Summer temperature gradients in northwest Europe during the Lateglacial to early Holocene transition (15-8 ka BP) inferred from chironomid assemblages

The raster temperature data was interpolated from site temperature data estimated from Chironomid records using Kriging. Temperatures are in Degrees Centigrage. The dataset covers all of Northern Europe including Iceland and Scandanavia.

Bibliographic Details
Main Authors: Langdon, Peter, Riddy, Liam, Brooks, Stephen J.
Format: Text
Language:English
Published: University of Southampton 2014
Subjects:
Online Access:https://eprints.soton.ac.uk/361991/
https://eprints.soton.ac.uk/361991/1/Instructions.pdf
https://eprints.soton.ac.uk/361991/2/GIS_symbology.lyr
https://eprints.soton.ac.uk/361991/3/Holocene_final_data.zip
https://eprints.soton.ac.uk/361991/4/Holocene_metadata.zip
https://eprints.soton.ac.uk/361991/5/Lateglacial_metadata.zip
https://eprints.soton.ac.uk/361991/6/Lateglacial_final_data.zip
Description
Summary:The raster temperature data was interpolated from site temperature data estimated from Chironomid records using Kriging. Temperatures are in Degrees Centigrage. The dataset covers all of Northern Europe including Iceland and Scandanavia.