Includes bibliographical references (p. -338) and index.
|Statement||Terence J. Hughes.|
|LC Classifications||GB2403.2 .H84 1998|
|The Physical Object|
|Pagination||xi, 343 p. :|
|Number of Pages||343|
|LC Control Number||96028246|
Linking the history of the planet with the lives of those who studied it, Sarah Dry follows the remarkable scientists who summited volcanic peaks to peer through an atmosphere’s worth of water vapor, cored mile-thick ice sheets to uncover the Earth’s ancient climate history, and flew inside storm clouds to understand how small changes in energy can produce both massive storms and the general 5/5(2). Dynamics of Ice Sheets and Glaciers presents an introduction to the dynamics and thermodynamics of flowing ice masses on Earth. Based on an outline of general continuum mechanics, the different initial-boundary-value problems for the flow of ice sheets, ice shelves, ice caps and glaciers are. Ice Sheets. While we have seen that the world's glaciers are melting en masse, and at an accelerating rate, we have not yet addressed the behavior of the two largest glaciers in the world — glaciers that are so large, we call them continental ice sheets. There are two continental ice sheets — the Greenland ice sheet and the Antarctic Ice Sheet. This goes back a ways (to , in fact) but "The Ice Schooner" is what occurred to me immediately. To be honest, I don't remember the details of the book - just the arresting image of a frozen Earth with large ships sailing over the ice. By the way, the vessels in question are square-riggers, not schooners.
Ice Ages> is an informative book for a general reader having an interest in geology with an emphasis on earth's ice ages and their causes. Written by the late John Imbrie and his daughter Katherine, this substantive work names the experts going back in time to Louis Agassiz and the several pioneers who pointed him in the right direction in glacial by: An ice sheet is a mass of glacial ice more t square kilometers (19, square miles). Ice sheets contain about 99% of the freshwater on Earth, and are sometimes called continental glaciers. As ice sheets extend to the coast and over the ocean, they become ice shelves. Home» Operations Info The following documents have been assembled to help manage and plan your operations and are the result 25 plus years in the ice rink business. We have selected some of the most requested and needed information from our extensive library of documentation and information with the intent of making your job of running an ice. Fast Synthetic Ice. D1 Glide Infused Pro Self Lubricated Synthetic Ice is the fastest synthetic ice surface available today. More consumers, municipalities, hockey training facilities and professional hockey players will choose D1 synthetic ice over other available brands.
Antarctic Ice Sheet. The Antarctic ice sheet is the largest single mass of ice on Earth. It covers almost 14 million square kilometers, has 30 million cubic kilometers of ice, and holds approximately 90 percent of the freshwater on our planet. If melted, the Antarctic ice sheet would raise sea levels by meters. In particular, the dynamics of marine ice sheets (ice sheets on a bed that would be below sea level after removal of ice and full isostatic rebound) is a subject of continuous research. This interest stems from the fact that the West Antarctic Ice Sheet is a marine ice sheet which, according to some workers, may be close to a complete collapse. In his new book “The Ice at the End of the World: An Epic Journey into Greenland’s Buried Past and Our Perilous Future” (Random House, pp., ★★★½ out of four), Jon Gertner makes a compelling case that it’s time to start thinking seriously about Greenland and its growing relevance to our lives, and those of our descendants. 2. Ice Afloat—Ice Shelves, Icebergs, and Sea Ice 3. Impermanent Permafrost 4. Darkening Mountains—Disappearing Glaciers 5. The Greenland Ice Sheet 6. Antarctica: The Giant Ice Locker 7. From Greenhouse to Icehouse 8. Return to the Greenhouse 9. The Importance of Ice Appendix A. Anticipating Future Climate Change.