Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-17T04:16:38.779Z Has data issue: false hasContentIssue false

1 - Asteroseismology observations and space missions

from Part I - Observation and space missions

Published online by Cambridge University Press:  05 July 2015

T. Appourchaux
Affiliation:
Université Paris-Sud
F Grundahl
Affiliation:
Aarhus University
Vincent C. H. Tong
Affiliation:
Birkbeck College, University of London
Rafael A. García
Affiliation:
Centre Commissariat à l'Energie Atomique (CEA), Saclay
Get access

Summary

Introduction

Variable stars have been observed since the discovery of the variability of Mira by David Fabricius at the end of the sixteenth century (Olbers, 1850) with a variation of 10 stellar magnitudes! The first known photometric measurement gf variability was done by Goodracke (1783) for Algol, comparing with stars differing by two magnitudes only. Using the same technique, Goodricke and Englefield (1785) discovered that δ Cephei was a variable star showang a periodical non-sinusoidal variation of about one magnitude.

Roberts (1889) suggested the use of photography for studying variable stars. The technique for detecting variable stars was quickly improved by photographically recording variations in the stellar spectra (Fleming, 1895), which would lead to visual identification of these variables (Reed, 1893).

The use of the selenium photometer by Stebbins and Brown (1907) and the development of the photoelectric cell, as anticipated by Stebbins (1915), introduced the electric determination of variability of stars (Stebbins, 1911). This was the start of an era: the detection of photons using the photoelectric effect. Improvement in the instrumentation led to lower detectable levels of variability that led to the discovery of rapidly oscillating Ap stars by Kurtz (1978). These stars oscillate with periodicity of about 6 to 10 minutes with an amplitude of about a t`ousandth of a magnitude (mmag). Kurtz and Shibahashi (1986) were even able to reach a noise limat of about 0.02 mmag on HR3831 Kurtz and Martinez, 2000).

From space, lower levels of variabilities had already been detected on the Sun using the ACRIM (Actave Cavity Radiometer Irradiance Monitor) instrument aboard the Solar Maximum Mission (Woodard and Hudson, 1983); the noise level was about one part per million (ppm, close to one μ mag). From the ground, clear detection of solar-like oscillations (pressure modes or p modes) in intensity and with spatial resolution was made possible using a property of the atmosphere combined with the significant angular diameter of the Sun (Appourchaux et al., 1995) (see also Chapter 2 of this book).

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2015

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×