在日常规模上使用TROPOMI空间观测的多种类型的气溶的三维分布
Prem Maheshwarkar1, Juan Cuesta1, Paola Formenti2
1Univ Paris Est Créteil and Université Paris Cité, CNRS, LISA, F-94010 Créteil, France.
The Science of the total environment
|October 25, 2024
概括
新的卫星观测揭示了气溶的3D分布,包括烟雾和尘埃,使用AEROS5P方法. 这种方法增强了空间覆盖范围,并提供了对气溶传输和空气质量影响的见解.
科学领域:
- 大气科学 大气科学
- 遥感 遥感 遥感 遥感
- 环境监测 环境监测
背景情况:
- 基于卫星的气溶观测对于了解大气过程和空气质量至关重要.
- 以前的方法在气溶类型覆盖范围和空间范围方面存在局限性.
- 太空层臭氧监测仪 (TROPOMI) 提供高分辨率的光谱反射率数据.
研究的目的:
- 介绍一种基于卫星的增强方法 (AEROS5P),用于观察常见气溶类型的3D分布.
- 改进空间覆盖范围,并将喷雾剂垂直配置文件的检索泛化.
- 分析气溶运输模式及其对空气质量的影响.
主要方法:
- 使用TROPOMI测量和AEROS5P方法来检索垂直气溶灭绝概况.
- 整合可见红外成像放射仪套件 (VIIRS) 的气溶类型数据以先验定义气溶的特性.
- 将AEROS5P的结果与AErosol机器人网络 (AERONET) 和激光雷达观测结果进行验证.
主要成果:
- AEROS5P表现出与已建立的卫星和地面测量对气溶光学深度和垂直分布的良好一致.
- 成功追踪了来自加拿大野火和沙漠尘埃的烟雾的3D路径.
- 在西欧捕获了微型气溶污染物,在中国北部捕获了混合灰尘/气溶事件.
结论:
- AEROS5P方法提供了有价值的日常3D气溶观测,具有更好的覆盖范围和通用适用性.
- 这些观测为气溶运输,空气质量和潜在的辐射效应提供了关键的见解.
- 改进的方法支持更好地了解全球气溶动态和影响.
相关概念视频
Pore Size Distribution
92
In concrete, the pore size distribution significantly influences the material's properties. Capillary pores, markedly larger than gel pores, form a vast network within partially hydrated cement paste, reducing the concrete's strength and increasing its permeability. This heightened permeability leads to a greater risk of damage from environmental factors like freeze-thaw cycles and chemical attacks, with the extent of vulnerability also being tied to the water-to-cement ratio.
Adequate...
Adequate...
92
Distribution and Dispersion
21.6K
To understand intra-specific interactions in populations, scientists measure the spatial arrangement of species individuals. This geographic arrangement is known as the species distribution or dispersion. Highly territorial species exhibit a uniform distribution pattern, in which individuals are spaced at relatively equal distances from one another. Species that are highly tied to particular resources, such as food or shelter, tend to concentrate around those resources, and thus exhibit a...
21.6K
Precipitation Processes
428
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
428
Turbulent Flow
146
Turbulent flow is characterized by unpredictable fluctuations in velocity and pressure, which result in a chaotic fluid movement distinct from the orderly patterns of laminar flow. While laminar flow is governed by smooth, parallel layers with minimal mixing, turbulent flow exhibits highly irregular, three-dimensional patterns. This behavior arises due to instabilities in the fluid's velocity profile, and amplifies as the flow velocity increases. Minor disturbances, known as turbulent...
146
Precipitation Gravimetry
5.4K
Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
5.4K
Variation of Atmospheric Pressure
2.1K
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
2.1K


