Asian dust events of April 1998

被引:686
|
作者
Husar, RB
Tratt, DM
Schichtel, BA
Falke, SR
Li, F
Jaffe, D
Gassó, S
Gill, T
Laulainen, NS
Lu, F
Reheis, MC
Chun, Y
Westphal, D
Holben, BN
Gueymard, C
McKendry, I
Kuring, N
Feldman, GC
McClain, C
Frouin, RJ
Merrill, J
DuBois, D
Vignola, F
Murayama, T
Nickovic, S
Wilson, WE
Sassen, K
Sugimoto, N
Malm, WC
机构
[1] Washington Univ, Ctr Air Pollut Impact & Trend Anal, St Louis, MO 63130 USA
[2] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[3] Univ Washington, Seattle, WA 98195 USA
[4] Texas Tech Univ, Dept Geosci, Lubbock, TX 79409 USA
[5] Pacific NW Natl Lab, Richland, WA 99352 USA
[6] China Meteorol Adm, Natl Satellite Meteorol Ctr, Beijing, Peoples R China
[7] US Geol Survey, Washington, DC 20242 USA
[8] Meteorol Res Inst, Seoul, South Korea
[9] Naval Res Lab, Monterey, CA 93943 USA
[10] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[11] Univ Cent Florida, Orlando, FL 32816 USA
[12] Univ British Columbia, Dept Geog, Vancouver, BC, Canada
[13] Univ San Diego, Scripps Inst Oceanog, La Jolla, CA 92110 USA
[14] Univ Rhode Isl, Ctr Atmospher Chem Studies, Kingston, RI 02881 USA
[15] New Mexico Environm Dept, Air Qual Bur, Santa Fe, NM 87505 USA
[16] Univ Oregon, Solar Monitoring Lab, Eugene, OR 97403 USA
[17] Tokyo Univ Mercantile Marine, Dept Phys, Tokyo, Japan
[18] Univ Malta, Euro Mediterranean Ctr Insular Coastal Dynam ICoD, Valletta, Malta
[19] US EPA, Natl Ctr Environm Assessment, Res Triangle Pk, NC 27711 USA
[20] Univ Utah, Dept Meteorol, Salt Lake City, UT 84112 USA
[21] Natl Inst Environm Studies, Tsububa, Iburaki, Japan
[22] Colorado State Univ, NPS Air Resources Div, Ft Collins, CO 80521 USA
来源
关键词
D O I
10.1029/2000JD900788
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
On April 15 and 19, 1998, two intense dust storms were generated over the Gobi desert by springtime low-pressure systems descending from the northwest. The windblown dust was detected and its evolution followed by its yellow color on SeaWiFS satellite images, routine surface-based monitoring, and through serendipitous observations. The April 15 dust cloud was recirculating, and it was removed by a precipitating weather system over east Asia. The April 19 dust cloud crossed the Pacific Ocean in 5 days, subsided to the surface along the mountain ranges between British Columbia and California, and impacted severely the optical and the concentration environments of the region. In east Asia the dust clouds increased the albedo over the cloudless ocean and land by up to 10-20%, but it reduced the near-UNI cloud reflectance, causing a yellow coloration of all surfaces. The yellow colored backscattering by the dust eludes a plausible explanation using simple Mie theory with constant refractive index. Over the West Coast the dust layer has increased the spectrally uniform optical depth to about 0.4, reduced the direct solar radiation by 30-40%, doubled the diffuse radiation, and caused a whitish discoloration of the blue sky. On April 29 the average excess surface-level dust aerosol concentration over the valleys of the West Coast was about 20-50 mug/m(3) with local peaks > 100 mug/m(3). The dust mass mean diameter was 2-3 mum, and the dust chemical fingerprints were evident throughout the West Coast and extended to Minnesota. The April 1998 dust event has impacted the surface aerosol concentration 2-4 times more than any other dust event since 1988. The dust events were observed and interpreted by an ad hoc international web-based virtual community. It would be useful to set up a community-supported web-based infrastructure to monitor the global aerosol pattern for such extreme aerosol events, to alert and to inform the interested communities, and to facilitate collaborative analysis for improved air quality and disaster management.
引用
收藏
页码:18317 / 18330
页数:14
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