NDLI: The interannual and decadal variability of the sea level in the Japan/East Sea

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Journal of Ocean University of China : Volume 8, Issue 3, September 2009

Journal of Ocean University of China : Volume 8, Issue 2, June 2009

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Journal of Ocean University of China : Volume 7

Journal of Ocean University of China : Volume 6

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The interannual and decadal variability of the sea level in the Japan/East Sea

Content Provider	Springer Nature Link
Author	Wang, Tianshun Liu, Yuguang Zong, Haibo Rong, Zengrui
Copyright Year	2009
Abstract	Sea level observed by altimeter during the 1993–2007 period and the thermosteric sea level from 1945 through 2005 obtained by using the global ocean temperature data sets recently published are used to investigate the interannual and decadal variability of the sea level in the Japan/East Sea (JES) and its response to El Niño and Southern Oscillation (ENSO). Both the interannual variations of the sea level observed by altimeter and those of the thermosteric sea level obtained from reanalyzed data in the JES are closely related to ENSO. As a result, one important consequence is that the sea level trends are mainly caused by the thermal expansion in the JES. An ‘enigma’ is revealed that the correlation between the thermosteric sea level and ENSO during the PDO (Pacific Decadal Oscillation) warm phase (post mid-1970s) is inconsistent with that during the cold phase (pre mid-1970s) in the JES. The thermosteric sea level trends and the Southern Oscillation Index (SOI) suggest a strong negative correlation during the period 1977–1998, whereas there appears a relatively weak positive correlation during the period 1945–1976 in the JES. Based on the SODA (Simple Oceanographic Data Assimilation) datasets, possible mechanisms of the interannual and decadal variability of the sea level in the JES are discussed. Comprehensive analysis reveals that the negative anomalies of SOI correspond to the positive anomalies of the southeast wind stress, the net advective heat flux and the sea level in the JES during the PDO warm phase. During the PDO cold phase, the negative anomalies of SOI correspond to the positive anomalies of the southwest wind stress, the negative anomalies of the net advective heat flux and the sea level in the JES.
Starting Page	335
Ending Page	342
Page Count	8
File Format	PDF
ISSN	16725182
Journal	Journal of Ocean University of China
Volume Number	8
Issue Number	4
e-ISSN	19935021
Language	English
Publisher	Springer-Verlag
Publisher Date	2009-10-25
Publisher Place	Berlin, Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	interannual and decadal variability Japan/East Sea sea level anomalies thermosteric sea level anomalies ENSO Oceanography
Content Type	Text
Resource Type	Article
Subject	Oceanography Ocean Engineering

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