2005: High resolution regional climate simulations over Iceland using Polar MM5
High-resolution regional climate simulations of Iceland for 1991–2000 have been performed using the fifth-generation Pennsylvania State University–National Center for Atmospheric Research (PSU–NCAR) Mesocale Model (MM5) modified for use in polar regions (Polar MM5) with three nested domains and shor...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.668.1103 2023-05-15T16:44:15+02:00 2005: High resolution regional climate simulations over Iceland using Polar MM5 David H. Bromwich Lesheng Bai The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.668.1103 http://polarmet.osu.edu/PMG_publications/bromwich_bai_mwr_2005.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.668.1103 http://polarmet.osu.edu/PMG_publications/bromwich_bai_mwr_2005.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://polarmet.osu.edu/PMG_publications/bromwich_bai_mwr_2005.pdf text ftciteseerx 2016-01-08T17:11:30Z High-resolution regional climate simulations of Iceland for 1991–2000 have been performed using the fifth-generation Pennsylvania State University–National Center for Atmospheric Research (PSU–NCAR) Mesocale Model (MM5) modified for use in polar regions (Polar MM5) with three nested domains and short-duration integrations. The simulated results are compared with monthly mean surface observations from Iceland for 1991–2000 to demonstrate the high level of model performance; correlation coefficients exceed 0.9 for most variables considered. The simulation results are used to analyze the near-surface climate over Iceland. The simulated near-surface winds in winter are primarily katabatic. The land–sea-breeze circulation is clearly evident in sum-mer. The land is colder than the ocean during winter, with a strong (weak) temperature gradient along the southern (northern) coast. This temperature pattern over the sloping terrain forces the katabatic wind. The diurnal cycle of near-surface air temperature is marked in summer over the land areas, which drives the land–sea breeze. The near-surface climate variations for extremes of the North Atlantic Oscillation (NAO) index during winter and summer result from the large-scale atmospheric advection conditions. The time-averaged mesoscale precipitation distribution over Iceland is reasonably well simulated by Text Iceland North Atlantic North Atlantic oscillation Unknown |
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Open Polar |
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ftciteseerx |
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English |
description |
High-resolution regional climate simulations of Iceland for 1991–2000 have been performed using the fifth-generation Pennsylvania State University–National Center for Atmospheric Research (PSU–NCAR) Mesocale Model (MM5) modified for use in polar regions (Polar MM5) with three nested domains and short-duration integrations. The simulated results are compared with monthly mean surface observations from Iceland for 1991–2000 to demonstrate the high level of model performance; correlation coefficients exceed 0.9 for most variables considered. The simulation results are used to analyze the near-surface climate over Iceland. The simulated near-surface winds in winter are primarily katabatic. The land–sea-breeze circulation is clearly evident in sum-mer. The land is colder than the ocean during winter, with a strong (weak) temperature gradient along the southern (northern) coast. This temperature pattern over the sloping terrain forces the katabatic wind. The diurnal cycle of near-surface air temperature is marked in summer over the land areas, which drives the land–sea breeze. The near-surface climate variations for extremes of the North Atlantic Oscillation (NAO) index during winter and summer result from the large-scale atmospheric advection conditions. The time-averaged mesoscale precipitation distribution over Iceland is reasonably well simulated by |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
David H. Bromwich Lesheng Bai |
spellingShingle |
David H. Bromwich Lesheng Bai 2005: High resolution regional climate simulations over Iceland using Polar MM5 |
author_facet |
David H. Bromwich Lesheng Bai |
author_sort |
David H. Bromwich |
title |
2005: High resolution regional climate simulations over Iceland using Polar MM5 |
title_short |
2005: High resolution regional climate simulations over Iceland using Polar MM5 |
title_full |
2005: High resolution regional climate simulations over Iceland using Polar MM5 |
title_fullStr |
2005: High resolution regional climate simulations over Iceland using Polar MM5 |
title_full_unstemmed |
2005: High resolution regional climate simulations over Iceland using Polar MM5 |
title_sort |
2005: high resolution regional climate simulations over iceland using polar mm5 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.668.1103 http://polarmet.osu.edu/PMG_publications/bromwich_bai_mwr_2005.pdf |
genre |
Iceland North Atlantic North Atlantic oscillation |
genre_facet |
Iceland North Atlantic North Atlantic oscillation |
op_source |
http://polarmet.osu.edu/PMG_publications/bromwich_bai_mwr_2005.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.668.1103 http://polarmet.osu.edu/PMG_publications/bromwich_bai_mwr_2005.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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