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 .
To save content items to your Kindle, first ensure no-reply@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.
Images from the MESSENGER spacecraft show that irregular, flat-floored depressions with high-reflectance interiors and haloes are common on the surface of planet Mercury. These landforms, called hollows, are among Mercury's youngest non-impact features and may be forming today. Hollows are unique to Mercury, with no close equivalent on other planetary bodies. Clues to understanding hollows come from consideration of morphological features associated with ice-bearing surfaces on Mars and icy satellites, and of processes leading to loss of sulfur from asteroids. Evidence suggests that hollows form when sublimation or destruction of a volatile-bearing phase weakens the host rock, causing collapse and scarp retreat. The phase susceptible to loss may be a sulfide mineral or graphite. Loss of the volatile component could be driven by solar heating, exposure to solar ultraviolet radiation, exposure to the solar wind, sputtering by magnetospheric ions, and micrometeoroid bombardment. The depth to which hollows grow may be controlled by accumulation of a protective lag deposit. The volatile-bearing phase that is lost appears to be a pervasive component of the host rock, but in some cases the hollow-forming phase may have been concentrated by volcanic processes or differentiation of impact melts.
Images from the MESSENGER spacecraft show that irregular, flat-floored depressions with high-reflectance interiors and haloes are common on the surface of planet Mercury. These landforms, called hollows, are among Mercury's youngest non-impact features and may be forming today. Hollows are unique to Mercury, with no close equivalent on other planetary bodies. Clues to understanding hollows come from consideration of morphological features associated with ice-bearing surfaces on Mars and icy satellites, and of processes leading to loss of sulfur from asteroids. Evidence suggests that hollows form when sublimation or destruction of a volatile-bearing phase weakens the host rock, causing collapse and scarp retreat. The phase susceptible to loss may be a sulfide mineral or graphite. Loss of the volatile component could be driven by solar heating, exposure to solar ultraviolet radiation, exposure to the solar wind, sputtering by magnetospheric ions, and micrometeoroid bombardment. The depth to which hollows grow may be controlled by accumulation of a protective lag deposit. The volatile-bearing phase that is lost appears to be a pervasive component of the host rock, but in some cases the hollow-forming phase may have been concentrated by volcanic processes or differentiation of impact melts.
Gamma-ray bursts (GRBs) are the most luminous explosions in the universe, which within seconds release energy comparable to what the Sun releases in its entire lifetime. The field of GRBs has developed rapidly and matured over the past decades. Written by a leading researcher, this text presents a thorough treatment of every aspect of the physics of GRBs. It starts with an overview of the field and an introduction to GRB phenomenology. After laying out the basics of relativity, relativistic shocks, and leptonic and hadronic radiation processes, the volume covers all topics related to GRBs, including a general theoretical framework, afterglow and prompt emission models, progenitor, central engine, multi-messenger aspects (cosmic rays, neutrinos, and gravitational waves), cosmological connections, and broader impacts on fundamental physics and astrobiology. It is suitable for advanced undergraduates, graduate students, and experienced researchers in the field of GRBs and high-energy astrophysics in general.
This book chronicles the history of climate science and planetary exploration, focusing on our ever-expanding knowledge of Earth's climate, and the parallel research underway on some of our nearest neighbours: Mars, Venus and Titan. From early telescopic observation of clouds and ice caps on planetary bodies in the seventeenth century, to the dawn of the space age and the first robotic planetary explorers, the book presents a comprehensive chronological overview of planetary climate research, right up to the dramatic recent developments in detecting and characterising exoplanets. Meanwhile, the book also documents the discoveries about our own climate on Earth, not only about how it works today, but also how profoundly different it has been in the past. Highly topical and written in an accessible and engaging narrative style, this book provides invaluable historical context for students, researchers, professional scientists, and those with a general interest in planetary climate research.
The Cassini Orbiter mission, launched in 1997, has provided state-of-the-art information into the origins and workings of Saturn. Drawing from new discoveries and scientific insight from the mission, this book provides a detailed overview of the planet as revealed by Cassini. Chapters by eminent planetary scientists and researchers from across the world comprehensively review the current state of knowledge regarding Saturn's formation, interior, atmosphere, ionosphere, thermosphere and magnetosphere. Specialised chapters discuss the planet's seasonal variability; the circulation of strong zonal winds; the constantly changing polar aurorae; and the Great Storm of 2010–2011, the most powerful convective storm ever witnessed by humankind. Documenting the latest research on the planet, from its formation to how it operates today, this is an essential reference for graduate students, researchers and planetary scientists.