Snow and Ice in the Hydrosphere

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10281686" target="_blank" >RIV/00216208:11310/14:10281686 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/B978-0-12-394849-6.00004-4" target="_blank" >http://dx.doi.org/10.1016/B978-0-12-394849-6.00004-4</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/B978-0-12-394849-6.00004-4" target="_blank" >10.1016/B978-0-12-394849-6.00004-4</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Snow and Ice in the Hydrosphere

Popis výsledku v původním jazyce

In large areas of the world, runoff and other hydrological variables are controlled by the spatial and temporal variation of the 0 C isotherm, which is central for the temporal storage of precipitation as snow or ice. This storage is of crucial importance for the seasonal distribution of snow and ice melt, a major component of the movement of water in the global water cycle. This chapter provides an introduction to the role of snow and ice in the hydrosphere by discussing topics including snowpack characteristics, snow observation approaches, the energy balance of snow-covered areas, and modeling of snowmelt. Furthermore, the role of glaciers and glacial mass balances, including modeling glacier discharge, is discussed. Finally, an overview of the hydrology of snow- and ice-covered catchments is given, and the influence of snow, glaciers, river ice, and frozen soils on discharge is discussed.

Název v anglickém jazyce

Snow and Ice in the Hydrosphere

Popis výsledku anglicky

In large areas of the world, runoff and other hydrological variables are controlled by the spatial and temporal variation of the 0 C isotherm, which is central for the temporal storage of precipitation as snow or ice. This storage is of crucial importance for the seasonal distribution of snow and ice melt, a major component of the movement of water in the global water cycle. This chapter provides an introduction to the role of snow and ice in the hydrosphere by discussing topics including snowpack characteristics, snow observation approaches, the energy balance of snow-covered areas, and modeling of snowmelt. Furthermore, the role of glaciers and glacial mass balances, including modeling glacier discharge, is discussed. Finally, an overview of the hydrology of snow- and ice-covered catchments is given, and the influence of snow, glaciers, river ice, and frozen soils on discharge is discussed.

Druh

C - Kapitola v odborné knize

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název knihy nebo sborníku

Snow and Ice-Related Hazards, Risks, and Disasters

ISBN

978-0-12-394849-6

Počet stran výsledku

39

Strana od-do

99-137

Počet stran knihy

762

Název nakladatele

Elsevier

Místo vydání

Amsterdam, Netherlands

Kód UT WoS kapitoly

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