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Related Concept Videos

Intermolecular Forces03:13

Intermolecular Forces

Atoms and molecules interact through bonds (or forces): intramolecular and intermolecular. The forces are electrostatic as they arise from interactions (attractive or repulsive) between charged species (permanent, partial, or temporary charges) and exist with varying strengths between ions, polar, nonpolar, and neutral molecules. The different types of intermolecular forces are ion–dipole, dipole–dipole, hydrogen bonds, and dispersion; among these, dipole–dipole, hydrogen bonds, and dispersion...
Intermolecular Forces03:13

Intermolecular Forces

Atoms and molecules interact through bonds (or forces): intramolecular and intermolecular. The forces are electrostatic as they arise from interactions (attractive or repulsive) between charged species (permanent, partial, or temporary charges) and exist with varying strengths between ions, polar, nonpolar, and neutral molecules. The different types of intermolecular forces are ion–dipole, dipole–dipole, hydrogen bonds, and dispersion; among these, dipole–dipole, hydrogen bonds, and dispersion...
Acceleration due to Gravity on Other Planets01:24

Acceleration due to Gravity on Other Planets

The gravitational acceleration of an object near the Earth's surface is called the acceleration due to gravity. It can be measured by conducting simple experiments on Earth. However, such an experiment is impossible to conduct on the surface of other planets.
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Escape Velocities of Gases01:19

Escape Velocities of Gases

To escape the Earth's gravity, an object near the top of the atmosphere at an altitude of 100 km must travel away from Earth at 11.1 km/s. This speed is called the escape velocity. The temperature at which gas molecules attain the rms speed, which is equal to the escape velocity, can be estimated by using the equation for the average kinetic energy of the gas molecules. According to the kinetic theory of gas, the average kinetic energy of the gas molecules is proportional to its temperature.
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...
Planes in Space01:31

Planes in Space

A plane in three-dimensional space is fundamentally characterized by a point that lies on the plane and a normal vector that is perpendicular to its surface. This normal vector uniquely determines the orientation of the plane, making it an essential geometric descriptor. In architectural applications, such as the installation of a sloped glass panel on a building façade, this mathematical model provides a precise representation of the panel’s position and orientation in space.Let r₀ be the...

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Related Experiment Video

Updated: Jul 9, 2026

Bringing the Visible Universe into Focus with Robo-AO
10:35

Bringing the Visible Universe into Focus with Robo-AO

Published on: February 12, 2013

An intense stratospheric jet on Jupiter.

F M Flasar1, V G Kunde, R K Achterberg

  • 1NASA/Goddard Space Flight Center, Code 693, Greenbelt, Maryland 20771, USA. f.m.flasar@nasa.gov

Nature
|January 9, 2004
PubMed
Summary

Jupiter

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Area of Science:

  • Planetary Science
  • Atmospheric Science
  • Aerospace Engineering

Background:

  • Earth's stratosphere exhibits quasi-biennial oscillation (QBO) affecting global weather.
  • Jupiter's stratosphere may have similar temperature oscillations, but data are limited.
  • Previous Jupiter studies lacked vertical resolution and wind velocity data.

Purpose of the Study:

  • To map Jupiter's stratospheric temperatures and winds with high spatial resolution.
  • To investigate atmospheric oscillations on Jupiter.
  • To compare Jovian atmospheric dynamics with Earth's QBO.

Main Methods:

  • Spacecraft measurements of infrared spectra from Jupiter's stratosphere.
  • Analysis of temperature and wind velocity data.
  • High-resolution spatial mapping of atmospheric phenomena.

Main Results:

  • Discovery of an intense, high-altitude equatorial jet (approx. 140 m/s).
  • Identification of a quasi-quadrennial oscillation in the equatorial jet's structure.
  • Observation of stratospheric wave activity analogous to Earth's.
  • Mapping of polar hot spots penetration into the stratosphere.

Conclusions:

  • Jupiter's stratosphere exhibits complex dynamics, including oscillations and wave activity similar to Earth's QBO.
  • High-resolution data reveal detailed atmospheric jet structures and interactions.
  • Plasma environment significantly influences Jupiter's upper atmosphere and stratosphere.