Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

X-ray Crystallography02:18

X-ray Crystallography

The size of the unit cell and the arrangement of atoms in a crystal may be determined from measurements of the diffraction of X-rays by the crystal, termed X-ray crystallography.
Diffraction
Diffraction is the change in the direction of travel experienced by an electromagnetic wave when it encounters a physical barrier whose dimensions are comparable to those of the wavelength of the light. X-rays are electromagnetic radiation with wavelengths about as long as the distance between neighboring...
Types of Coprecipitation01:10

Types of Coprecipitation

Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
Determination of Crystal Structures01:29

Determination of Crystal Structures

In the late 1800s, the revelation that light extended beyond visible wavelengths led to the discovery of X-rays by Wilhelm Roentgen. Recognized as high-energy electromagnetic radiation with short wavelengths, X-rays prompted exploration into their interaction with crystals. Max von Laue proposed in 1912 that the periodic arrangement of atoms, ions, or molecules in crystals would cause them to diffract X-rays, a hypothesis confirmed through experiments with copper sulfate and zinc sulfide...
Ionic Crystal Structures02:42

Ionic Crystal Structures

Ionic crystals consist of two or more different kinds of ions that usually have different sizes. The packing of these ions into a crystal structure is more complex than the packing of metal atoms that are the same size.
Most monatomic ions behave as charged spheres, and their attraction for ions of opposite charge is the same in every direction. Consequently, stable structures for ionic compounds result (1) when ions of one charge are surrounded by as many ions as possible of the opposite...
Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
Metallic Solids02:37

Metallic Solids

Metallic solids such as crystals of copper, aluminum, and iron are formed by metal atoms. The structure of metallic crystals is often described as a uniform distribution of atomic nuclei within a “sea” of delocalized electrons. The atoms within such a metallic solid are held together by a unique force known as metallic bonding that gives rise to many useful and varied bulk properties.
All metallic solids exhibit high thermal and electrical conductivity, metallic luster, and malleability. Many...

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Backscattering properties of quasi-horizontally oriented ice crystals for scanning lidars with small tilt angles.

Optics express·2025
Same author

Backscattering properties of randomly oriented hexagonal hollow columns for lidar application.

Optics express·2023
Same author

Degree of linear polarization of light at backscattering by a single large particle of irregular shape.

Optics letters·2023
Same author

Lidar backscatter simulation for angular scanning of cirrus clouds with quasi-horizontally oriented ice crystals.

Optics letters·2022
Same author

Radar-lidar ratio for ice crystals of cirrus clouds.

Optics express·2021
Same author

Wavelength dependence of ice cloud backscatter properties for space-borne polarization lidar applications.

Optics express·2020

Related Experiment Video

Updated: May 9, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Backscattering by hexagonal ice crystals of cirrus clouds.

Anatoli Borovoi1, Alexander Konoshonkin, Natalia Kustova

  • 1V.E. Zuev Institute of Atmospheric Optics, Russian Academy of Sciences, Tomsk, Russia. borovoi@iao.ru

Optics Letters
|August 2, 2013
PubMed
Summary

Light backscattering from cirrus cloud ice crystals was analyzed. Researchers found a specific hollow in the depolarization ratio for long hexagonal columns near the backward direction.

More Related Videos

Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity
08:46

Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity

Published on: January 15, 2014

A Microfluidic Approach for the Study of Ice and Clathrate Hydrate Crystallization
08:01

A Microfluidic Approach for the Study of Ice and Clathrate Hydrate Crystallization

Published on: August 18, 2022

Related Experiment Videos

Last Updated: May 9, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity
08:46

Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity

Published on: January 15, 2014

A Microfluidic Approach for the Study of Ice and Clathrate Hydrate Crystallization
08:01

A Microfluidic Approach for the Study of Ice and Clathrate Hydrate Crystallization

Published on: August 18, 2022

Area of Science:

  • Atmospheric optics
  • Cloud physics
  • Light scattering

Background:

  • Cirrus clouds are composed of ice crystals and significantly impact Earth's radiative budget.
  • Understanding light scattering by these crystals is crucial for climate modeling and remote sensing.
  • Previous studies have focused on various crystal shapes and orientations, but fine angular structures require detailed investigation.

Purpose of the Study:

  • To investigate light backscattering by randomly oriented hexagonal ice crystals in cirrus clouds.
  • To analyze the fine angular structure of Mueller matrix elements near the backward direction.
  • To derive and discuss an approximate equation for the differential scattering cross section and its spectral dependence.

Main Methods:

  • Application of the physical-optics approximation for light scattering calculations.
  • Detailed computation of Mueller matrix elements in the vicinity of the backward direction.
  • Derivation of an approximate equation for the differential scattering cross section.

Main Results:

  • The fine angular structure of Mueller matrix elements near the backward direction was calculated and discussed.
  • A simple spectral dependence of the differential scattering cross section was obtained.
  • A distinct hollow in the linear depolarization ratio was observed around the exact backward direction for long hexagonal columns.

Conclusions:

  • The physical-optics approximation provides detailed insights into light backscattering by cirrus ice crystals.
  • The derived approximate equation offers a simplified way to understand spectral dependencies.
  • The revealed hollow in depolarization ratio is a characteristic feature for specific ice crystal habits (long hexagonal columns) and can be used for remote sensing applications.