Autumn snowfall and hydroclimatic variability during the past millennium inferred from the varved sediments of meromictic Lake A, northern Ellesmere Island, Canada

Abstract We examined the hydroclimatic signal in a record of annual lamina (varve) thickness from High Arctic Lake A, Ellesmere Island (83°00.00′N, 75°30.00′W). In this unglacierized catchment, nival melt is the dominant source for meltwater and transport of sediment to the lake, and autumn snowfall...

Full description

Bibliographic Details
Published in:Quaternary Research
Main Authors: Tomkins, Jessica D., Lamoureux, Scott F., Antoniades, Dermot, Vincent, Warwick F.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2010
Subjects:
Online Access:http://dx.doi.org/10.1016/j.yqres.2010.06.005
http://api.elsevier.com/content/article/PII:S0033589410000645?httpAccept=text/xml
http://api.elsevier.com/content/article/PII:S0033589410000645?httpAccept=text/plain
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400036322