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Related Concept Videos

Variation of Atmospheric Pressure01:18

Variation of Atmospheric Pressure

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...
Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

Influence of Earth's Curvature and Atmospheric Refraction on Leveling

During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance. Over a...
What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Application of Linearization and Approximation01:29

Application of Linearization and Approximation

A drone flying through complex terrain often relies on more than one sensing method to estimate small changes in altitude. Along with direct measurements, air pressure provides a useful indirect indicator of vertical movement. Atmospheric pressure decreases as altitude increases, and this relationship is commonly described using an exponential model. Although accurate, converting pressure measurements into altitude values requires calculations that are too complex to perform repeatedly during...
Boundary Layer Characteristics01:18

Boundary Layer Characteristics

When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
What is Weather?01:07

What is Weather?

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Related Experiment Video

Updated: Jun 8, 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

Variability in atmospheric light-scattering properties with altitude.

F W Gibson

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

    This study measured atmospheric angular scattering properties using a balloonborne polar nephelometer. Aerosol characteristics like size distribution were inferred from scattering data at different altitudes.

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    Last Updated: Jun 8, 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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    11:57

    Measuring Spatially- and Directionally-varying Light Scattering from Biological Material

    Published on: May 20, 2013

    Scattering And Absorption of Light in Planetary Regoliths
    11:34

    Scattering And Absorption of Light in Planetary Regoliths

    Published on: July 1, 2019

    Area of Science:

    • Atmospheric Science
    • Aerosol Physics
    • Optical Remote Sensing

    Background:

    • Understanding aerosol properties is crucial for climate modeling.
    • Altitudinal variations in atmospheric optics influence radiation transfer.
    • Previous studies often lack detailed in situ measurements of scattering properties.

    Purpose of the Study:

    • To investigate the altitudinal variability of angular scattering properties in the troposphere and stratosphere.
    • To infer aerosol size distribution and scattering phase function using experimental parameters.
    • To explore the relationship between scattering dissymmetry, spectral turbidity, and aerosol phase function.

    Main Methods:

    • Utilized a balloonborne polar nephelometer for in situ measurements.
    • Analyzed interdependent experimental parameters to derive optical properties.
    • Correlated scattering dissymmetry with spectral dispersion in turbidity.

    Main Results:

    • Demonstrated extractability of aerosol characteristics from scattering data.
    • Provided altitude-resolved information on scattering phase function and aerosol size distribution.
    • Addressed the correlation between backscatter and extinction based on in situ observations.

    Conclusions:

    • In situ measurements provide valuable insights into aerosol optical properties.
    • Scattering dissymmetry is a key parameter for inferring aerosol characteristics.
    • The study enhances understanding of atmospheric aerosol behavior with altitude.