Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece
This study investigates the possibility of Holocene glaciation on Mount Olympus (Greece) with a respective local temperature–precipitation equilibrium line altitude (TP-ELA) at c. 2200 m a.s.l., based on geomorphologic and paleoclimatic evidence. At present, the local TP-ELA is situated above the mo...
Published in: | The Holocene |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
SAGE Publications
2015
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1177/0959683615618259 http://journals.sagepub.com/doi/pdf/10.1177/0959683615618259 http://journals.sagepub.com/doi/full-xml/10.1177/0959683615618259 |
id |
crsagepubl:10.1177/0959683615618259 |
---|---|
record_format |
openpolar |
spelling |
crsagepubl:10.1177/0959683615618259 2024-09-15T18:23:56+00:00 Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece Styllas, Michael Nikolaos Schimmelpfennig, Irene Ghilardi, Matthieu Benedetti, Lucilla 2015 http://dx.doi.org/10.1177/0959683615618259 http://journals.sagepub.com/doi/pdf/10.1177/0959683615618259 http://journals.sagepub.com/doi/full-xml/10.1177/0959683615618259 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 26, issue 5, page 709-721 ISSN 0959-6836 1477-0911 journal-article 2015 crsagepubl https://doi.org/10.1177/0959683615618259 2024-07-29T04:24:48Z This study investigates the possibility of Holocene glaciation on Mount Olympus (Greece) with a respective local temperature–precipitation equilibrium line altitude (TP-ELA) at c. 2200 m a.s.l., based on geomorphologic and paleoclimatic evidence. At present, the local TP-ELA is situated above the mountain’s summit ( c. 2918 m a.s.l.), but permanent snowfields and ice bodies survive within Megala Kazania cirque between c. 2400 and c. 2300 m a.s.l., because of the cirque’s maritime setting that results from its close proximity ( c. 18 km) to the Aegean Sea and of the local topographical controls. The snow and ice bodies occupied a considerably larger area and attained a stabilization phase between AD 1960 and 1980, also manifested from aerial photographs, a period characterized by increased winter precipitation ( P w ) with subsequent TP-ELA depression to c. 2410 m a.s.l. Mid- to late-20th-century P w and TP-ELA variations exhibit negative correlations with the winter North Atlantic Oscillation index (NAO w ) at annual and multidecadal (30 years) timescales. Late Holocene (AD 1680–1860) reconstructed summer mean temperatures were lower by T s < 1.1°C in relation to the reference period between AD 1960 and 1980 and were also superimposed to negative NAO w phases, thus bracketing this time interval as a favorable one to glacial formation and/or advance. Millennial-scale annual precipitation reconstructions at the hypothesized TP-ELA ( c. 2200 m a.s.l.) point the period between 8 and 4 kyr BP as another glacier-friendly candidate. The mid-Holocene rather simplistic sequence of potential glacial advance phase was disturbed by short-lived cold climatic deteriorations, well-documented over the northern Aegean region that may partly explain the multicrested shape of the highest ( c. 2200 m a.s.l.) morainic complex of Megala Kazania cirque. Article in Journal/Newspaper North Atlantic North Atlantic oscillation SAGE Publications The Holocene 26 5 709 721 |
institution |
Open Polar |
collection |
SAGE Publications |
op_collection_id |
crsagepubl |
language |
English |
description |
This study investigates the possibility of Holocene glaciation on Mount Olympus (Greece) with a respective local temperature–precipitation equilibrium line altitude (TP-ELA) at c. 2200 m a.s.l., based on geomorphologic and paleoclimatic evidence. At present, the local TP-ELA is situated above the mountain’s summit ( c. 2918 m a.s.l.), but permanent snowfields and ice bodies survive within Megala Kazania cirque between c. 2400 and c. 2300 m a.s.l., because of the cirque’s maritime setting that results from its close proximity ( c. 18 km) to the Aegean Sea and of the local topographical controls. The snow and ice bodies occupied a considerably larger area and attained a stabilization phase between AD 1960 and 1980, also manifested from aerial photographs, a period characterized by increased winter precipitation ( P w ) with subsequent TP-ELA depression to c. 2410 m a.s.l. Mid- to late-20th-century P w and TP-ELA variations exhibit negative correlations with the winter North Atlantic Oscillation index (NAO w ) at annual and multidecadal (30 years) timescales. Late Holocene (AD 1680–1860) reconstructed summer mean temperatures were lower by T s < 1.1°C in relation to the reference period between AD 1960 and 1980 and were also superimposed to negative NAO w phases, thus bracketing this time interval as a favorable one to glacial formation and/or advance. Millennial-scale annual precipitation reconstructions at the hypothesized TP-ELA ( c. 2200 m a.s.l.) point the period between 8 and 4 kyr BP as another glacier-friendly candidate. The mid-Holocene rather simplistic sequence of potential glacial advance phase was disturbed by short-lived cold climatic deteriorations, well-documented over the northern Aegean region that may partly explain the multicrested shape of the highest ( c. 2200 m a.s.l.) morainic complex of Megala Kazania cirque. |
format |
Article in Journal/Newspaper |
author |
Styllas, Michael Nikolaos Schimmelpfennig, Irene Ghilardi, Matthieu Benedetti, Lucilla |
spellingShingle |
Styllas, Michael Nikolaos Schimmelpfennig, Irene Ghilardi, Matthieu Benedetti, Lucilla Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece |
author_facet |
Styllas, Michael Nikolaos Schimmelpfennig, Irene Ghilardi, Matthieu Benedetti, Lucilla |
author_sort |
Styllas, Michael Nikolaos |
title |
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece |
title_short |
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece |
title_full |
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece |
title_fullStr |
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece |
title_full_unstemmed |
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece |
title_sort |
geomorphologic and paleoclimatic evidence of holocene glaciation on mount olympus, greece |
publisher |
SAGE Publications |
publishDate |
2015 |
url |
http://dx.doi.org/10.1177/0959683615618259 http://journals.sagepub.com/doi/pdf/10.1177/0959683615618259 http://journals.sagepub.com/doi/full-xml/10.1177/0959683615618259 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
The Holocene volume 26, issue 5, page 709-721 ISSN 0959-6836 1477-0911 |
op_rights |
http://journals.sagepub.com/page/policies/text-and-data-mining-license |
op_doi |
https://doi.org/10.1177/0959683615618259 |
container_title |
The Holocene |
container_volume |
26 |
container_issue |
5 |
container_start_page |
709 |
op_container_end_page |
721 |
_version_ |
1810464223249039360 |