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Exploring Doppler Effect & Telescopes: Wavelength Shifts & Space Observations - Prof. Timo, Study notes of Astronomy

Explore the doppler effect, a phenomenon causing a shift in wave length due to motion of the source or observer. Learn how astronomers use large telescopes, including non-optical radio and infrared telescopes, to observe the universe at various wavelengths and gain valuable insights into the composition, temperature, and motion of celestial bodies. Discover the importance of spectroscopy in identifying unique emission and absorption spectra for each element.

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Pre 2010

Uploaded on 08/18/2009

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DopplerEffect theapparentshiftinthewavelengthofa
waveduetothemotionofthesource(ofthewave) or the
observer.
Ifthesource&observerare approaching ,thereisashiftto
shorterwavelengths="blueshift"
Ifthesource&observerare receding ,thereisashiftto
longerwavelengths="redshift"
Theamountofshiftinfrequencyispreciselydependenton
thespeedofapproachorrecessionthe"lineofsight"
velocityor"radial"velocity.
Title:May149:01AM(1of13)
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Download Exploring Doppler Effect & Telescopes: Wavelength Shifts & Space Observations - Prof. Timo and more Study notes Astronomy in PDF only on Docsity!

Doppler Effect the apparent shift in the wavelength of a

wave due to the motion of the source (of the wave) or the

observer.

If the source & observer are approaching , there is a shift to

shorter wavelengths = "blueshift"

If the source & observer are receding , there is a shift to

longer wavelengths = "redshift"

The amount of shift in frequency is precisely dependent on

the speed of approach or recession the "line of sight"

velocity or "radial" velocity.

Astronomers want large telescopes for

increased lightgathering ability

increased angular resolution

Our atmosphere distorts our views of objects in space. The

level of distortion is called the "seeing," and it gives an idea

of the smallest details visible in any telescope.

Astronomers get around limits to seeing by:

put observatories on mountain tops

observe from space or balloons

compensate with "active" control of telescope

Infrared (IR) telescopes detect the "heat" from objects/events in space like dust in clouds, young stars, "cool" objects, etc. Must be done from mountain tops, balloons, & space

Ultraviolet (UV) (must be from space) View hot stars, exploded stars, energetic events

Xray & Gammaray (must be from space) View very highenergy events, very hot stars & gas

By observing the universe at all wavelengths, we can learn much more about objects in space than we could just from one part of the spectrum.

Ch 4 Light & Other EM Radiation

Blackbody Radiation An object at a uniform temperature emits EM waves over a range of wavelengths in a particular way we callblackbody radiation. The intensity of a particular wavelength depends on the temperature of the object. With higher temperature: more energy is emitted at all wavelengths the most intense radiation is emitted at shorter wavelengths

By looking at an object's color, we can tell its temperature.

Temperature scale: We'll use the "kelvin" temperature scale. It's basically the celsius scale set to start "zero" at absolute zero instead of at the freezing point of water. water freezes at 273 K, boils at 373 K

Formation of Spectral Lines

Electrons (e's) orbit the nucleus of the atom (where the

protons [p+] and neutrons [n°] reside) in orbits with specific

energy. These orbits are distinct, there are limited number

of them in a particular element's atoms, and so the e's only

have a few specific energies available to them. As e's

change orbits, they release or absorb a single photon with a

specific energy, and, hence, specific wavelength/color.

emission line spectrum

absorption line spectrum

Each element has its own unique orbits for the e's since

each element's atoms have a specific # of p+'s in the

nucleus. Thus, each element has a unique

emission/absorption spectrum.

Formation of the Solar System

The Earth & planets formedwith the Sun out of a collapsing cloud of gas and (just a tiny bit) of dust. The gas is 3/4 H and 1/4 He, accounting for 99% of the mass.

As the cloud collapsed, the central region became very compressed an hot > the Sun.

Other material farther out "fell" or formed into a rotating disk.

Heat from the Sun drives the lighter gas out to the outer parts of the disk, leaving the small fraction of dust in the inner regions. Over a few 100 million years the dust/ice accumulates into small objects"planetesimals"a few kilometers across.

The planetesimals build into larger objects capable of growing larger by collision ("accretion") and by gravitational attraction. The larger object grow larger by "gobbling up" smaller planetesimals. At stage we call the bigger object "protoplanets."

In the outer part of the disk, the planetismals and protoplanets also grow from collecting the gas (and there's a lot more gas), forming large, gaseous planets.

We can divide the 8 planets into 2 groups.

The terrestrial planets Mercury, Venus, Earth, Mars are

close to the Sun, small, dense, rocky, rotate slowly, have few

moons, no rings...

The jovian planets Jupiter, Saturn, Uranus, Neptune are

far from the Sun, large, lowdensity, gassy/liquid, rotate

rapidly, have many moons & rings...

(Pluto doesn't fit in either group.)

Title: May 14 12:27 PM (13 of 13)

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