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Related Concept Videos

UV–Vis Spectrometers01:14

UV–Vis Spectrometers

The absorbance of UV and visible (UV–visible) radiations is measured using a UV–visible spectrophotometer. Deuterium lamps, which emit UV radiation, and tungsten lamps, which produce radiation in the visible region, are used as light sources in UV–visible spectrophotometers. A monochromator or prism is used for diffraction grating, i.e., to split the incoming radiation into different wavelengths. A system of slits is used to focus the desired wavelength on the sample cell. Samples for...
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Ultraviolet–visible (UV–visible or UV–Vis) spectroscopy is an analytical technique that investigates the interaction between matter and UV–Vis light within the electromagnetic spectrum. This method is widely used for its versatility, simplicity, and relatively quick data acquisition, making it valuable for both qualitative and quantitative analysis. When UV–Vis radiation passes through a material,  molecules absorb light depending on the energy required for electronic transitions. As a result...
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Related Experiment Video

Updated: Jun 12, 2026

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
06:27

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

Published on: May 29, 2019

Problems in comparing particulate spectrometer and visibility meter data.

R B Loveland, J D Lindberg

    Applied Optics
    |June 12, 2010
    PubMed
    Summary
    This summary is machine-generated.

    Discrepancies in aerosol extinction measurements were found between particulate spectrometers and visibility meters in stratus clouds. Instrument design limitations, specifically the visibility meter's acceptance angle and the spectrometer's electro-optical design, cause errors at high and low aerosol extinction, respectively.

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    Last Updated: Jun 12, 2026

    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
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    Published on: May 29, 2019

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    Area of Science:

    • Atmospheric Science
    • Cloud Physics
    • Aerosol Science

    Background:

    • Accurate measurement of aerosol properties is crucial for understanding cloud formation and climate.
    • Vertical profiles of aerosol properties in low stratus clouds are important for atmospheric modeling.
    • Simultaneous data acquisition using different instruments is necessary for cross-validation.

    Purpose of the Study:

    • To investigate discrepancies between particulate spectrometers and visibility meters in measuring aerosol extinction in stratus clouds.
    • To identify the causes of measurement errors under varying aerosol extinction conditions.
    • To improve the accuracy of aerosol property measurements in cloudy environments.

    Main Methods:

    • Simultaneous data collection using particulate spectrometers and a visibility meter.
    • Application of Mie theory for calculating extinction from particulate data.
    • Analysis of discrepancies between calculated and inferred extinction values.
    • Investigation of potential instrument-specific error sources.

    Main Results:

    • Discrepancies observed between particulate spectrometer and visibility meter data, particularly at high and low aerosol extinction.
    • The limited acceptance angle of the visibility meter (integrating nephelometer) contributes to errors at high extinction.
    • Electro-optical design peculiarities of the particulate spectrometer lead to errors in aerosol density estimates at low extinction.

    Conclusions:

    • Both particulate spectrometers and visibility meters have limitations affecting aerosol extinction measurements in stratus clouds.
    • Instrument design factors significantly influence measurement accuracy under specific aerosol loading conditions.
    • Further research and instrument refinement are needed for reliable aerosol property profiling in clouds.