Quantification of the cold air pool in Kevo valley, Finnish Lapland

The ponding of cold air at low elevations is a major feature of the high-latitude climates of the Arctic, wherever low solar angles combine with incised topography. In Finnish Lapland this cold-air accumulation is critical for flora and fauna (Tenow and Nilssen, 1990; Virtanen et al., 1998) since ab...

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Published in:Weather
Main Authors: Pepin, Nick, Schaefer, Martin, Riddy, Liam
Format: Article in Journal/Newspaper
Language:unknown
Published: 2009
Subjects:
Online Access:https://eprints.soton.ac.uk/348729/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:348729 2023-07-30T04:02:04+02:00 Quantification of the cold air pool in Kevo valley, Finnish Lapland Pepin, Nick Schaefer, Martin Riddy, Liam 2009-03 https://eprints.soton.ac.uk/348729/ unknown Pepin, Nick, Schaefer, Martin and Riddy, Liam (2009) Quantification of the cold air pool in Kevo valley, Finnish Lapland. Weather, 64 (3), 60-67. (doi:10.1002/wea.260 <http://dx.doi.org/10.1002/wea.260>). Article PeerReviewed 2009 ftsouthampton https://doi.org/10.1002/wea.260 2023-07-09T21:44:26Z The ponding of cold air at low elevations is a major feature of the high-latitude climates of the Arctic, wherever low solar angles combine with incised topography. In Finnish Lapland this cold-air accumulation is critical for flora and fauna (Tenow and Nilssen, 1990; Virtanen et al., 1998) since absolute minimum temperatures control the survival of the eggs of the autumnal moth Epirrita autumnata. This moth is responsible for outbreaks of defoliation of the mountain birch Betula pubescens. Without cold-air accumulation there would be far more destructive outbreaks in the main inhabited areas. Added to the above concern is that of global warming. Warming is expected to be greater than the global average in the high latitudes (IPCC, 2007) and the temperature rise in winter in Finland over the twenty-first century is expected to be particularly large (Jylhä et al., 2004). Current predictions made by the Intergovernmental Panel on Climate Change (IPCC) (2007) indicate a best estimate annual warming of around +5 degC for northern Finland by 2099 (~+7 degC in winter), as opposed to +3.2 degC for Europe as a whole (A1B scenario). If the enhancement of greenhouse gases in the atmosphere also alters the propensity for cold-pool formation, local increases in winter temperatures could be even more dramatic than the regional mean, with large consequences for forest damage, local ecology, and the formation/destruction of lake ice in autumn and spring. The cold pool is transient and its formation and destruction are controlled by synoptic conditions (atmospheric gradient winds and cloud cover/radiation balance) as well as the interaction with local topography. The research summarized in this paper comes from a pilot study which aimed to quantify the existence, temporal and spatial extent of the cold pool in Kevo Valley, northern Finland, through operation of an elevationaltransect of automatic temperature loggers.Future research is mapping the spatial extent of this cold pool in more detail, and examining the mechanisms ... Article in Journal/Newspaper Arctic Climate change Global warming Northern Finland Lapland University of Southampton: e-Prints Soton Arctic Kevo ENVELOPE(27.020,27.020,69.758,69.758) Weather 64 3 60 67
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language unknown
description The ponding of cold air at low elevations is a major feature of the high-latitude climates of the Arctic, wherever low solar angles combine with incised topography. In Finnish Lapland this cold-air accumulation is critical for flora and fauna (Tenow and Nilssen, 1990; Virtanen et al., 1998) since absolute minimum temperatures control the survival of the eggs of the autumnal moth Epirrita autumnata. This moth is responsible for outbreaks of defoliation of the mountain birch Betula pubescens. Without cold-air accumulation there would be far more destructive outbreaks in the main inhabited areas. Added to the above concern is that of global warming. Warming is expected to be greater than the global average in the high latitudes (IPCC, 2007) and the temperature rise in winter in Finland over the twenty-first century is expected to be particularly large (Jylhä et al., 2004). Current predictions made by the Intergovernmental Panel on Climate Change (IPCC) (2007) indicate a best estimate annual warming of around +5 degC for northern Finland by 2099 (~+7 degC in winter), as opposed to +3.2 degC for Europe as a whole (A1B scenario). If the enhancement of greenhouse gases in the atmosphere also alters the propensity for cold-pool formation, local increases in winter temperatures could be even more dramatic than the regional mean, with large consequences for forest damage, local ecology, and the formation/destruction of lake ice in autumn and spring. The cold pool is transient and its formation and destruction are controlled by synoptic conditions (atmospheric gradient winds and cloud cover/radiation balance) as well as the interaction with local topography. The research summarized in this paper comes from a pilot study which aimed to quantify the existence, temporal and spatial extent of the cold pool in Kevo Valley, northern Finland, through operation of an elevationaltransect of automatic temperature loggers.Future research is mapping the spatial extent of this cold pool in more detail, and examining the mechanisms ...
format Article in Journal/Newspaper
author Pepin, Nick
Schaefer, Martin
Riddy, Liam
spellingShingle Pepin, Nick
Schaefer, Martin
Riddy, Liam
Quantification of the cold air pool in Kevo valley, Finnish Lapland
author_facet Pepin, Nick
Schaefer, Martin
Riddy, Liam
author_sort Pepin, Nick
title Quantification of the cold air pool in Kevo valley, Finnish Lapland
title_short Quantification of the cold air pool in Kevo valley, Finnish Lapland
title_full Quantification of the cold air pool in Kevo valley, Finnish Lapland
title_fullStr Quantification of the cold air pool in Kevo valley, Finnish Lapland
title_full_unstemmed Quantification of the cold air pool in Kevo valley, Finnish Lapland
title_sort quantification of the cold air pool in kevo valley, finnish lapland
publishDate 2009
url https://eprints.soton.ac.uk/348729/
long_lat ENVELOPE(27.020,27.020,69.758,69.758)
geographic Arctic
Kevo
geographic_facet Arctic
Kevo
genre Arctic
Climate change
Global warming
Northern Finland
Lapland
genre_facet Arctic
Climate change
Global warming
Northern Finland
Lapland
op_relation Pepin, Nick, Schaefer, Martin and Riddy, Liam (2009) Quantification of the cold air pool in Kevo valley, Finnish Lapland. Weather, 64 (3), 60-67. (doi:10.1002/wea.260 <http://dx.doi.org/10.1002/wea.260>).
op_doi https://doi.org/10.1002/wea.260
container_title Weather
container_volume 64
container_issue 3
container_start_page 60
op_container_end_page 67
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