His primary areas of investigation include Oceanography, Radiocarbon dating, Paleoclimatology, Younger Dryas and Paleontology. He focuses mostly in the field of Oceanography, narrowing it down to topics relating to Glacial period and, in certain cases, Ice sheet, Structural basin and Ice core. His Ice core study combines topics in areas such as Epigravettian, Multi proxy and Geomorphology.
His Radiocarbon dating research is multidisciplinary, incorporating perspectives in Pleistocene and Physical geography. His research integrates issues of Tropical Atlantic and Intertropical Convergence Zone in his study of Paleoclimatology. The concepts of his Younger Dryas study are interwoven with issues in Deglaciation and Quaternary.
Konrad A Hughen mainly investigates Oceanography, Dendrochronology, Subfossil, Pinus
The various areas that Konrad A Hughen examines in his Ice core study include Younger Dryas, Paleontology and Stadial. When carried out as part of a general Paleontology research project, his work on Before Present, Chronology and Varve is frequently linked to work in Calibration, therefore connecting diverse disciplines of study. His work on Absolute dating as part of general Radiocarbon dating study is frequently linked to Foraminifera, therefore connecting diverse disciplines of science.
Konrad A Hughen mostly deals with Sediment core, Geochemistry, Oceanography, Radiocarbon dating and Environmental science. His Oceanography research focuses on subjects like Sediment, which are linked to Structural basin. His studies deal with areas such as Inversion, Physical geography and Extinction event as well as Radiocarbon dating.
His Physical geography study combines topics from a wide range of disciplines, such as Ocean circulation model, Archaeological record, Agathis australis and Earth system science. His studies in Coral integrate themes in fields like Reef, East Asian Monsoon, El Niño Southern Oscillation and Microbial ecology. His Sea surface temperature research is multidisciplinary, incorporating perspectives in Glacial period, Deglaciation, Salinity, Climate change and Ocean current.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
IntCal13 and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP
Paula J Reimer;Edouard Bard;Alex Bayliss;J Warren Beck.
INTCAL98 Radiocarbon Age Calibration, 24,000-0 cal BP
M Stuiver;P.J Reimer;E Bard;J.W Beck.
IntCal04 terrestrial radiocarbon age calibration, 0-26 cal kyr BP
Paula J. Reimer;Mike G.L. Baillie;Edouard Bard;Alex Bayliss.
Southward Migration of the Intertropical Convergence Zone Through the Holocene
Gerald H. Haug;Konrad A. Hughen;Daniel M. Sigman;Larry C. Peterson.
The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0-55 cal kBP)
Paula J Reimer;William E N Austin;Edouard Bard;Alex Bayliss.
Arctic Environmental Change of the Last Four Centuries
J. Overpeck;K. Hughen;D. Hardy;R. Bradley.
Marine04 marine radiocarbon age calibration, 0-26 cal kyr BP
Konrad A Hughen;Mike G L Baillie;Edouard Bard;J Warren Beck.
Climate and the Collapse of Maya Civilization
Gerald H. Haug;Detlef Günther;Larry C. Peterson;Daniel Mikhail Sigman.
Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial.
Larry C. Peterson;Gerald H. Haug;Konrad A. Hughen;Ursula Röhl.
Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records
Mike Walker;Sigfus Johnsen;Sune Olander Rasmussen;Trevor Popp;Trevor Popp.
Journal of Quaternary Science (2009)
If you think any of the details on this page are incorrect, let us know.
We appreciate your kind effort to assist us to improve this page, it would be helpful providing us with as much detail as possible in the text box below: