scholarly journals Precipitation Regime Shift Associated with the Pacific Decadal Oscillation in the Maritime Continent

2020 ◽  
Vol 09 (02) ◽  
pp. 123-135
Author(s):  
V. Kokorev ◽  
J. Ettema ◽  
P. Siegmund ◽  
G. van der Schrier
Keyword(s):  
Pacific Decadal Oscillation ◽  
Regime Shift ◽  
Maritime Continent ◽  
Precipitation Regime ◽  
The Pacific

On the Pacific Ocean regime shift

2001 ◽  
Vol 28 (19) ◽  
pp. 3721-3724
Author(s):  
Cathy Stephens
Keyword(s):  
Pacific Ocean ◽  
Regime Shift ◽  
The Pacific ◽  
The Pacific Ocean

scholarly journals The climate regime shift over the Pacific during 1996/1997

2013 ◽  
Vol 43 (1-2) ◽  
pp. 435-446 ◽  
Author(s):  
Chi-Cherng Hong ◽  
Yi-Kai Wu ◽  
Tim Li ◽  
Chih-Chun Chang
Keyword(s):  
Regime Shift ◽  
Climate Regime ◽  
Climate Regime Shift ◽  
The Pacific

scholarly journals Salinity signature of the Pacific Decadal Oscillation

1999 ◽  
Vol 26 (9) ◽  
pp. 1337-1340 ◽  
Author(s):  
James E. Overland ◽  
Sigrid Salo ◽  
Jennifer Miletta Adams
Keyword(s):  
Pacific Decadal Oscillation ◽  
The Pacific

scholarly journals North Pacific dissolved inorganic carbon variations related to the Pacific Decadal Oscillation

2014 ◽  
Vol 41 (3) ◽  
pp. 1005-1011 ◽  
Author(s):  
Sayaka Yasunaka ◽  
Yukihiro Nojiri ◽  
Shin-ichiro Nakaoka ◽  
Tsuneo Ono ◽  
Hitoshi Mukai ◽  
...  
Keyword(s):  
Pacific Decadal Oscillation ◽  
North Pacific ◽  
Inorganic Carbon ◽  
Dissolved Inorganic Carbon ◽  
The Pacific

scholarly journals Coral Luminescence Identifies the Pacific Decadal Oscillation as a Primary Driver of River Runoff Variability Impacting the Southern Great Barrier Reef

PLoS ONE ◽  
2014 ◽  
Vol 9 (1) ◽  
pp. e84305 ◽  
Author(s):  
Alberto Rodriguez-Ramirez ◽  
Craig A. Grove ◽  
Jens Zinke ◽  
John M. Pandolfi ◽  
Jian-xin Zhao
Keyword(s):  
Great Barrier Reef ◽  
Pacific Decadal Oscillation ◽  
River Runoff ◽  
Barrier Reef ◽  
The Pacific ◽  
Primary Driver ◽  
Runoff Variability

Manifestation of the Pacific Decadal Oscillation in the stationary planetary waves activity

2021 ◽  
Author(s):  
Daria Sobaeva ◽  
Yulia Zyulyaeva ◽  
Sergey Gulev
Keyword(s):  
Pacific Decadal Oscillation ◽  
North American ◽  
Lower Stratosphere ◽  
El Nino ◽  
Planetary Waves ◽  
Positive Phase ◽  
Negative Phase ◽  
Middle Troposphere ◽  
The Pacific ◽  
The Tropics

<p>Strong quasi-decadal oscillations of the stratospheric polar vortex (SPV) intensity are in phase with the Pacific decadal oscillation (PDO). A stronger SPV is observed during the positive phase of the PDO, and during the negative phase, the intensity of the SPV is below the mean climate values. The SPV intensity anomalies, formed by the planetary waves and zonal mean flow interaction, lead to the weakening/intensification of the vortex.</p><p>This research aimed to obtain the differences in the characteristics and the spatial propagation pattern of the planetary waves in the middle troposphere and lower stratosphere during different PDO phases. We analyzed composite periods of years when the PDO index has extremely high and low values. Two periods were constructed for both positive and negative phases, the first consisting of years with El-Nino/La-Nina events and the second without prominent sea surface temperature anomalies in the tropics. </p><p>During the wintertime in the Northern Hemisphere (December-February), wave 2 with two ridges (Siberian and North American Highs) and two troughs (Icelandic and Aleutian Lows) dominates in the middle troposphere, along with wave 1 dominating in the lower stratosphere. In the middle troposphere, at the positive phase ​​of the PDO, the amplitude of wave 2 is higher than in years with negative values of the PDO index. The differences in the Aleutian Low and the North American High intensity between the two phases are significant at the 97.5% level. In the lower stratosphere, the wave amplitude is lower at the negative phase ​​of the PDO, but we can also talk about a slight shift of the wave phase to the east. The regions of the heavy rains in the tropics during El-Nino events are the planetary waves source. They propagate from low to high latitudes, which results in modifying the characteristics and locations of the intensification of the stationary planetary waves in mid-latitudes.</p>

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