Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ...
Over annual to decadal timescales changes in the storm track influences regional climate in Europe, however little is known about how the storm track varies over centennial and millennial timescales. We here present two datasets. The first is a reconstruction of storminess from northwest Spain spann...
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ftdatacite:10.1594/pangaea.931005 2024-09-09T19:57:17+00:00 Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ... Orme, Lisa C Charman, Dan J Reinhardt, Liam Jones, Richard T Mitchell, Fraser J G Stefanini, B S Barkwith, Andrew Ellis, Michael A Grosvenor, Mark 2021 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.931005 https://doi.pangaea.de/10.1594/PANGAEA.931005 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.931007 https://dx.doi.org/10.1130/g38521.1 https://dx.doi.org/10.1023/a:1008119611481 https://dx.doi.org/10.1016/j.quascirev.2015.10.045 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Europe Holocene North Atlantic Oscillation storminess storm track DEPTH, sediment/rock AGE Ignition residue Density, organic matter Size fraction 0.18-0.12 mm Size fraction > 0.180 mm Peat corer After Heiri et al., 2001 Grain size, sieving dataset Dataset 2021 ftdatacite https://doi.org/10.1594/pangaea.93100510.1594/pangaea.93100710.1130/g38521.110.1023/a:100811961148110.1016/j.quascirev.2015.10.045 2024-08-01T10:50:55Z Over annual to decadal timescales changes in the storm track influences regional climate in Europe, however little is known about how the storm track varies over centennial and millennial timescales. We here present two datasets. The first is a reconstruction of storminess from northwest Spain spanning the period 4600-0 cal yrs BP, which was developed by measuring aeolian sand deposits in a peat core from Pedrido Bog, Galicia, Spain. Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and >180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as proxies for storminess. The second dataset is a North-South storm track index reconstruction for western Europe spanning the period 3940-120 cal yrs BP. To create the storm track index, the above described ... Dataset North Atlantic North Atlantic oscillation DataCite |
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Open Polar |
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DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Europe Holocene North Atlantic Oscillation storminess storm track DEPTH, sediment/rock AGE Ignition residue Density, organic matter Size fraction 0.18-0.12 mm Size fraction > 0.180 mm Peat corer After Heiri et al., 2001 Grain size, sieving |
spellingShingle |
Europe Holocene North Atlantic Oscillation storminess storm track DEPTH, sediment/rock AGE Ignition residue Density, organic matter Size fraction 0.18-0.12 mm Size fraction > 0.180 mm Peat corer After Heiri et al., 2001 Grain size, sieving Orme, Lisa C Charman, Dan J Reinhardt, Liam Jones, Richard T Mitchell, Fraser J G Stefanini, B S Barkwith, Andrew Ellis, Michael A Grosvenor, Mark Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ... |
topic_facet |
Europe Holocene North Atlantic Oscillation storminess storm track DEPTH, sediment/rock AGE Ignition residue Density, organic matter Size fraction 0.18-0.12 mm Size fraction > 0.180 mm Peat corer After Heiri et al., 2001 Grain size, sieving |
description |
Over annual to decadal timescales changes in the storm track influences regional climate in Europe, however little is known about how the storm track varies over centennial and millennial timescales. We here present two datasets. The first is a reconstruction of storminess from northwest Spain spanning the period 4600-0 cal yrs BP, which was developed by measuring aeolian sand deposits in a peat core from Pedrido Bog, Galicia, Spain. Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and >180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as proxies for storminess. The second dataset is a North-South storm track index reconstruction for western Europe spanning the period 3940-120 cal yrs BP. To create the storm track index, the above described ... |
format |
Dataset |
author |
Orme, Lisa C Charman, Dan J Reinhardt, Liam Jones, Richard T Mitchell, Fraser J G Stefanini, B S Barkwith, Andrew Ellis, Michael A Grosvenor, Mark |
author_facet |
Orme, Lisa C Charman, Dan J Reinhardt, Liam Jones, Richard T Mitchell, Fraser J G Stefanini, B S Barkwith, Andrew Ellis, Michael A Grosvenor, Mark |
author_sort |
Orme, Lisa C |
title |
Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ... |
title_short |
Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ... |
title_full |
Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ... |
title_fullStr |
Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ... |
title_full_unstemmed |
Sand-based storminess proxies from Pedrido Bog, Galicia, Spain ... |
title_sort |
sand-based storminess proxies from pedrido bog, galicia, spain ... |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://dx.doi.org/10.1594/pangaea.931005 https://doi.pangaea.de/10.1594/PANGAEA.931005 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
https://dx.doi.org/10.1594/pangaea.931007 https://dx.doi.org/10.1130/g38521.1 https://dx.doi.org/10.1023/a:1008119611481 https://dx.doi.org/10.1016/j.quascirev.2015.10.045 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.93100510.1594/pangaea.93100710.1130/g38521.110.1023/a:100811961148110.1016/j.quascirev.2015.10.045 |
_version_ |
1809928182339469312 |