Brenda L. Hall

University of Maine

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

George H. Denton

University of Maine

Thomas V. Lowell

University of Cincinnati

Gordon Bromley

Ollscoil na Gaillimhe – University of Galway

M. A. Kelly

Dartmouth College

Brent M. Goehring

Los Alamos National Laboratory

Keir A. Nichols

Imperial College London

Joanne S. Johnson

British Antarctic Survey

Greg Balco

Lawrence Livermore National Laboratory

Dylan H. Rood

Imperial College London

John Woodward

Northumbria University

Cooperative Institutions

University of Maine

Centre National de la Recherche Scientifique

United States Geological Survey

Columbia University

Lamont-Doherty Earth Observatory

University of Washington

British Antarctic Survey

University of Cambridge

Planetary Science Institute

Natural Environment Research Council

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Holocene glacial history of Renland Ice Cap, East Greenland, reconstructed from lake sediments

Quaternary Science Reviews (2021)

Aaron Medford Brenda L. Hall Thomas V. Lowell M. A. Kelly Laura B. Levy

Meltwater

Deglaciation

Ice core

10.1016/j.quascirev.2021.106883

Cite

Citations (21)

Antarctic Ice Sheet retreat in the western Ross Embayment since the Last Glacial Maximum constrained by geochronology and ice flow modeling

AGU Fall Meeting Abstracts (2018)

Trevor R. Hillebrand Courtney King Michelle Koutnik Jeffrey C. Stone Brenda L. Hall

Geochronology

Antarctic ice sheet

Source

Cite

Citations (0)

Holocene climate and environmental history of East Greenland inferred from lake sediments

Journal of Paleolimnology (2017)

Amanda R. Lusas Brenda L. Hall Thomas V. Lowell M. A. Kelly Ole Bennike

Deglaciation

Holocene climatic optimum

Meltwater

Greenland ice sheet

10.1007/s10933-017-9951-5

Cite

Citations (11)

Holocene history of the Wilson Piedmont Glacier along the southern Scott Coast, Antarctica

The Holocene (2002)

Brenda L. Hall George H. Denton

Geometric and cross-cutting relationships between the Wilson Piedmont Glacier and raised beach ridges indicate that the glacier margin has undergone Holocene ‘ uctuations. During mid-Holocene time, the Wilson Piedmont Glacier retreated to a position less extensive than at present. A subsequent readvance culmi nated less than 250 years ago. Since ad 1956, the glacier and adjacent large snow ramps have retreated up to 600 m in some locations. Large snowbanks have also disappeared. Although the cross-cutting relationships and chronology indicate a late-Holocene advance at approximately the same time as the ‘Little Ice Age’ event, the magnitude and style of that advance differ from those of the classic ‘Little Ice Age’ glacier ‘ uctuations in the Northern Hemisphere.

Glacier morphology

Cirque glacier

Little ice age

Chronology

10.1191/0959683602hl572rp

Cite

Citations (31)

History of the Antarctic Ice Sheet in the McMurdo Sound region at and since the Last Glacial Maximum: Evidence from Miers Valley

Quaternary Science Reviews (2024)

Tobias Koffman Brenda L. Hall George H. Denton Chris H. Hendy Gideon M. Henderson

Antarctic ice sheet

10.1016/j.quascirev.2024.108787