Peter U Clark

Biographic Data

ID3440667
NAMEPeter U Clark
GIVEN NAMESPeter U
FAMILY NAMEClark
SIGNATURECLARK P U
AFFILIATIONSOregon State University
ORCID0000-0003-4752-6045
VERIFIEDYes
TOTAL WORKS9
TOTAL CITATIONS33
AUTHOR COUNT9
EDITOR COUNT0
FIRST PUBLICATION YEAR1990
LATEST PUBLICATION YEAR2021
H-INDEX2

  • Migration towards Bangladesh coastlines projected to increase with sea-level rise through 2100

    Open AccessAndrew Reid Bell, David Wrathall et al.ARTICLEEnvironmental Research Letters2021

    To date, projections of human migration induced by sea-level change (SLC) largely suggest large-scale displacement away from vulnerable coastlines. However, results from our model of Bangladesh suggest counterintuitively that people will continue to migrate toward the vulnerable coastline irrespective of the flooding amplified by future SLC under all emissions scenarios until the end of this century. We developed an empirically calibrated agent-b…

  • A Reconstruction of Regional and Global Temperature for the Past 11,300 Years

    Open AccessShaun A Marcott, Jeremy D Shakun et al.ARTICLEScience2013

    Exceptional Now The climate has been warming since the industrial revolution, but how warm is climate now compared with the rest of the Holocene? Marcott et al. (p. 1198 ) constructed a record of global mean surface temperature for more than the last 11,000 years, using a variety of land- and marine-based proxy data from all around the world. The pattern of temperatures shows a rise as the world emerged from the last deglaciation, warm conditions…

  • The Last Glacial Maximum

    Open AccessPeter U Clark, Arthur S Dyke et al.ARTICLEScience2009

    The Melting Is in the Details Global sea level rises and falls as ice sheets and glaciers melt and grow, providing an integrated picture of the changes in ice volume but little information about how much individual ice fields are contributing to those variations. Knowing the regional structure of ice variability during glaciations and deglaciations will clarify the mechanisms of the glacial cycle. Clark et al. (p. 710 ) compiled and analyzed more…

  • A Speleothem Record of Younger Dryas Cooling, Klamath Mountains, Oregon, USA

    Open AccessDavid A Vacco, Peter U Clark et al.ARTICLEQuaternary Research2005

    A well-dated δ 18 O record in a stalagmite from a cave in the Klamath Mountains, Oregon, with a sampling interval of 50 yr, indicates that the climate of this region cooled essentially synchronously with Younger Dryas climate change elsewhere in the Northern Hemisphere. The δ 18 O record also indicates significant century-scale temperature variability during the early Holocene. The δ 13 C record suggests increasing biomass over the cave through t…

  • The World of the Tavern: Public Houses in Early Modern Europe

    P Clark, Peter U ClarkARTICLEThe English Historical Review2003Cited by: 7

    Journal Article The World of the Tavern: Public Houses in Early Modern Europe Get access Peter Clark Peter Clark Search for other works by this author on: Oxford Academic Google Scholar The English Historical Review, Volume 118, Issue 476, April 2003, Pages 513–514, https://doi.org/10.1093/ehr/118.476.513 Published: 01 April 2003

  • Willandra Lakes Archaeological Investigations 1968–98

    Open AccessHarvey Johnston, Peter U Clark et al.ARTICLEArchaeology in Oceania/Archæology…1998Cited by: 26References: 27

    The broadly generalised and widely cited late Pleistocene prehistory of the Willandra Lakes Region that has emerged over the last 30 years is based on analyses of a limited sample of the region's archaeology. This paper points to the expansive nature of Pleistocene sediments and archaeological exposures that exist in the region and identifies issues and problems faced by researchers who have investigated its archaeological record.Poorly understoo…

  • Unstable Behavior of the Laurentide Ice Sheet over Deforming Sediment and Its Implications for Climate Change

    Open AccessPeter U ClarkARTICLEQuaternary Research1994

    Geologic records of fluctuations of the Laurentide ice sheet margin following the most recent glacial maximum ( ca. 20,000 14 C yr B.P.) identify fundamental differences in ice-sheet behavior depending on subglacial bed conditions. Rapid and irregular icemargin fluctuations occurred only over areas of deforming sediment, indicating nonclimatic forcing controlled by the inherent instability of coupled ice sheet-deforming sediment dynamics. In cont…

  • Landscapes of Glacial Erosion, Torngat Mountains, Northern Labrador/Ungava

    Open AccessPeter U ClarkARTICLECanadian Geographies /…1991References: 13

  • Late Deglaciation of the Central Labrador Coast and Its Implications for the Age of Glacial Lakes Naskaupi and McLean and for Prehistory

    Open AccessPeter U Clark, William W FitzhughARTICLEQuaternary Research1990

    The age of the marine limit and associated deglaciation has been estimated from relative sea-level curves for the Hopedale and Nain areas of the central Labrador coast as approximately 7600 ± 200 and 8500 ± 200 yr ago, respectively. These ages indicate that the ice margin remained on the coast for up to 3000 yr longer than previously estimated. Because the central coast is due east of glacial lakes Naskaupi and McLean, the earliest the lakes coul…