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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| Language: | Russian |
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Nauka
2015-07-01
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| Series: | Lëd i Sneg |
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| Online Access: | https://ice-snow.igras.ru/jour/article/view/179 |
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doaj-bf858c930cb143a7be83c3dba82dc4c12021-08-02T08:42:08ZrusNaukaLëd i Sneg2076-67342412-37652015-07-0155351310.15356/2076-6734-2015-3-5-13172Assessment 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 |
| collection |
DOAJ |
| language |
Russian |
| format |
Article |
| sources |
DOAJ |
| author |
I. A. Korneva S. M. Semenov |
| spellingShingle |
I. A. Korneva S. M. Semenov Assessment of surface albedo effect on the position of zero isotherm Lëd i Sneg albedo cryosphere earth surface temperature distribution zero isotherm |
| author_facet |
I. A. Korneva S. M. Semenov |
| author_sort |
I. A. Korneva |
| title |
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_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_sort |
assessment of surface albedo effect on the position of zero isotherm |
| publisher |
Nauka |
| series |
Lëd i Sneg |
| issn |
2076-6734 2412-3765 |
| publishDate |
2015-07-01 |
| 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. |
| 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 |
| _version_ |
1721237832619524096 |