[Keyword='oxygen Isotopes']
Arabian Sea Summer Monsoon Proxy Data for the Past 3.5 Myr
Entry ID:
NOAA_NCDC_PALEO_2005-082
Summary
Abstract:
Paleoclimate records indicate that the strength of the Asian summer monsoon is
sensitive to orbital forcing at the obliquity and precession periods (41,000 and 23,000 years, respectively) and the extent of Northern Hemisphere glaciation. Over the past 2.6 million years, the timing (phase) of strong monsoons has changed by ~83° in the precession and ~124° in the obliquity bands relative to the phase of maximum global ice-volume (inferred from the marine d18O record). These results suggest that one or both of these systems is nonstationary relative to orbital forcing. Geographic Coverage
Spatial coordinates
Data Set Citation
Dataset Originator/Creator:
Clemens, S.C., D.W. Murray, and W.L. Prell
Dataset Title:
Arabian Sea Summer Monsoon Proxy Data for the Past 3.5 Myr
Dataset Series Name:
IGBP PAGES/WDCA CONTRIBUTION SERIES NUMBER: 2005-082
Dataset Release Date:
12/2005
Dataset Release Place:
Boulder,CO
Dataset Publisher:
IGBP PAGES/World Data Center for Paleoclimatology
Issue Identification:
2005-082
Other Citation Details:
NOAA/NCDC Paleoclimatology Program
Online Resource:
ftp://ftp.ncdc.noaa.gov/pub/data/paleo/paleocean/by_contributor/cle...
Paleo Temporal Coverage
Paleo Start Date:
3.5 ma
Paleo Stop Date: 0 ma Chrono Unit: Chrono Unit: Location Keywords
ISO Topic Category
Ancillary Keywords
Data Set Progress
COMPLETE
Originating Center
Data Center
Distribution
Distribution Media:
ftp
Distribution Format:
text, excel
Fees:
none
Personnel
Role:
INVESTIGATOR
Contact Address:
Brown University
Province or State:
RI
Country:
USA
Publications/References
Clemens, S.C., D.W. Murray, and W.L. Prell. 1996. Nonstationary phase of the
Plio-Pleisotcene Asian Monsoon. Science, 274, 943-948. Extended Metadata Properties
(Click to view more)
Creation and Review Dates
DIF Creation Date:
2006-11-08
Last DIF Revision Date:
2018-02-05
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