scholarly journals Evaluation of reconstructed sea surface temperatures based on U37k′ from sediment surface samples of the North Pacific

2020 ◽  
Vol 243 ◽  
pp. 106496
Author(s):  
Lars Max ◽  
Lester Lembke-Jene ◽  
Jianjun Zou ◽  
Xuefa Shi ◽  
Ralf Tiedemann
2018 ◽  
Vol 31 (12) ◽  
pp. 4669-4681 ◽  
Author(s):  
Samantha M. Wills ◽  
David W. J. Thompson

Observational analyses reveal that wintertime variations in sea surface temperatures (SST) in the Kuroshio–Oyashio Extension (KOE) region of the North Pacific are associated with two distinct and robust patterns of atmospheric variability: 1) a pattern that peaks in amplitude approximately 2–3 weeks prior to large KOE SST anomalies and is consistent with atmospheric forcing of the SST field and 2) a very different pattern that lags SST anomalies in the KOE region by approximately a month. The latter pattern is dominated by low sea level pressure anomalies and turbulent heat fluxes directed into the atmosphere over warm SST anomalies and is interpreted as the transient atmospheric response to SST anomalies over the KOE region. The results contribute to a growing body of evidence that suggests variations in SSTs in the midlatitude oceans are capable of significantly influencing the large-scale atmospheric circulation, especially near western boundary currents.


2007 ◽  
Vol 20 (4) ◽  
pp. 667-680 ◽  
Author(s):  
Soon-Il An ◽  
Jong-Seong Kug ◽  
Axel Timmermann ◽  
In-Sik Kang ◽  
Oliver Timm

Abstract This diagnostic study explores the generation of decadal variability in the North Pacific resulting from the asymmetry of the El Niño–Southern Oscillation phenomenon and the nonlinearity of the atmospheric tropical–extratropical teleconnection. Nonlinear regression analysis of the North Pacific sea surface temperatures and atmospheric fields with respect to the ENSO index reveals that the main teleconnection centers shift between El Niño and La Niña years. This asymmetry in the ENSO response, together with the skewed probabilistic distribution of ENSO itself, may contribute to the generation of the long-term decadal variability of sea surface temperatures in the extratropical North Pacific. It is argued that this hypothesis may explain the significant variance of the observed Pacific decadal oscillation in the extratropics.


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