OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE
Abstract: Conditions for wet snow icing are estimated in terms of mean daily values of temperature, precipitation and wind speed. On the basis of this estimation, calculations are made of the change in frequency of events of wet snow icing in simulations of future climate. In coastal areas of Icelan...
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Format: | Text |
Language: | English |
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Croatian meteorological society; info@meteohmd.hr
2005
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Online Access: | http://hrcak.srce.hr/64952 http://hrcak.srce.hr/file/97267 |
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author | Rögnvaldsson, Ólafur; University of Bergen, Norway, Institute for Meteorological Research, Iceland and Icelandic Meteorological Office; or@os.is Ólafsson, Haraldur; University of Iceland, Icelandic Meteorological Office and Institute for Meteorological Research |
author_facet | Rögnvaldsson, Ólafur; University of Bergen, Norway, Institute for Meteorological Research, Iceland and Icelandic Meteorological Office; or@os.is Ólafsson, Haraldur; University of Iceland, Icelandic Meteorological Office and Institute for Meteorological Research |
author_sort | Rögnvaldsson, Ólafur; University of Bergen, Norway, Institute for Meteorological Research, Iceland and Icelandic Meteorological Office; or@os.is |
collection | Hrčak - Portal of scientific journals of Croatia |
description | Abstract: Conditions for wet snow icing are estimated in terms of mean daily values of temperature, precipitation and wind speed. On the basis of this estimation, calculations are made of the change in frequency of events of wet snow icing in simulations of future climate. In coastal areas of Iceland, a large reduction in the number of wet snow icing events is predicted for the period 2071-2100, but at an elevation of 400-700 m.a.s.l., there is a different result: in Southwest-Iceland, there is only a moderate decrease in the number of events, while in Northeast-Iceland, there is a large increase in the frequency of wet snow icing events. The decrease of the number of wet snow icing events is associated with fewer days with temperatures close to 0°C, while in the case of an increase in precipitation, the impact of the temperature increase is overrun by an increase in frequency of heavy precipitation in the mountains. |
format | Text |
genre | Iceland |
genre_facet | Iceland |
id | fthrcak:oai:hrcak.srce.hr:64952 |
institution | Open Polar |
language | English |
op_collection_id | fthrcak |
op_relation | http://hrcak.srce.hr/64952 http://hrcak.srce.hr/file/97267 |
op_rights | The papers of this Journal are free of charge for personal or educational use, with respect of copyright of authors and publisher. |
op_source | Croatian meteorological journal (nikolic@cirus.dhz.hr); Vol.40 No.40 |
publishDate | 2005 |
publisher | Croatian meteorological society; info@meteohmd.hr |
record_format | openpolar |
spelling | fthrcak:oai:hrcak.srce.hr:64952 2025-01-16T22:31:20+00:00 OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE Rögnvaldsson, Ólafur; University of Bergen, Norway, Institute for Meteorological Research, Iceland and Icelandic Meteorological Office; or@os.is Ólafsson, Haraldur; University of Iceland, Icelandic Meteorological Office and Institute for Meteorological Research 2005-12-15 pdf http://hrcak.srce.hr/64952 http://hrcak.srce.hr/file/97267 en eng Croatian meteorological society; info@meteohmd.hr http://hrcak.srce.hr/64952 http://hrcak.srce.hr/file/97267 The papers of this Journal are free of charge for personal or educational use, with respect of copyright of authors and publisher. Croatian meteorological journal (nikolic@cirus.dhz.hr); Vol.40 No.40 Wet snow icing;Iceland;future climate;dynamic downscaling text 2005 fthrcak 2012-10-27T15:59:49Z Abstract: Conditions for wet snow icing are estimated in terms of mean daily values of temperature, precipitation and wind speed. On the basis of this estimation, calculations are made of the change in frequency of events of wet snow icing in simulations of future climate. In coastal areas of Iceland, a large reduction in the number of wet snow icing events is predicted for the period 2071-2100, but at an elevation of 400-700 m.a.s.l., there is a different result: in Southwest-Iceland, there is only a moderate decrease in the number of events, while in Northeast-Iceland, there is a large increase in the frequency of wet snow icing events. The decrease of the number of wet snow icing events is associated with fewer days with temperatures close to 0°C, while in the case of an increase in precipitation, the impact of the temperature increase is overrun by an increase in frequency of heavy precipitation in the mountains. Text Iceland Hrčak - Portal of scientific journals of Croatia |
spellingShingle | Wet snow icing;Iceland;future climate;dynamic downscaling Rögnvaldsson, Ólafur; University of Bergen, Norway, Institute for Meteorological Research, Iceland and Icelandic Meteorological Office; or@os.is Ólafsson, Haraldur; University of Iceland, Icelandic Meteorological Office and Institute for Meteorological Research OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE |
title | OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE |
title_full | OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE |
title_fullStr | OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE |
title_full_unstemmed | OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE |
title_short | OROGRAPHIC IMPACT ON THE PREDICTED CHANGE IN THE FREQUENCY OF CONDITIONS FOR WET SNOW ICING IN FUTURE CLIMATE |
title_sort | orographic impact on the predicted change in the frequency of conditions for wet snow icing in future climate |
topic | Wet snow icing;Iceland;future climate;dynamic downscaling |
topic_facet | Wet snow icing;Iceland;future climate;dynamic downscaling |
url | http://hrcak.srce.hr/64952 http://hrcak.srce.hr/file/97267 |