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Introduction to the Physics of the Cryosphere is intended for graduates with a numerical sciences background, particularly those who are heading towards postgraduate study or are generally interested in environmental physics. Conservation equations underpin the physics encompassed in this book, although the interesting part comes in how the necessary variables and boundary conditions are defined to be able to simulate changes in the cryosphere. Phase changes between ice, liquid water and water vapour also come into play.

Cryosphere. --- Physics.

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"Polar Ice and Global Warming in Cryosphere Regions" is based on recent and past climate variabilities data gathered through satellites and spatial-temporal analysis to explain the role of global warming on cryosphere regions such as high-latitude Himalaya, Arctic and Antarctic regions, and the surrounding Southern Ocean and Arctic Ocean. The featured case studies describe the atmospheric processes and their interactions with high-latitude regions helping readers better understand climate variability, and develop plans and policies for disaster risk management.Intended for researchers, academics, and graduate students following oceanography, meteorology, or environmental studies, and those working on projects related to climate change in governmental organizations, institutions, and global NGOs, this book outlines ways in which readers can initiate plans and policies to help mitigate the effects of global warming in these regions.

Cryosphere. --- Climatic changes. --- Cryosphère. --- Changements climatiques --- Cryosphère --- Remote sensing. --- Télédétection.

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The Himalaya Mountains contain not only one of the largest concentrations of ice outside the polar regions, but contribute to the hydrological requirements of large populations spread over seven nations. The exceptionally high elevations of this low-latitude cryosphere presents a natural laboratory and archives to study climate-tectonics interactions as well as regional v. global climate influences. The existing base-level data on the Himalayan cryosphere are highly variable. Several climate fluctuations occurred during the late Quaternary (MIS1-MIS5, especially the last c. 100 ka), which led to the evolution of the Himalayan landscape. Detailed studies of these archives, along with those of the present cryosphere and related hydrosphere, are essential for understanding the controls on present and future hydrology of the glacial-fed mountain rivers. This volume, a follow-up of the XII International Symposium on Antarctic Earth Science, Goa (A SCAR symposium), provides new data from locales spread over the entire Himalaya region and from Tibet. It provides a glimpse of the late Quaternary cryosphere, as well as a discussion in the last section on sustainability in the context of geohazard mitigations as well as the hydrological budget.--

Geology --- Cryosphere. --- Cryosphere. --- Geology. --- Himalaya Mountains.

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Glaciers --- Cryosphere --- Ice --- Glaciology --- Meltwater

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"Now in its fourth edition, this classic text covers the physical principles underlying the behavior of glaciers---terrestrial ice bodies originating as accumulations of snow---including mountain glaciers, small ice caps, ice sheets, and ice shelves. New and expanded chapters discuss climate change topics, including: how ice core studies obtain information about past climate and atmospheric composition; the reaction of glaciers and ice sheets to global warming; quaternary climate history and the ice ages; and the challenge of projecting future sea-level rise. The book explores many additional topics of interest to geologists and geophysicists who study tectonics and geomorphology."--Jacket.

552.96 --- Glaciers --- Cryosphere --- Ice --- Glaciology --- Meltwater