Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1029/2000JD900556 |
Physical and chemical characteristics of aerosols over the Negev Desert (Israel) during summer 1996 | |
Formenti, P; Andreae, MO; Andreae, TW; Ichoku, C; Schebeske, G; Kettle, J; Maenhaut, W; Cafmeyer, J; Ptasinsky, J; Karnieli, A; Lelieveld, J | |
通讯作者 | Formenti, P |
来源期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2001 |
卷号 | 106期号:D5页码:4871-4890 |
英文摘要 | Sde Boker, in the Negev Desert of Israel (30 degrees 51’N, 34 degrees 47’E; 470 m above sea level (asl), is a long-term station to investigate anthropogenic and natural aerosols in the eastern Mediterranean in the framework of the Aerosol, Radiation and Chemistry Experiment (ARACHNE), Ground-level measurements of physical and chemical properties of aerosols and supporting trace gases were performed during an intensive campaign in summer 1996 (ARACHNE-96). Fine non sea salt (nss)-SO42- averaged 8 +/- 3 mug m(-3) and fine black carbon averaged 1.4 +/- 0.5 mug m(-3), comparable to values observed off the east coast of the United States. Optical parameters relevant for radiative forcing calculations were determined, The backscatter ratio for ARACHNE-96 was beta = 0.13 +/- 0.01. The mass absorption efficiency for tine black carbon (alpha (a),(BCEf)) was estimated as 8.9 +/- 1.3 m(2) g(-1) at 550 nm, while the mass scattering efficiency for fine nss-SO4-2 (alpha (s,nss-SO42-f)) was 7.4 +/- 2.0 m(2) g(-1). The average dry single-scattering albedo, omega (0) characterizing polluted conditions was 0.89, whereas during "clean" periods omega (0) was 0.94. The direct radiative effect of the pollution aerosols is estimated to be cooling. At low altitudes (below 800 hPa), the area was generally impacted by polluted air masses traveling over the Balkan region, Greece, and Turkey. Additional pollution was often added to these air masses along the Israeli Mediterranean coast, where population and industrial centers are concentrated. At higher altitudes (700 and 500 hPa), air masses came either from eastern Europe or from North Africa (Algerian or Egyptian deserts). The combination of measurements of SO2, CO, CN (condensation nuclei), and accumulation mode particles allowed to characterize the air masses impacting the site in terms of a mixture of local and long range transported pollution. In particular, the lack of correlation between SO2 and nss-SO42- indicates that the conversion of regional SO2 into the particulate phase is not an efficient process in summer and that aged pollution dominates the accumulation mode particle concentrations. |
类型 | Article |
语种 | 英语 |
国家 | Germany ; Netherlands ; Belgium ; Israel |
收录类别 | SCI-E |
WOS记录号 | WOS:000167482900014 |
WOS关键词 | ANTHROPOGENIC SULFATE AEROSOLS ; LONG-RANGE TRANSPORT ; LIGHT EXTINCTION ; UNITED-STATES ; EAST-COAST ; CARBONACEOUS AEROSOLS ; ATMOSPHERIC AEROSOLS ; MEDITERRANEAN REGION ; PIXE ANALYSIS ; SAHARAN DUST |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源机构 | Ben-Gurion University of the Negev |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/141253 |
作者单位 | (1)Max Planck Inst Chem, Biogeochem Dept, D-55020 Mainz, Germany;(2)Univ Utrecht, Inst Marine & Atmospher Res, IMAU, NL-3584 Utrecht, Netherlands;(3)Univ Ghent, Inst Nucl Sci, B-9000 Ghent, Belgium;(4)Ben Gurion Univ Negev, IL-84990 Beer Sheva, Israel |
推荐引用方式 GB/T 7714 | Formenti, P,Andreae, MO,Andreae, TW,et al. Physical and chemical characteristics of aerosols over the Negev Desert (Israel) during summer 1996[J]. Ben-Gurion University of the Negev,2001,106(D5):4871-4890. |
APA | Formenti, P.,Andreae, MO.,Andreae, TW.,Ichoku, C.,Schebeske, G.,...&Lelieveld, J.(2001).Physical and chemical characteristics of aerosols over the Negev Desert (Israel) during summer 1996.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,106(D5),4871-4890. |
MLA | Formenti, P,et al."Physical and chemical characteristics of aerosols over the Negev Desert (Israel) during summer 1996".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 106.D5(2001):4871-4890. |
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