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Arctic Study of Tropospheric Aerosol and Radiation (ASTAR) 2000: Arctic haze case study

机译:对流层气溶胶和辐射的北极研究(astar)2000:北极阴霾案例研究

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摘要

The ASTAR 2000 (Arctic Study of Tropospheric Aerosol and Radiation) campaign ran from 12 March until 25 April 2000 with extensive flight operations in the vicinity of Svalbard (Norway) from Longyearbyen airport (78.25°N, 15.49°E). It was a joint Japanese (NIPR Tokyo)German (AWI Bremerhaven/Potsdam) airborne measurement campaign using AWI aircraft POLAR 4 (Dornier 228-101). Simultaneous ground-based measurements were done at the international research site Ny-lesund (78.95°N, 11.93°E) in Svalbard, at the German Koldewey station, at the Japanese Rabben station and at the Scandinavian station at Zeppelin Mountain (475 m above sea level). During the campaign 19 profiles of various aerosol properties were measured. In general, the Arctic spring aerosol in the vicinity of Svalbard had significant temporal and vertical variability.A strong haze event occurred between 21 and 25 March in which the optical depth from ground-based observation was 0.18, which was significantly greater than the background value of 0.06. Airborne measurements on 23 March during this haze event showed a high aerosol layer with an extinction coefficient of 0.03 km1 or more up to 3 km and a scattering coefficient from 0.02 in the same altitude range. From the chemical analyses of airborne measurements, sulfate, soot and sea salt particles were dominant, and there was a high mixing ratio of external soot particles in some layers during the haze event, whereas internal mixing of soot in sulfate was noticeable in some layers for the background condition. We argue that the high aerosol loading is due to direct transport from anthropogenic source regions. In this paper we focus on the course of the haze event in detail through analyses of the airborne and ground-based results.
机译:ASTAR 2000(对流层气溶胶和辐射的北极研究)运动于2000年3月12日至4月25日进行,从朗伊尔城机场(北纬78.25度,东经15.49度)在斯瓦尔巴特(挪威)附近进行了大规模飞行。这是一次日本(NIPR东京)德国人(AWI不来梅港/波茨坦)空战测量战,使用AWI飞机POLAR 4(多尼尔228-101)进行。在斯瓦尔巴特群岛的国际研究地点Ny-lesund(78.95°N,11.93°E),德国的Koldewey站,日本的Rabben站和Zeppelin山的斯堪的纳维亚站(海拔475 m)上进行了同时的地面测量海平面)。在竞选期间,测量了19种各种气溶胶特性的轮廓。总体而言,斯瓦尔巴特群岛附近的北极春季气溶胶具有明显的时间和垂直变化性.3月21日至25日发生了强烈的霾事件,地面观测的光学深度为0.18,明显大于背景值为0.06。 3月23日在此霾事件期间的空中测量显示,在相同的高度范围内,高气溶胶层的消光系数为0.03 km1或更高,直至3 km,散射系数为0.02。从空气传播测量的化学分析来看,在雾霾事件中,硫酸盐,烟灰和海盐颗粒占主导地位,并且在某些层中外部烟灰颗粒的混合比很高,而对于某些层,烟灰在硫酸盐中的内部混合很明显。背景条件。我们认为高的气溶胶负荷是由于来自人为源区域的直接运输。在本文中,我们通过对机载和地面结果的分析来详细研究霾事件的发生过程。

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