ISO 28902-4:2026 PDF
Air quality — Environmental meteorology — Part 4: Ground-based remote sensing of meteorological parameters by particle backscatter lidar
Air quality — Environmental meteorology — Part 4: Ground-based remote sensing of meteorological parameters by particle backscatter lidar
- Статус документа:
- Действующий
- Формат:
- Электронный (PDF)
- Количество страниц:
- 69
- Дата публикации:
- 13 августа 2026 г.
- Издание:
- ISO IS 28902 edition 1 version 1
- ICS:
- 07.060
This document specifies the determination of height-resolved profiles of atmospheric backscattering by means of active optical sounding. The measurements allow the following properties of the atmosphere up to several kilometres above ground to be derived: cloud bases; upper boundaries of optically thin clouds; upper and lower boundaries and internal structures of particle layers: height of structures, e.g. inversions, boundary layer height, mixing layer height (under suitable conditions); attenuated backscatter of the particles; particle backscatter and extinction coefficients (requires further assumptions). The document also addresses the depolarisation lidar and the use of multi-wavelength systems. This allows further parameters to be determined: particle size classification (Ångström exponent, colour ratio); shape classification (linear depolarisation degree). The following fields of application are particularly important: air quality monitoring (vertical structure of the boundary layer); aviation safety (cloud base and visual range) (see ISO 28902-1[8]); particle content and transport (e.g. volcanic dust); weather forecasting and climate modelling (e.g. atmospheric boundary layer, cloud base, cloud microphysics); satellite remote sensing (validation). Examples that illustrate these applications are discussed in Annex A. The benefits of scanning systems for parameters mentioned above are also discussed in Clause A.7. In addition, particle backscatter lidars that measure at least two carefully selected wavelengths can be used to determine atmospheric gas concentrations. This is known as the differential absorption lidar “DIAL” technique. This technique is not part of this document and has been described in VDI 4210-1[12]. This document does not specify extended lidar techniques that monitor the following parameters quantitatively: inelastic scattering effects such as, Raman scattering, Doppler broadening, Doppler shift, multiple scattering, modulation techniques, and spectral separation of molecular and particle backscattering [high spectral resolution lidar (HSRL)]. Some of these extended techniques are or will be described in other parts of the ISO 28902 series. This document does not address special features of airborne or satellite-borne systems.
Abstract
Overview
ISO 28902-4:2026 addresses the use of ground-based particle backscatter lidar to remotely sense meteorological parameters critical for air quality and atmospheric studies. Developed by the International Organization for Standardization (ISO), this standard is part of the broader ISO 28902 series on environmental meteorology and remote sensing. It specifically provides a framework for determining vertical, height-resolved profiles of atmospheric backscattering using active optical (lidar) measurements. These measurements enable the derivation of essential atmospheric features such as cloud bases, boundaries of optically thin clouds, internal structures of aerosol layers, and particle characteristics up to several kilometers above ground level.
Key Topics
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Lidar Principle and Measurement: Uses laser pulses directed into the atmosphere and measures backscattered light to analyze atmospheric conditions. The distance to scattering particles is calculated using travel time of the light, providing height-resolved data.
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Derived Atmospheric Parameters: Enables determination of:
- Cloud base height and penetration depth
- Upper and lower boundaries of atmospheric layers (e.g., boundary layer, mixing layer)
- Attenuated backscatter of particles
- Particle backscatter and extinction coefficients (with relevant assumptions)
- Particle size (Ångström exponent, colour ratio) and shape classification (linear depolarisation ratio) through multi-wavelength and depolarisation lidar techniques
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System Components: Describes essential lidar system elements, including lasers, transmitting and receiving optics, detectors, filters, data acquisition systems, and support infrastructure. Addresses mono- and multi-wavelength, as well as polarization-sensitive (depolarisation) systems.
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Measurement Planning and Uncertainty: Covers best practices for planning lidar measurements, safety considerations, instrument adjustment, maintenance, and uncertainty estimation associated with collected data.
Applications
Particle backscatter lidar, as standardized in ISO 28902-4:2026, is essential in a range of atmospheric and environmental applications:
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Air Quality Monitoring:
- Provides vertical profiling of the atmospheric boundary layer, helping to assess pollutant dispersion and stratification.
- Supports identification and tracking of particle layers such as dust, smoke, or pollution events.
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Aviation Safety:
- Enables accurate detection of cloud base heights and visibility range, supporting real-time decision-making for air traffic and airport operations.
- Offers measurements in support of the requirements found in ISO 28902-1 for visual range assessments.
-
Weather Forecasting and Climate Modeling:
- Supplies crucial input for models by providing high-resolution data on cloud properties, atmospheric layering, and aerosol distribution.
- Enhances understanding of phenomena such as mixing layers and temperature inversions.
-
Particle Transport Studies:
- Useful for monitoring movement of volcanic ash, desert dust, and other aerosol events, thus informing public health advisories and mitigating transportation disruption.
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Satellite Remote Sensing Validation:
- Lidar observations are used to validate and calibrate satellite-derived atmospheric data.
Related Standards
For organizations integrating particle backscatter lidar systems within their monitoring networks, the following related ISO standards should be considered:
- ISO 28902-1: Ground-based remote sensing of visual range by lidar
- ISO 28902-2: Ground-based remote sensing of wind by heterodyne pulsed Doppler lidar
- ISO 28902-3: Ground-based remote sensing of wind by continuous-wave Doppler lidar
- ISO 19926-1: Weather radar system performance for frequencies between 2 GHz - 10 GHz
- VDI 4210-1: Differential absorption lidar (DIAL) for gaseous air pollution measurement (the DIAL technique is referenced but not covered in detail in ISO 28902-4)
Practical Value
Adhering to ISO 28902-4:2026 ensures:
- Consistent and reliable generation of lidar-based meteorological data.
- Improved comparability of results across international studies and regulatory monitoring.
- Safe and effective operation of instrumentation under varying atmospheric and site conditions.
- High value for air quality agencies, meteorological services, climate researchers, and industries requiring validated atmospheric profiling tools.
By following this standard, users can enhance the accuracy, repeatability, and utility of ground-based lidar observations, supporting robust air quality management and environmental decision-making.
Технические детали
- Технический комитет
- ISO/TC 146/SC 5 - Meteorology
- SKU
- ISO 28902-4:2026
Похожие стандарты
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