Article

 

Changes in wind-driven upwelling during the last three centuries: Interocean teleconnections Public Deposited

Downloadable Content

Download PDF
https://ir.library.oregonstate.edu/concern/articles/qz20sv000

Descriptions

Attribute NameValues
Creator
Abstract
  • Analysis of sediments from two wind-driven upwelling systems, Guaymas and Cariaco basins, using the alkenonebased U_37^(K^' ) paleothermometer yielded high-resolution records of sea surface temperatures (SST) from 1700 to 2000 AD. The trends in the U K'/37 index reveal steady SST increases of 1 to 2°C at both sites since the end of the Little Ice Age. Higher-frequency changes in SST indicate a decoupling in the relative intensity of wind-driven upwelling at the two sites. Periods of enhanced upwelling in Guaymas correspond to periods of decreased upwelling in Cariaco (and vice versa). We propose that these contrasts reflect regional differences in the upwelling response of upwelling to changes in the positioning of the Inter-Tropical Convergence Zone (ITCZ) and the Subtropical High (SH) under current climate conditions.
Resource Type
DOI
Date Available
Date Issued
Citation
  • Goñi, M. A., R. C. Thunell, M. P. Woodwort, and F. E. Müller-Karger (2006), Changes in wind-driven upwelling during the last three centuries: Interocean teleconnections, Geophys. Res. Lett., 33, L15604, doi:10.1029/2006GL026415.
Journal Title
Journal Volume
  • 33
Rights Statement
Funding Statement (additional comments about funding)
  • Funding of this work was provided by NSF grants OCE-0540793, OCE-0315234, OCE-0326313 and OCE-0118349.
Publisher
Language
Replaces
ISSN
  • 0094-8276

Relationships

Parents:

This work has no parents.

Items