWAY, CC
    NEFTEL, A
    OESCHGER, H
    SCHOTTERER, U
    SCHWANDER, J
    SIEGENTHALER, U
    SUTER, M
    WAGENBACH, D
    WOLFLI, W
    [J]. ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1991, 25 (5-6): : 899 - 904
  • [6] BARROW SURFACE AEROSOL - 1976-1986
    BODHAINE, BA
    [J]. ATMOSPHERIC ENVIRONMENT, 1989, 23 (11) : 2357 - 2369
  • [7] STUDIES OF ICE NUCLEATION BY ARCTIC AEROSOL ON AGASP-II
    BORYS, RD
    [J]. JOURNAL OF ATMOSPHERIC CHEMISTRY, 1989, 9 (1-3) : 169 - 185
  • [8] ASSESSMENT OF ICE PARTICLE GROWTH-PROCESSES AT DYE-3, GREENLAND
    BORYS, RD
    DELVECCHIO, D
    JAFFREZO, JL
    DAVIDSON, CI
    MITCHELL, DL
    [J]. ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1993, 27 (17-18): : 2815 - 2822
  • [9] SIZE VARIATIONS IN HEAVY-METAL CONCENTRATIONS IN FRESH GREENLAND SNOW FROM JANUARY TO AUGUST 1989
    BOUTRON, CF
    DUCROZ, FM
    GORLACH, U
    JAFFREZO, JL
    DAVIDSON, CI
    BOLSHOV, MA
    [J]. ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1993, 27 (17-18): : 2773 - 2779
  • [10] THE THERMODYNAMICS OF POLLUTANT REMOVAL AS AN INDICATOR OF POSSIBLE SOURCE AREAS FOR ARCTIC HAZE
    BOWLING, SA
    SHAW, GE
    [J]. ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1992, 26 (16): : 2953 - 2961