noaa-cave-6211
Zhou et al. 2008 Suozi Cave, China MIS 5 Speleothem Stable Isotope Data
Zhou, H.; Zhao, J.-x.; Zhang, P.; Shen, C.-C.; Chi, B.; Feng, Y.-x.; Lin, Y.; Guan, H.; You, C.-F.
Zhou et al. 2008 Suozi Cave, China MIS 5 Speleothem Stable Isotope Data
2008-07-01
NCDC-Paleoclimatology
ONLINE Files
Pending
https://www.ncdc.noaa.gov/paleo/study/6211
Investigator
H.
Zhou
Investigator
J.-x.
Zhao
Investigator
P.
Zhang
Investigator
C.-C.
Shen
Investigator
B.
Chi
Investigator
Y.-x.
Feng
Investigator
Y.
Lin
Investigator
H.
Guan
Investigator
C.-F.
You
earth science
paleoclimate
speleothems
depth,null,null,millimeter,null,speleothems,null,null,N,null
earth science
paleoclimate
speleothems
delta 18O,calcium carbonate,null,per mil VPDB,null,speleothems,raw,isotope ratio mass spectrometry,N,null
earth science
paleoclimate
speleothems
age,null,null,calendar kiloyear before present,null,speleothems,null,null,N,null
earth science
paleoclimate
speleothems
delta 13C,calcium carbonate,null,per mil VPDB,null,speleothems,raw,isotope ratio mass spectrometry,N,null
earth science
paleoclimate
speleothems
carbon isotopes
earth science
paleoclimate
speleothems
oxygen isotopes
geoscientificInformation
-117340 AD
-100810 AD
119290 cal yr BP
102760 cal yr BP
Complete
32.43
32.43
107.17
107.17
700
700
Continent
Asia
Eastern Asia
China
Souzi Cave>LATITUDE 32.43>LONGITUDE 107.17
None
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English
DOC/NOAA/NESDIS/NCEI
National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce
https://www.ncdc.noaa.gov/data-access/paleoclimatology-data
DATA Center Contact
Bruce
Bauer
bruce.a.bauer@noaa.gov
paleo@noaa.gov
303-497-6280
303-497-6513
325 Broadway, E/NE31
Boulder
CO
80305-3328
USA
online
ASCII
Zhou, H.,Zhao, J.-x.,Zhang, P.,Shen, C.-C. ,Chi, B.,Feng, Y.,Lin, Y.,Guan, H.,You, C.-F. 2008. Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d. Quaternary Research, 70(2), 315-321.
The Asian monsoon is an important component of the global climate system. Seasonal variations in wind, rainfall, and temperature associated with the Asian monsoon systems affect a vast expanse of tropical and subtropical Asia. Speleothem-derived summer monsoon variation in East Asia was previously found to be closely associated with millennial-scale change in temperature in the North Atlantic region between 75 and 10 ka. New evidence recovered from East Asia, however, suggests that the teleconnection between summer monsoon in East Asia and temperature change in the North Atlantic region may have significantly reduced during 120 to ~ 110 ka, a period directly after the full last interglaciation and corresponding roughly to marine oxygen isotope stage 5d. This reduction may be due to the low ice volume in the North Hemisphere at that time, which makes the millennial-scale change in temperature in the North Atlantic region less effective in influencing the Asian summer monsoon. This is important for investigating the mechanisms controlling the Asian summer monsoon and the paleoclimatic teleconnection between East Asia and the North Atlantic region, and for predicting monsoon-associated precipitation in East Asia under a global-warming trend.
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/china/suozi2008.txt
USA/NOAA
DIF
Version 9.8.4
2019-04-01
2019-04-01