ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Publication Date: 2023-01-30
    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 storminess record from Spain was subtracted from a storminess record from Scotland, derived by averaging the results of two storminess reconstructions from the Outer Hebrides, Scotland (Orme et al., 2016). Each record was sampled to the same 20 year temporal resolution and standardised prior to this.
    Keywords: Europe; Holocene; North Atlantic Oscillation; storminess; storm track
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2023-02-07
    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 storminess record from Spain was subtracted from a storminess record from Scotland, derived by averaging the results of two storminess reconstructions from the Outer Hebrides, Scotland (Orme et al., 2016). Each record was sampled to the same 20 year temporal resolution and standardised prior to this.
    Keywords: After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Holocene; Ignition residue; North Atlantic Oscillation; PEATC; Peat corer; Pedrido_Bog; Size fraction 〉 0.180 mm; Size fraction 0.18-0.12 mm; Spain; storminess; storm track
    Type: Dataset
    Format: text/tab-separated-values, 968 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2023-02-08
    Description: Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this project two storminess reconstructions were developed from the Outer Hebrides, Scotland. Peat cores were sampled using a Russian corer from a peatbog Struban Bog (57°33'35''N; 7°20'45''W). 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 a proxies for storminess. Chronological constraints were provided by AMS radiocarbon dates; with 6 dates. The reconstruction from Struban Bog spans the period 4200-180 cal yrs BP.
    Keywords: After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Holocene; Ignition residue; North Atlantic Oscillation; Outer Hebrides, Scotland; PEATC; Peat corer; Size fraction 〉 0.180 mm; Size fraction 0.18-0.12 mm; storminess; STR; Struban_Bog
    Type: Dataset
    Format: text/tab-separated-values, 1132 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2023-02-07
    Description: To create the storm track index, the above described storminess record from Spain was subtracted from a storminess record from Scotland, derived by averaging the results of two storminess reconstructions from the Outer Hebrides, Scotland (Orme et al., 2016). Each record was sampled to the same 20 year temporal resolution and standardised prior to this.
    Keywords: DEPTH, sediment/rock; Europe; Hill_Top_Bog; Holocene; North Atlantic Oscillation; North-south storm track index; Outer Hebrides, Scotland; PEATC; Peat corer; Pedrido_Bog; Spain; storminess; storm track; STR; Struban_Bog
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2023-02-07
    Description: Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this project two storminess reconstructions were developed from the Outer Hebrides, Scotland. Peat cores were sampled using a Russian corer from a peatbog Hill Top Bog (57°10'5''N; 7°20'52W). 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 a proxies for storminess. Chronological constraints were provided by AMS radiocarbon dates; with 8 dates on the Hill Top Bog core. The reconstruction from Hill Top Bog spans the period 3940-0 cal yrs BP.
    Keywords: After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Hill_Top_Bog; Holocene; Ignition residue; North Atlantic Oscillation; Outer Hebrides, Scotland; PEATC; Peat corer; Size fraction 〉 0.180 mm; Size fraction 0.18-0.12 mm; storminess
    Type: Dataset
    Format: text/tab-separated-values, 1286 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...