Skip to main content
Book Chapter

High frequency variations of water flux and sediment discharge during the Little Ice Age (1586–1725 AD) in the Rhône Delta (Mediterranean France). Relationship to the catchment basin

  • Arnaud-Fassetta G
  • Provansal M
Springer Netherlands, (1999), 241-250
DOI: 10.1007/978-94-017-2163-9_25
N/ACitations
Citations of this article
1Readers
Mendeley users who have this article in their library.
Get full text

Abstract

During the 17th and 18th centuries, the Rhône delta recorded high frequency fluctuations in water and sediment influx. These variations resulted from the drastic climatic changes that took place during the Little Ice Age, which were intensified by dense land...

Cite

CITATION STYLE

APA

Arnaud-Fassetta, G., & Provansal, M. (1999). High frequency variations of water flux and sediment discharge during the Little Ice Age (1586–1725 AD) in the Rhône Delta (Mediterranean France). Relationship to the catchment basin. In Man and River Systems (pp. 241–250). Springer Netherlands. https://doi.org/10.1007/978-94-017-2163-9_25

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free