Intense sea-effect snowfall case on the western coast of Finland

A new national daily snowfall record was measured in Finland on 8 January 2016 when it snowed 73 cm (31 mm as liquid water) in less than a day in Merikarvia on the western coast of Finland. The area of the most intense snowfall was very small, which is common in convective precipitation. In this...

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Main Authors: T. Olsson, T. Perttula, K. Jylhä, A. Luomaranta
Format: Article
Language:English
Published: Copernicus Publications 2017-07-01
Series:Advances in Science and Research
Online Access:https://www.adv-sci-res.net/14/231/2017/asr-14-231-2017.pdf
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spelling doaj-dc7d40679edd424490b110cd26454b442020-11-25T01:05:13ZengCopernicus PublicationsAdvances in Science and Research1992-06281992-06362017-07-011423123910.5194/asr-14-231-2017Intense sea-effect snowfall case on the western coast of FinlandT. Olsson0T. Perttula1K. Jylhä2A. Luomaranta3Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, FinlandFinnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, FinlandFinnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, FinlandFinnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, FinlandA new national daily snowfall record was measured in Finland on 8 January 2016 when it snowed 73 cm (31 mm as liquid water) in less than a day in Merikarvia on the western coast of Finland. The area of the most intense snowfall was very small, which is common in convective precipitation. In this work we used hourly weather radar images to identify the sea-effect snowfall case and to qualitatively estimate the performance of HARMONIE, a non-hydrostatic convection-permitting weather prediction model, in simulating the spatial and temporal evolution of the snowbands. The model simulation, including data assimilation, was run at 2.5 km horizontal resolution and 65 levels in vertical. HARMONIE was found to capture the overall sea-effect snowfall situation quite well, as both the timing and the location of the most intense snowstorm were properly simulated. Based on our preliminary analysis, the snowband case was triggered by atmospheric instability above the mostly ice-free sea and a low-level convergence zone almost perpendicular to the coastline. The simulated convective available potential energy (CAPE) reached a value of 87 J kg<sup>−1</sup> near the site of the observed snowfall record.https://www.adv-sci-res.net/14/231/2017/asr-14-231-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Olsson
T. Perttula
K. Jylhä
A. Luomaranta
spellingShingle T. Olsson
T. Perttula
K. Jylhä
A. Luomaranta
Intense sea-effect snowfall case on the western coast of Finland
Advances in Science and Research
author_facet T. Olsson
T. Perttula
K. Jylhä
A. Luomaranta
author_sort T. Olsson
title Intense sea-effect snowfall case on the western coast of Finland
title_short Intense sea-effect snowfall case on the western coast of Finland
title_full Intense sea-effect snowfall case on the western coast of Finland
title_fullStr Intense sea-effect snowfall case on the western coast of Finland
title_full_unstemmed Intense sea-effect snowfall case on the western coast of Finland
title_sort intense sea-effect snowfall case on the western coast of finland
publisher Copernicus Publications
series Advances in Science and Research
issn 1992-0628
1992-0636
publishDate 2017-07-01
description A new national daily snowfall record was measured in Finland on 8 January 2016 when it snowed 73 cm (31 mm as liquid water) in less than a day in Merikarvia on the western coast of Finland. The area of the most intense snowfall was very small, which is common in convective precipitation. In this work we used hourly weather radar images to identify the sea-effect snowfall case and to qualitatively estimate the performance of HARMONIE, a non-hydrostatic convection-permitting weather prediction model, in simulating the spatial and temporal evolution of the snowbands. The model simulation, including data assimilation, was run at 2.5 km horizontal resolution and 65 levels in vertical. HARMONIE was found to capture the overall sea-effect snowfall situation quite well, as both the timing and the location of the most intense snowstorm were properly simulated. Based on our preliminary analysis, the snowband case was triggered by atmospheric instability above the mostly ice-free sea and a low-level convergence zone almost perpendicular to the coastline. The simulated convective available potential energy (CAPE) reached a value of 87 J kg<sup>−1</sup> near the site of the observed snowfall record.
url https://www.adv-sci-res.net/14/231/2017/asr-14-231-2017.pdf
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