Skip to main content Accessibility help
×
Hostname: page-component-76fb5796d-vvkck Total loading time: 0 Render date: 2024-04-26T13:29:38.693Z Has data issue: false hasContentIssue false

33 - Meteor showers on other planets

from Part VI - Impact and relevance of meteor showers

Published online by Cambridge University Press:  05 July 2015

Peter Jenniskens
Affiliation:
The SETI Institute, California
Get access

Summary

Some day in the future, we will perhaps travel to Mars or Venus to watch a particularly nice meteor shower. Super fast meteoroids entering at 85 km/s, or meteors in slow-motion at 5 km/s. Until that time, remote observing and robotic missions may glimpse these meteors, or in the absence of an atmosphere, the impact flashes. They will probe the large-grain dust environment away from Earth's orbit and sample comets not encountered by Earth. And they probe the ablation process in atmospheres more like that of the early Earth. A call to include meteor surveys on space landers has been made.

Meteoroid impacts may also be traced from the neutral atom debris layers (and their associated narrow ionospheric layers of electrons) that they leave behind high in the atmosphere. Theoretical models predict that such layers exist at Venus, Mars, Jupiter, Saturn, Neptune, and Saturn's moon Titan. Even the sparse atmospheres of Triton and Pluto may on occasion be lit up by slow meteors.

33.1 Meteor showers on the Moon

Our Moon does not have a permanent atmosphere, but impact flashes have been observed. Meteoroids hit the surface continuously. They add meteoric metals to the Moon's surface and are responsible for the release of the sodium atoms that cause our Moon's sodium atmosphere.

In 1939, Lincoln LaPaz estimated that 5 kg sized boulders hitting the Moon would produce visible flashes at a rate of 10 a year. Unconfirmed reports of impact flashes included that of F. H. Thornton, who detected a point of light on the floor of Plato in October of 1945. In August of 1948, A. J. Woodward saw a flash “like a bright sparkle of frost” that lasted three seconds. He described it as having “the appearance of an object striking the moon.” Another case was that of H. P. Wilkins, who observed a 1 s point of light in the crater Gassendi in May of 1951. Coordinated attempts by the Association of Lunar and Planetary Observers (ALPO) to observe such impacts, a project coordinated by Robert M. Adams from 1955 to 1965, never succeeded in obtaining simultaneous, independent observations of “Lunar transient phenomena.”

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2006

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
×