scispace - formally typeset
P

Paul J. Valdes

Researcher at University of Bristol

Publications -  384
Citations -  24048

Paul J. Valdes is an academic researcher from University of Bristol. The author has contributed to research in topics: Climate change & Climate model. The author has an hindex of 77, co-authored 344 publications receiving 20662 citations. Previous affiliations of Paul J. Valdes include University of Oxford & University of Reading.

Papers
More filters
Posted ContentDOI

Coupled simulations of the mid-Holocene and Last Glacial Maximum: new results from PMIP2

TL;DR: In this paper, a set of coupled ocean-atmosphere simulations using state of the art climate models is now available for the Last Glacial Maximum and the mid-Holocene through the second phase of the Paleoclimate Modeling Intercomparison Project (PMIP2).
Journal ArticleDOI

The Mechanisms that Determine the Response of the Northern Hemisphere's Stationary Waves to North American Ice Sheets

TL;DR: In this paper, changes in stationary waves caused by ice sheets over North America are examined, which describe the persistent meanders in the west-east flow of the extratropical atmosphere.
Journal ArticleDOI

Response of methane emissions from wetlands to the Last Glacial Maximum and an idealized Dansgaard-Oeschger climate event: insights from two models of different complexity

TL;DR: The role of different sources and sinks of CH4 in changes in atmospheric CH4 concentration during the last 100 000 yr is still not fully understood as discussed by the authors, and the uncertainties related to the parameterization of the wetland CH4 emission models relevant to these time periods by using two wetland models of different complexity (SDGVM and ORCHIDEE).
Journal ArticleDOI

Polar amplification of Pliocene climate by elevated trace gas radiative forcing

TL;DR: It is concluded that natural trace gas feedbacks are critical for interpreting climate warmth during the Pliocene and potentially many other warm phases of the Cenezoic.
Journal ArticleDOI

Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO(2)

TL;DR: In this article, the authors present a semi-continuous terrestrial temperature record spanning from the middle Eocene to the early Oligocene (~41-33 million years ago), using bacterial molecular fossils (biomarkers) preserved in a sequence of southeast Australian lignites.