A diatom-conductivity transfer function for reconstructing past changes in the Southern Hemisphere westerly winds over the Southern Ocean

Sub-Antarctic islands are ideally placed to reconstruct past changes in Southern Hemisphere westerly wind behaviour. They lie within their core belt (50–60°S) and the strong winds deliver sea salt ions to the islands resulting in a west to east conductivity gradient in their water bodies. This means...

Full description

Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Saunders, Krystyna M., Hodgson, Dominic A., McMurtrie, Shelley, Grosjean, Martin
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley 2015
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/510922/