Quaternary Internatio e o

sity sity ng 9 N; 65 a 1.75 km2 desiccated peat bog in the low hills of central Marine records of the last glacial from offshore Taiwan show that low-latitude sea-surface temperature is not as Farrera et al., 1999). On the other hand, a chronological timing of temperature changes from the Greenland...

Full description

Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Greenland
Greenland ice core
ice core
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.565.7588
http://140.112.56.1/pollen/images/doc/liew147.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.565.7588
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.565.7588 2023-05-15T16:27:54+02:00 Quaternary Internatio e o The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.565.7588 http://140.112.56.1/pollen/images/doc/liew147.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.565.7588 http://140.112.56.1/pollen/images/doc/liew147.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://140.112.56.1/pollen/images/doc/liew147.pdf text ftciteseerx 2016-01-08T12:15:23Z sity sity ng 9 N; 65 a 1.75 km2 desiccated peat bog in the low hills of central Marine records of the last glacial from offshore Taiwan show that low-latitude sea-surface temperature is not as Farrera et al., 1999). On the other hand, a chronological timing of temperature changes from the Greenland ice core GISP2 (Wang et al., 2001). This indicates that the East ARTICLE IN PRESSAsian monsoon is integral to millennial-scale changes in atmosphere/oceanic circulation patterns and is affected by orbitally induced insolation variations. Remarkable Text Greenland Greenland ice core ice core Unknown Greenland
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description sity sity ng 9 N; 65 a 1.75 km2 desiccated peat bog in the low hills of central Marine records of the last glacial from offshore Taiwan show that low-latitude sea-surface temperature is not as Farrera et al., 1999). On the other hand, a chronological timing of temperature changes from the Greenland ice core GISP2 (Wang et al., 2001). This indicates that the East ARTICLE IN PRESSAsian monsoon is integral to millennial-scale changes in atmosphere/oceanic circulation patterns and is affected by orbitally induced insolation variations. Remarkable
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title Quaternary Internatio e o
spellingShingle Quaternary Internatio e o
title_short Quaternary Internatio e o
title_full Quaternary Internatio e o
title_fullStr Quaternary Internatio e o
title_full_unstemmed Quaternary Internatio e o
title_sort quaternary internatio e o
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.565.7588
http://140.112.56.1/pollen/images/doc/liew147.pdf
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland ice core
ice core
genre_facet Greenland
Greenland ice core
ice core
op_source http://140.112.56.1/pollen/images/doc/liew147.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.565.7588
http://140.112.56.1/pollen/images/doc/liew147.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766017472555646976

Similar Items