Book contents
- The Global Cryosphere, Second Edition
- Reviews
- The Global Cryosphere
- Copyright page
- Contents
- Preface
- Acknowledgments
- 1 Introduction
- Part I The terrestrial cryosphere
- 2A Snowfall and snow cover
- 2B Avalanches
- 3 Glaciers and ice caps
- 4 Ice sheets
- 5 Frozen ground and permafrost
- 6 Freshwater ice
- Part II The marine cryosphere
- Part III The cryosphere past and future
- Part IV Applications
- References
- Index
- Plate Section (PDF Only)
2A - Snowfall and snow cover
from Part I - The terrestrial cryosphere
Published online by Cambridge University Press: 15 April 2022
- The Global Cryosphere, Second Edition
- Reviews
- The Global Cryosphere
- Copyright page
- Contents
- Preface
- Acknowledgments
- 1 Introduction
- Part I The terrestrial cryosphere
- 2A Snowfall and snow cover
- 2B Avalanches
- 3 Glaciers and ice caps
- 4 Ice sheets
- 5 Frozen ground and permafrost
- 6 Freshwater ice
- Part II The marine cryosphere
- Part III The cryosphere past and future
- Part IV Applications
- References
- Index
- Plate Section (PDF Only)
Summary
Terrestrial snow cover occupies higher latitude areas of the Northern Hemisphere (NH) from several up to 9 months each year in the Arctic land surface, with significant influence on the surface energy budget, subsoil thermal regime, and the freshwater storage. Snow cover also interacts with vegetation and affects terrestrial habitats and species.
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- Information
- The Global CryospherePast, Present, and Future, pp. 15 - 86Publisher: Cambridge University PressPrint publication year: 2022
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