atmospheric tide sentence in Hindi
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- Ii ) Atmospheric tides propagate in an atmosphere where density varies significantly with height.
- Atmospheric tides can be measured as regular fluctuations in wind, temperature, density and pressure.
- Although atmospheric tides share much in common with ocean tides they have two key distinguishing features:
- Atmospheric pressure shows a diurnal or semidiurnal ( twice-daily ) cycle caused by global atmospheric tides.
- Similarly, atmospheric tides arise from, for example, non-uniform solar heating associated with diurnal motion.
- Atmospheric tides dominate the dynamics of the mesosphere and lower thermosphere, essential to understanding the atmosphere as a whole.
- Lindzen's work on atmospheric tides led him to the study of planetary waves and the general circulation of atmospheres.
- At ground level, atmospheric tides can be detected as regular but small oscillations in surface pressure with periods of 24 and 12 hours.
- This led to their joint publication in 1969 of a 186-page monograph ( republished in 1970 as a book ) " Atmospheric Tides ".
- I ) Atmospheric tides are primarily excited by the Sun's heating of the atmosphere whereas ocean tides are primarily excited by the Moon's gravitational field.
- In addition to oceanic tides, large lakes can experience small tides and even planets can experience " atmospheric tides " and " Earth tides ".
- Hence, atmospheric tides are eigenoscillations ( eigenmodes ) of Earth's atmosphere with eigenfunctions \ Theta _ n, called Hough functions, and eigenvalues \ varepsilon _ n.
- The largest-amplitude atmospheric tides are mostly generated in the troposphere and stratosphere when the atmosphere is periodically heated, as water vapor and ozone absorb solar radiation during the day.
- While holding the position of Research Scientist at the Sydney Chapman, who had contributed to the theory of atmospheric tides in a number of papers from the 1920s through to the 1940s.
- In the mesosphere ( heights of ~ 50 100 km ) atmospheric tides can reach amplitudes of more than 50 m / s and are often the most significant part of the motion of the atmosphere.
- In the mesosphere ( heights of ~ 50 & ndash; 100 km ) atmospheric tides can reach amplitudes of more than 50 m / s and are often the most significant part of the motion of the atmosphere.
- There are so-called atmospheric tides and other density variations that could give you a " substantial " boost in pressure, improving your odds with any space shot depending on balloons or aircraft to get much of the height.
- Note that although solar heating is responsible for the largest-amplitude atmospheric tides, the gravitational fields of the Sun and Moon also raise tides in the atmosphere, with the lunar gravitational atmospheric tidal effect being significantly greater than its solar counterpart.
- This means that most atmospheric tides have periods of oscillation related to the 24-hour length of the solar day whereas ocean tides have longer periods of oscillation related to the lunar day ( time between successive lunar transits ) of about 24 hours 51 minutes.
- While at Birmingham he began his work on nuclear plasma, superconductivity and atmospheric tides induced by absorption of solar radiation in the ozone layer; for these contributions he was awarded the Thomas Ranken Lyle Medal from the Australian Academy of Science and a DSc from the Australian National University.
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