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Related Concept Videos

Attenuated Total Reflectance (ATR) Infrared Spectroscopy: Overview01:13

Attenuated Total Reflectance (ATR) Infrared Spectroscopy: Overview

Attenuated total reflectance (ATR) infrared spectroscopy is a powerful analytical technique used to study the composition of materials. It is widely employed in chemistry, materials science, forensic science, and other fields where sample characterization is required. ATR has several advantages over traditional transmission IR spectroscopy, including the requirement of little to no sample preparation and the ability to analyze a wide range of samples.
The ATR process begins by directing a beam...
IR Spectrum01:19

IR Spectrum

When infrared (IR) radiation passes through a molecule, the bonds stretch or bend by absorbing the radiation. This absorption creates the molecule's absorption spectrum, which is the plot of its percentage transmittance versus wavenumber.
Transmittance is defined as the ratio of the radiant power passing through a sample to that from the radiation's source. Multiplying the transmittance by 100 gives the percent transmittance (%T), which varies between 100% (no absorption) and 0% (complete...
Infrared (IR) Spectroscopy: Overview01:09

Infrared (IR) Spectroscopy: Overview

When electromagnetic radiation passes through a material, atoms or molecules transition from a lower to a higher energy state by absorbing radiation corresponding to the energy difference between the two states. The absorption of infrared (IR) radiation causes transitions between vibrational energy levels in a molecule. Therefore, IR spectroscopy is a useful analytical tool for determining the molecular structure of molecules.
Different compounds display unique properties due to their...
IR Frequency Region: Fingerprint Region01:03

IR Frequency Region: Fingerprint Region

IR spectra are divided into two main regions: the diagnostic region and the fingerprint region. The diagnostic region of the spectrum lies above 1500 cm−1. The absorptions resulting from single-bond vibrations of the N–H, C–H, and O–H stretch at higher wavenumbers and appear on the left side of the spectrum. The stretching absorptions of the C≡C and C≡N occur between 2100–2300 cm−1. In contrast, those arising from stretching absorptions of the C=O, C=N, and C=C occur between 1600–1850 cm−1.
The...
IR Spectrum Peak Intensity: Amount of IR-Active Bonds00:55

IR Spectrum Peak Intensity: Amount of IR-Active Bonds

When infrared radiation is passed through a molecule, absorption occurs if the molecule's vibration leads to a substantial change in its bond dipole moment. Transitions between vibrational energy levels, typically corresponding to infrared frequencies (4000–400 cm−1), allow absorption if the vibration significantly alters the dipole moment, making the molecule infrared active. The molecular bonds have different stretching and bending vibrations, resulting in various peaks with varying...
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...

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Related Experiment Video

Updated: Jun 17, 2026

The Use of High-resolution Infrared Thermography (HRIT) for the Study of Ice Nucleation and Ice Propagation in Plants
09:36

The Use of High-resolution Infrared Thermography (HRIT) for the Study of Ice Nucleation and Ice Propagation in Plants

Published on: May 8, 2015

Infrared reflectance of high altitude clouds.

W A Hovis, L R Blaine, M L Forman

    Applied Optics
    |January 16, 2010
    PubMed
    Summary

    Spectral reflectance differences were found between ice clouds, jet contrails, and snow. These findings aid in remote sensing of cloud types from satellites.

    Area of Science:

    • Atmospheric Science
    • Remote Sensing
    • Spectroscopy

    Background:

    • Accurate identification of cloud types is crucial for climate modeling and weather forecasting.
    • Distinguishing between natural ice clouds, artificial contrails, and surface features is challenging for satellite remote sensing.

    Purpose of the Study:

    • To investigate the spectral reflectance characteristics of cirrostratus, cirrus clouds, and jet contrails.
    • To determine if spectral signatures can differentiate between natural ice clouds, fresh jet contrails, and snow-covered surfaces.

    Main Methods:

    • Spectral reflectance measurements were conducted using a down-looking spectrometer.
    • Data acquisition was performed from a high-altitude aircraft platform.
    • The spectral interval of interest was 0.68–2.4 micrometers.

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    Improving Infrared Spectroscopy Characterization of Soil Organic Matter with Spectral Subtractions
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    The Use of High-resolution Infrared Thermography (HRIT) for the Study of Ice Nucleation and Ice Propagation in Plants
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    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
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    Improving Infrared Spectroscopy Characterization of Soil Organic Matter with Spectral Subtractions

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    Main Results:

    • Distinct spectral reflectance signatures were observed for cirrostratus, cirrus clouds, and jet contrails.
    • Significant differences were identified between the spectral signatures of ice clouds and a fresh jet contrail.
    • The spectral data also showed clear distinctions between these cloud types and a snow-covered surface.

    Conclusions:

    • Spectral reflectance analysis provides a viable method for differentiating between various ice cloud types and jet contrails.
    • These findings support the development of improved algorithms for cloud type classification in satellite remote sensing.
    • Understanding these spectral differences is essential for accurate atmospheric and climate studies.