Assessment of surface albedo effect on the position of zero isotherm

Calculations with one-layer radiative model of the atmosphere based upon the data of Surface Radiation Budget archive over 1984–2007 allowed to assess changes in temperature distribution over the earth’s surface associated with radiation factors in response to reduction of its albedo by 0.1. A shift...

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Main Authors: I. A. Korneva, S. M. Semenov
Format: Article
Language:Russian
Published: Nauka 2015-07-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/179
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author I. A. Korneva
S. M. Semenov
author_facet I. A. Korneva
S. M. Semenov
author_sort I. A. Korneva
collection DOAJ
description Calculations with one-layer radiative model of the atmosphere based upon the data of Surface Radiation Budget archive over 1984–2007 allowed to assess changes in temperature distribution over the earth’s surface associated with radiation factors in response to reduction of its albedo by 0.1. A shift in the zero isotherm, a proxy for the cryosphere boundary on the earth’s surface, was found moderate on the global scale, although some regional consequences are substantial. For example, ice systems of Western Himalayas, Tibet, Pamir and Kamchatka will degrade. However, shifts in the arctic ice boundary will be moderate assuming all non-radiative heat fluxes remain unchanged.
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spelling doaj.art-bf858c930cb143a7be83c3dba82dc4c12025-03-02T12:52:24ZrusNaukaЛëд и снег2076-67342412-37652015-07-0155351310.15356/2076-6734-2015-3-5-13172Assessment of surface albedo effect on the position of zero isothermI. A. Korneva0S. M. Semenov1Institute of Global Climate and Ecology of Roshydromet and RAS, MoscowInstitute of Global Climate and Ecology of Roshydromet and RAS, Moscow Institute of Geography, Russian Academy of Sciences, MoscowCalculations with one-layer radiative model of the atmosphere based upon the data of Surface Radiation Budget archive over 1984–2007 allowed to assess changes in temperature distribution over the earth’s surface associated with radiation factors in response to reduction of its albedo by 0.1. A shift in the zero isotherm, a proxy for the cryosphere boundary on the earth’s surface, was found moderate on the global scale, although some regional consequences are substantial. For example, ice systems of Western Himalayas, Tibet, Pamir and Kamchatka will degrade. However, shifts in the arctic ice boundary will be moderate assuming all non-radiative heat fluxes remain unchanged.https://ice-snow.igras.ru/jour/article/view/179albedocryosphereearth surfacetemperature distributionzero isotherm
spellingShingle I. A. Korneva
S. M. Semenov
Assessment of surface albedo effect on the position of zero isotherm
Лëд и снег
albedo
cryosphere
earth surface
temperature distribution
zero isotherm
title Assessment of surface albedo effect on the position of zero isotherm
title_full Assessment of surface albedo effect on the position of zero isotherm
title_fullStr Assessment of surface albedo effect on the position of zero isotherm
title_full_unstemmed Assessment of surface albedo effect on the position of zero isotherm
title_short Assessment of surface albedo effect on the position of zero isotherm
title_sort assessment of surface albedo effect on the position of zero isotherm
topic albedo
cryosphere
earth surface
temperature distribution
zero isotherm
url https://ice-snow.igras.ru/jour/article/view/179
work_keys_str_mv AT iakorneva assessmentofsurfacealbedoeffectonthepositionofzeroisotherm
AT smsemenov assessmentofsurfacealbedoeffectonthepositionofzeroisotherm