| Authors | Chondrogianni C., Arztegui D., Rolph T., Juggins S., Shemesh A., Rietti-Shati M., Niessen F., Guilizzoni P., Lami A., McKenzie J.A., Oldfield F. |
| Text | 52825 2004 10.1016/j.quaint.2004.01.029 ISI Web of Science WOS 000223364500003 Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum Chondrogianni C., Arztegui D., Rolph T., Juggins S., Shemesh A., Rietti Shati M., Niessen F., Guilizzoni P., Lami A., McKenzie J.A., Oldfield F. a Geological Institute, ETH Zentrum, Sonneggstr. 5, Z. urich 8092, Switzerland bDepartment of Geology and Paleontology, Institute Forel, University of Geneva, Rue des Mara# chers 13, Geneva 1205, Switzerland cDepartment of Geology, University of Newcastle, Callaghan 2308, NSW, Australia dDepartment of Geography, University of Newcastle, Newcastle upon Tyne NE1 7RU, UK e Department of Environmental Sciences, Weizmann Institute of Sciences, Rehovot 76100, Israel f Alfred Wegener Institute for Polar and Marine Research, Bremerhaven 27515, Germany g CNR Istituto per lo Studio degli Ecosistemi, sezione di Idrobiologia ed Ecologia delle Acque Interne , Verbania Pallanza 28922, Italy hPAGES Core Project Office, B. arenplatz 2, Bern 3011, Switzerland 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 B15.0 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. r 2004 Elsevier Ltd and INQUA. All rights reserved. 122 Millennial to interannual climate variability in the Mediterranean during the Last Glacial Maximum 48_Chondrogianni.pdf Articolo in rivista Pergamon. 1040 6182 Quaternary international Quaternary international Quat. int. piero.guilizzoni GUILIZZONI PIERO andrea.lami LAMI ANDREA TA.P02.005.002 Uso della paleolimnologia come strumento per lo studio del paleoclima e dell evoluzione climatica |
