Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

The Forms of Water in Clouds and Rivers, Ice, and Glaciers

View through CrossRef
John Tyndall (1820–93) was an Irish physicist who became fascinated by mountaineering after a scientific expedition to Switzerland in 1856. He traversed the summit of the Matterhorn in 1868 and climbed Mount Blanc three times. Alongside this love of mountains was a scientific interest in glaciers and ice formations. Tyndall was also well-regarded for his ability to communicate with the public about science. Many of his books, such as this one, published in 1872 as part of the International Scientific Series, are aimed at the general reader. Tyndall uses this work to explain many aspects of water, beginning with cloud formation and rain before moving on to ice, snow and glaciers. He also discusses the principles behind phenomena ranging from tropical rains to glacial movement. Illustrated and organised into 493 different points under themed headings, this book gives clear explanations of the complexity of the earth's water system.
Cambridge University Press
Title: The Forms of Water in Clouds and Rivers, Ice, and Glaciers
Description:
John Tyndall (1820–93) was an Irish physicist who became fascinated by mountaineering after a scientific expedition to Switzerland in 1856.
He traversed the summit of the Matterhorn in 1868 and climbed Mount Blanc three times.
Alongside this love of mountains was a scientific interest in glaciers and ice formations.
Tyndall was also well-regarded for his ability to communicate with the public about science.
Many of his books, such as this one, published in 1872 as part of the International Scientific Series, are aimed at the general reader.
Tyndall uses this work to explain many aspects of water, beginning with cloud formation and rain before moving on to ice, snow and glaciers.
He also discusses the principles behind phenomena ranging from tropical rains to glacial movement.
Illustrated and organised into 493 different points under themed headings, this book gives clear explanations of the complexity of the earth's water system.

Related Results

Ground ice detection and implications for permafrost geomorphology
Ground ice detection and implications for permafrost geomorphology
Most permafrost contains ground ice, often as pore ice or thin veins or lenses of ice. In certain circumstance, larger bodies of ice can form, such as ice wedges, or massive lenses...
Modelling very recent ice ages on Mars with the Planetary Climate Model
Modelling very recent ice ages on Mars with the Planetary Climate Model
Protected by centimeters of dry sediments, a planetary-scale mantle of relatively pure water ice covers the entire mid and high latitudes of Mars. Its presence down has been shown ...
Surface velocity and ice thickness of the Müller ice cap, Axel Heiberg Island
Surface velocity and ice thickness of the Müller ice cap, Axel Heiberg Island
Muller ice cap is situated on Axel Heiberg Island in Arctic Canada. It is characterised by a mountanious region separating the ice cap in the east from the outlet glaciers in the w...
Physical processes in polar stratospheric ice clouds
Physical processes in polar stratospheric ice clouds
A one‐dimensional model of cloud microphysics has been used to simulate the formation and evolution of polar stratospheric ice clouds. The model results are in general agreement wi...
Ice Management for Floating Ice Offshore Operations
Ice Management for Floating Ice Offshore Operations
Abstract This paper describes the practicalities and principles of use of icebreakers in support of ice offshore operations, and specifically their efficiency in ...
Constraining Ceres' exposed ice: grain size, abundance, and is it salty?
Constraining Ceres' exposed ice: grain size, abundance, and is it salty?
Ubiquitous phyllosilicates and carbonates in Ceres’ surface regolith reveal extensive water-rock interaction in the past [1]. A key area of continued study is the water i...
Grain growth of polycrystalline ice doped with soluble impurities
Grain growth of polycrystalline ice doped with soluble impurities
The grain size of polycrystalline ice affects key parameters related to planetary evolution such as the rheological and dielectric properties of Earth's glaciers and ice sheets as ...
Effect of ocean heat flux on Titan's topography and tectonic stresses
Effect of ocean heat flux on Titan's topography and tectonic stresses
INTRODUCTIONThe thermo-mechanical evolution of Titan's ice shell is primarily controlled by the mode of the heat transfer in the ice shell and the amount of heat coming from the oc...

Back to Top