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Optical and chemical properties of marine aerosols over the central equatorial Pacific Ocean during the 2003 R/V Mirai cruise

机译:2003年R / V Mirai巡游期间赤道中部太平洋海洋气溶胶的光学和化学性质

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The optical and chemical properties of atmospheric aerosols were measured over the central equatorial Pacific Ocean (from 150°E to 160°W longitude, near the equator) during the R/V Mirai cruise of January 2003. In the area from 165°E to 160°W along the equator, concentrations of anthropogenic chemical components were low; the average concentration of nonsea salt sulfate was 0.28 μg m~(-3), that of vanadium was less than the detection limit, and those of elemental carbon and organic carbon were 0.009 and 0.09 μg-C m~(-3). The scattering coefficients were low (3.2 × 10~(-6) m~(-1) on average), and the absorption coefficients were also extremely low (0.06 × 10~(-6) m~(-1) on average). The mean value of single scattering albedo was 0.98, with a standard deviation of 0.01, indicating that the measured aerosols were transparent and had low variability. The measurement results suggest that nonsea salt sulfate and organic carbon were from natural sources. Sea salt particles and nonsea salt sulfate composed a large fraction (94%) of the water-soluble components of fine particles. Thus the water-soluble components and organic materials from natural sources were primarily responsible for the scattering of solar radiation. The measurement results give typical values of the optical and chemical properties of aerosols in the unpolluted central equatorial Pacific Ocean.
机译:在2003年1月的R / V Mirai航行期间,在赤道中部太平洋海洋(经度150°E至160°W,在赤道附近)测量了大气气溶胶的光学和化学性质。在165°E至沿赤道160°W,人为化学成分的浓度较低;非海盐硫酸盐的平均浓度为0.28μgm〜(-3),钒的含量低于检出限,元素碳和有机碳的平均浓度为0.009和0.09μg-Cm〜(-3)。散射系数低(平均3.2×10〜(-6)m〜(-1),吸收系数也极低(平均0.06×10〜(-6)m〜(-1))。 。单次散射反照率的平均值为0.98,标准偏差为0.01,表明所测气溶胶是透明的,并且变异性低。测量结果表明,非海盐硫酸盐和有机碳均来自自然资源。海盐颗粒和非海盐硫酸盐占细颗粒的水溶性成分的很大一部分(94%)。因此,来自自然资源的水溶性成分和有机材料是造成太阳辐射散射的主要原因。测量结果给出了未污染的赤道中部太平洋气溶胶的光学和化学性质的典型值。

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