How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland?

Abstract A detailed analysis of 2 years' hourly microclimatic (mainly surface air temperature) data recently acquired from locations widely dispersed over 700 km 2 in the Abisko catchment encompassing Lake Torneträsk in Swedish Lapland is presented in this study. This project is designed to exp...

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Published in:Meteorological Applications
Main Authors: Yang, Zhenlin, Hanna, Edward, Callaghan, Terry V., Jonasson, Christer
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2011
Subjects:
Online Access:http://dx.doi.org/10.1002/met.276
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spelling crwiley:10.1002/met.276 2024-09-15T17:34:22+00:00 How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland? Yang, Zhenlin Hanna, Edward Callaghan, Terry V. Jonasson, Christer 2011 http://dx.doi.org/10.1002/met.276 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fmet.276 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.276 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Meteorological Applications volume 19, issue 4, page 454-463 ISSN 1350-4827 1469-8080 journal-article 2011 crwiley https://doi.org/10.1002/met.276 2024-07-23T04:14:00Z Abstract A detailed analysis of 2 years' hourly microclimatic (mainly surface air temperature) data recently acquired from locations widely dispersed over 700 km 2 in the Abisko catchment encompassing Lake Torneträsk in Swedish Lapland is presented in this study. This project is designed to explore the effects of microclimatic variability, past and future climate change (1913–2100) on regional vegetation and land‐use changes, at an unique Arctic ecological and climate monitoring site, to aid adaptation of stakeholders to future climate change. Dominant altitudinal lapse rate and radiation effects during summer are revealed in detailed analysis of spatial variations in temperature between the different sites, which become largely negated during winter when cold‐air ponding is much more significant. Moreover, near‐shore temperatures are moderated significantly by Lake Torneträsk during the spring lake‐ice melt season. The extent to which synoptic meteorological conditions affect these factors is explored. Examples of gridded temperature maps for the Abisko region are also presented, produced using a downscaling model based on the temperature data, which have numerous ecological and other applications. The long‐term Abisko Scientific Research Station meteorological record, which spans almost a century from 1913 to present is also explored, for evidence of climate change, to set the temperature logger data in a long‐term climate context. Exploratory analysis of the possible influence of future regional climate change on ecological/vegetation zones is also briefly discussed. Copyright © 2011 Royal Meteorological Society Article in Journal/Newspaper Abisko Climate change Lapland Wiley Online Library Meteorological Applications 19 4 454 463
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract A detailed analysis of 2 years' hourly microclimatic (mainly surface air temperature) data recently acquired from locations widely dispersed over 700 km 2 in the Abisko catchment encompassing Lake Torneträsk in Swedish Lapland is presented in this study. This project is designed to explore the effects of microclimatic variability, past and future climate change (1913–2100) on regional vegetation and land‐use changes, at an unique Arctic ecological and climate monitoring site, to aid adaptation of stakeholders to future climate change. Dominant altitudinal lapse rate and radiation effects during summer are revealed in detailed analysis of spatial variations in temperature between the different sites, which become largely negated during winter when cold‐air ponding is much more significant. Moreover, near‐shore temperatures are moderated significantly by Lake Torneträsk during the spring lake‐ice melt season. The extent to which synoptic meteorological conditions affect these factors is explored. Examples of gridded temperature maps for the Abisko region are also presented, produced using a downscaling model based on the temperature data, which have numerous ecological and other applications. The long‐term Abisko Scientific Research Station meteorological record, which spans almost a century from 1913 to present is also explored, for evidence of climate change, to set the temperature logger data in a long‐term climate context. Exploratory analysis of the possible influence of future regional climate change on ecological/vegetation zones is also briefly discussed. Copyright © 2011 Royal Meteorological Society
format Article in Journal/Newspaper
author Yang, Zhenlin
Hanna, Edward
Callaghan, Terry V.
Jonasson, Christer
spellingShingle Yang, Zhenlin
Hanna, Edward
Callaghan, Terry V.
Jonasson, Christer
How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland?
author_facet Yang, Zhenlin
Hanna, Edward
Callaghan, Terry V.
Jonasson, Christer
author_sort Yang, Zhenlin
title How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland?
title_short How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland?
title_full How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland?
title_fullStr How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland?
title_full_unstemmed How can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around Abisko, Swedish Lapland?
title_sort how can meteorological observations and microclimate simulations improve understanding of 1913–2010 climate change around abisko, swedish lapland?
publisher Wiley
publishDate 2011
url http://dx.doi.org/10.1002/met.276
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fmet.276
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.276
genre Abisko
Climate change
Lapland
genre_facet Abisko
Climate change
Lapland
op_source Meteorological Applications
volume 19, issue 4, page 454-463
ISSN 1350-4827 1469-8080
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/met.276
container_title Meteorological Applications
container_volume 19
container_issue 4
container_start_page 454
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