Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum
Climate change during the late Pleistocene is dominated by periodicities on millennial time scales as documented by ice cores and sedimentary marine and terrestrial records of global distribution. Interannual to decadal variations have also been demonstrated in dust concentrations in Greenland ice c...
Main Authors: | , , , , , , , , , , |
---|---|
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Pergamon
2004
|
Subjects: | |
Online Access: | http://hdl.handle.net/1959.13/34532 |
id |
ftunivnewcastnsw:uon:3573 |
---|---|
record_format |
openpolar |
spelling |
ftunivnewcastnsw:uon:3573 2023-05-15T16:28:52+02:00 Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum Chonrogianni, Christina Ariztegui, Daniel Oldfield, Frank Rolph, Tim Juggins, Stephen Shemesh, Aldo Rietti-Shati, Miri Niessen, Frank Guilizzoni, Piero Lami, Andrea McKenzie, Judith A. The University of Newcastle. Faculty of Science & Information Technology, School of Environmental and Life Science 2004 http://hdl.handle.net/1959.13/34532 eng eng Pergamon Quaternary International Vol. 122, Issue 1, p. 31-41 10.1016/j.quaint.2004.01.029 Pleistocene millennial time scale ice cores marine records terrestrial sedimentary journal article 2004 ftunivnewcastnsw 2018-07-27T01:04:27Z Climate change during the late Pleistocene is dominated by periodicities on millennial time scales as documented by ice cores and sedimentary marine and terrestrial records of global distribution. Interannual to decadal variations have also been demonstrated in dust concentrations in Greenland ice cores but there is lack of comparable detail in sedimentary records. An 8.5 m long multiproxy record from Lake Albano (central Italy) spanning the time interval between 15.0 and 28.0 cal kyr BP reveals a high temporal resolution window into climate change during the Last Glacial Maximum (LGM). Distinct warm/cold cycles of millennial to centennial duration indicate a major response of the lake to climate-induced environmental changes. Flickering interannual to interdecadal variations within these cycles are interpreted to reflect oscillations of the North Atlantic (NAO) implying shifts in temperature, wind strength, source of moisture and atmospheric circulation pattern. Article in Journal/Newspaper Greenland Greenland ice cores North Atlantic NOVA: The University of Newcastle Research Online (Australia) Greenland |
institution |
Open Polar |
collection |
NOVA: The University of Newcastle Research Online (Australia) |
op_collection_id |
ftunivnewcastnsw |
language |
English |
topic |
Pleistocene millennial time scale ice cores marine records terrestrial sedimentary |
spellingShingle |
Pleistocene millennial time scale ice cores marine records terrestrial sedimentary Chonrogianni, Christina Ariztegui, Daniel Oldfield, Frank Rolph, Tim Juggins, Stephen Shemesh, Aldo Rietti-Shati, Miri Niessen, Frank Guilizzoni, Piero Lami, Andrea McKenzie, Judith A. Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum |
topic_facet |
Pleistocene millennial time scale ice cores marine records terrestrial sedimentary |
description |
Climate change during the late Pleistocene is dominated by periodicities on millennial time scales as documented by ice cores and sedimentary marine and terrestrial records of global distribution. Interannual to decadal variations have also been demonstrated in dust concentrations in Greenland ice cores but there is lack of comparable detail in sedimentary records. An 8.5 m long multiproxy record from Lake Albano (central Italy) spanning the time interval between 15.0 and 28.0 cal kyr BP reveals a high temporal resolution window into climate change during the Last Glacial Maximum (LGM). Distinct warm/cold cycles of millennial to centennial duration indicate a major response of the lake to climate-induced environmental changes. Flickering interannual to interdecadal variations within these cycles are interpreted to reflect oscillations of the North Atlantic (NAO) implying shifts in temperature, wind strength, source of moisture and atmospheric circulation pattern. |
author2 |
The University of Newcastle. Faculty of Science & Information Technology, School of Environmental and Life Science |
format |
Article in Journal/Newspaper |
author |
Chonrogianni, Christina Ariztegui, Daniel Oldfield, Frank Rolph, Tim Juggins, Stephen Shemesh, Aldo Rietti-Shati, Miri Niessen, Frank Guilizzoni, Piero Lami, Andrea McKenzie, Judith A. |
author_facet |
Chonrogianni, Christina Ariztegui, Daniel Oldfield, Frank Rolph, Tim Juggins, Stephen Shemesh, Aldo Rietti-Shati, Miri Niessen, Frank Guilizzoni, Piero Lami, Andrea McKenzie, Judith A. |
author_sort |
Chonrogianni, Christina |
title |
Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum |
title_short |
Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum |
title_full |
Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum |
title_fullStr |
Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum |
title_full_unstemmed |
Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum |
title_sort |
millennial to interannual climate variability in the mediterranean during the last glacial maximum |
publisher |
Pergamon |
publishDate |
2004 |
url |
http://hdl.handle.net/1959.13/34532 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland ice cores North Atlantic |
genre_facet |
Greenland Greenland ice cores North Atlantic |
op_relation |
Quaternary International Vol. 122, Issue 1, p. 31-41 10.1016/j.quaint.2004.01.029 |
_version_ |
1766018556050276352 |