Reconstructing lake ice cover in subarctic lakes using a diatom-based inference model

A new quantitative diatom‐based lake ice cover inference model was developed to reconstruct past ice cover histories and applied to four subarctic lakes. The used ice cover model is based on a calculated melting degree day value of +130 and a freezing degree day value of −30 for each lake. The recon...

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Veröffentlicht in:Geophysical research letters 2014-03, Vol.41 (6), p.2026-2032
Hauptverfasser: Weckström, Jan, Hanhijärvi, Sami, Forsström, Laura, Kuusisto, Esko, Korhola, Atte
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container_end_page 2032
container_issue 6
container_start_page 2026
container_title Geophysical research letters
container_volume 41
creator Weckström, Jan
Hanhijärvi, Sami
Forsström, Laura
Kuusisto, Esko
Korhola, Atte
description A new quantitative diatom‐based lake ice cover inference model was developed to reconstruct past ice cover histories and applied to four subarctic lakes. The used ice cover model is based on a calculated melting degree day value of +130 and a freezing degree day value of −30 for each lake. The reconstructed Holocene ice cover duration histories show similar trends to the independently reconstructed regional air temperature history. The ice cover duration was around 7 days shorter than the average ice cover duration during the warmer early Holocene (approximately 10 to 6.5 calibrated kyr B.P.) and around 3–5 days longer during the cool Little Ice Age (approximately 500 to 100 calibrated yr B.P.). Although the recent climate warming is represented by only 2–3 samples in the sediment series, these show a rising trend in the prolonged ice‐free periods of up to 2 days. Diatom‐based ice cover inference models can provide a powerful tool to reconstruct past ice cover histories in remote and sensitive areas where no measured data are available. Key Points A quantitative diatom‐based ice‐cover model has been created Inferred past ice‐cover trends are similar to the regional climate history Diatoms can provide a valuable tool to reconstruct past ice‐cover regimes
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The used ice cover model is based on a calculated melting degree day value of +130 and a freezing degree day value of −30 for each lake. The reconstructed Holocene ice cover duration histories show similar trends to the independently reconstructed regional air temperature history. The ice cover duration was around 7 days shorter than the average ice cover duration during the warmer early Holocene (approximately 10 to 6.5 calibrated kyr B.P.) and around 3–5 days longer during the cool Little Ice Age (approximately 500 to 100 calibrated yr B.P.). Although the recent climate warming is represented by only 2–3 samples in the sediment series, these show a rising trend in the prolonged ice‐free periods of up to 2 days. Diatom‐based ice cover inference models can provide a powerful tool to reconstruct past ice cover histories in remote and sensitive areas where no measured data are available. Key Points A quantitative diatom‐based ice‐cover model has been created Inferred past ice‐cover trends are similar to the regional climate history Diatoms can provide a valuable tool to reconstruct past ice‐cover regimes</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1002/2014GL059474</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Air temperature ; Bacillariophyceae ; Climate ; Climate change ; diatoms ; Freezing ; Freshwater ; Global warming ; Holocene ; Ice ; Ice ages ; Ice cover ; Ice-free periods ; Inference ; Lake ice ; Lakes ; paleoclimate ; Plankton ; quantitative reconstruction ; Regional ; subarctic lakes ; Trends</subject><ispartof>Geophysical research letters, 2014-03, Vol.41 (6), p.2026-2032</ispartof><rights>2014. American Geophysical Union. 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Res. Lett</addtitle><description>A new quantitative diatom‐based lake ice cover inference model was developed to reconstruct past ice cover histories and applied to four subarctic lakes. The used ice cover model is based on a calculated melting degree day value of +130 and a freezing degree day value of −30 for each lake. The reconstructed Holocene ice cover duration histories show similar trends to the independently reconstructed regional air temperature history. The ice cover duration was around 7 days shorter than the average ice cover duration during the warmer early Holocene (approximately 10 to 6.5 calibrated kyr B.P.) and around 3–5 days longer during the cool Little Ice Age (approximately 500 to 100 calibrated yr B.P.). Although the recent climate warming is represented by only 2–3 samples in the sediment series, these show a rising trend in the prolonged ice‐free periods of up to 2 days. 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subjects Air temperature
Bacillariophyceae
Climate
Climate change
diatoms
Freezing
Freshwater
Global warming
Holocene
Ice
Ice ages
Ice cover
Ice-free periods
Inference
Lake ice
Lakes
paleoclimate
Plankton
quantitative reconstruction
Regional
subarctic lakes
Trends
title Reconstructing lake ice cover in subarctic lakes using a diatom-based inference model
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