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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Latitudinal, vertical, and seasonal variations of C-1-C-4 alkyl nitrates in the troposphere over the Pacific Ocean during PEM-Tropics A and B: Oceanic and continental sources - art. no. 8242
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Latitudinal, vertical, and seasonal variations of C-1-C-4 alkyl nitrates in the troposphere over the Pacific Ocean during PEM-Tropics A and B: Oceanic and continental sources - art. no. 8242

机译:PEM-热带A和B期间太平洋对流层中C-1-C-4烷基硝酸盐的纬度,垂直和季节性变化:海洋和大陆来源-艺术。没有。 8242

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摘要

We present concentration distributions of C-1-C-4 alkyl nitrates observed during the NASA airborne campaigns Pacific Exploratory Mission (PEM)-Tropics A (September October 1996) and PEM-Tropics B (March - April 1999). The total geographic range for PEM-Tropics A was 45degreesN-72degreesS latitude and 153degreesE-75degreesW longitude, and for PEM-Tropics B was 40degreesN-36degreesS latitude and 149degreesE-75degreesW longitude. The maximum altitude for these missions was 12 km. These experiments provide the most extensive set of tropospheric measurements collected to date over the tropical Pacific Ocean. We observed high methyl nitrate (MeONO2, CH3ONO2) mixing ratios ( approximately 50 pptv) at low altitudes in a latitude band between 8degreesN to 13degreesS stretching across the equatorial Pacific, illustrating the oceanic source of MeONO2. This source may be associated with the high-nutrient, low-chlorophyll character of equatorial Pacific waters. We discuss MeONO2 and ethyl nitrate (EtONO2, C2H5ONO2), whose abundance is dominated by equatorial oceanic sources, 2-Propyl nitrate (2-PrONO2, 2-C3H7ONO2), which has significant oceanic and northern hemispheric (NH) sources associated with urban/industrial hydrocarbon emissions, and 2-butyl nitrate (2-BuONO2 2-C4H8ONO2), which has mostly NH sources. PEM-Tropics A and B resulted in remarkably similar equatorial mixing ratios. The excellent correlations between MeONO2 and the other alkyl nitrates in this region produced comparable correlation slopes between the two expeditions. By contrast, NH air masses influenced by urban/industrial emissions typically exhibited much lower MeONO2: EtONO2, MeONO2: 2-PrONO2, and MeONO2: 2-BuONO2 ratios. These relationships can be useful as a diagnostic of air mass origin. North of 10degreesN, the springtime PEM-Tropics B mixing ratios of C-2-C-4 alkyl nitrates were many-fold higher at low-mid altitudes than for late summer PEM-Tropics A, consistent with strong continental outflow of NMHC precursors during spring. [References: 50]
机译:我们介绍了在NASA航空运动太平洋探索团(PEM)-热带A(1996年10月)和PEM-热带B(1999年3月-1999年4月)观察到的C-1-C-4烷基硝酸盐的浓度分布。 PEM-热带A的总地理范围是北纬45度N-72度,东经153度E-75度,PEM-B热带B的总地理范围是北纬40度N-36度和149度E-75度W。这些任务的最大高度为12公里。这些实验提供了迄今为止在热带太平洋上最广泛的对流层测量数据集。我们观察到,低海拔地区在北纬8度到13度之间的高纬度地区,硝酸甲酯(MeONO2,CH3ONO2)的混合比很高(大约50 pptv),说明了MeONO2的海洋来源。这种来源可能与赤道太平洋水域的高营养,低叶绿素特征有关。我们讨论了MeONO2和硝酸乙酯(EtONO2,C2H5ONO2),它们的丰度主要由赤道海洋源2-硝酸丙酯(2-PrONO2、2-C3H7ONO2)组成,后者具有与城市/城市相关的重要海洋和北半球(NH)源工业碳氢化合物的排放以及硝酸2-丁酯(2-BuONO2 2-C4H8ONO2),其中大部分为NH。 PEM-热带A和B导致赤道混合比率非常相似。 MeONO2与该区域其他硝酸烷基酯之间的极好相关性在两次考察之间产生了可比的相关斜率。相比之下,受城市/工业排放影响的NH气团通常表现出低得多的MeONO2:EtONO2,MeONO2:2-PrONO2和MeONO2:2-BuONO2比。这些关系可用于诊断空气质量起源。在北纬10度以北,中低海拔地区春季C-2-C-4烷基硝酸盐的PEM-热带B的春季混合比要比夏末PEM-热带A的高很多倍,这与NMHC前体在大陆上大量外流相一致。弹簧。 [参考:50]

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