The role of summer monsoon-typhoons in the formation of nearshore coarse-grained ripples, depression, and sand-ridge systems along the Shimizu coast, Suruga Bay facing the Pacific Ocean, Japan

2014 ◽  
Vol 353 ◽  
pp. 84-98 ◽  
Author(s):  
Shuro Yoshikawa ◽  
Kenji Nemoto
Keyword(s):  
Pacific Ocean ◽  
Summer Monsoon ◽  
Coarse Grained ◽  
Sand Ridge ◽  
Suruga Bay ◽  
The Pacific ◽  
The Pacific Ocean

scholarly journals Surface ocean iron fertilization: The role of airborne volcanic ash from subduction zone and hot spot volcanoes and related iron fluxes into the Pacific Ocean

2011 ◽  
Vol 25 (4) ◽  
pp. n/a-n/a ◽  
Author(s):  
Nazlı Olgun ◽  
Svend Duggen ◽  
Peter Leslie Croot ◽  
Pierre Delmelle ◽  
Heiner Dietze ◽  
...  
Keyword(s):  
Pacific Ocean ◽  
Subduction Zone ◽  
Volcanic Ash ◽  
Hot Spot ◽  
Surface Ocean ◽  
Iron Fertilization ◽  
The Pacific ◽  
The Pacific Ocean

scholarly journals A Recent Shift in the Monsoon Centers Associated with the Tropospheric Biennial Oscillation

2017 ◽  
Vol 31 (1) ◽  
pp. 325-340 ◽  
Author(s):  
Lei Wang ◽  
Jin-Yi Yu
Keyword(s):  
Pacific Ocean ◽  
Atlantic Ocean ◽  
Summer Monsoon ◽  
Indian Monsoon ◽  
Tropical Atlantic ◽  
Tropospheric Biennial Oscillation ◽  
The Pacific ◽  
The Pacific Ocean ◽  
Biennial Oscillation ◽  
Australian Summer

Abstract The tropospheric biennial oscillation (TBO) is conventionally considered to involve transitions between the Indian and Australian summer monsoons and the interactions between these two monsoons and the underlying Indo-Pacific Oceans. Here it is shown that, since the early 1990s, the TBO has evolved to mainly involve the transitions between the western North Pacific (WNP) and Australian monsoons. In this framework, the WNP monsoon replaces the Indian monsoon as the active Northern Hemisphere TBO monsoon center during recent decades. This change is found to be caused by stronger Pacific–Atlantic coupling and an increased influence of the tropical Atlantic Ocean on the Indian and WNP monsoons. The increased Atlantic Ocean influence damps the Pacific Ocean influence on the Indian summer monsoon (leading to a decrease in its variability) but amplifies the Pacific Ocean influence on the WNP summer monsoon (leading to an increase in its variability). These results suggest that the Pacific–Atlantic interactions have become more important to the TBO dynamics during recent decades.

Exploring the role of Micronesian islands in the maintenance of coral genetic diversity in the Pacific Ocean

2014 ◽  
Vol 24 (1) ◽  
pp. 70-82 ◽  
Author(s):  
S. W. Davies ◽  
E. A. Treml ◽  
C. D. Kenkel ◽  
M. V. Matz
Keyword(s):  
Genetic Diversity ◽  
Pacific Ocean ◽  
The Pacific ◽  
The Pacific Ocean

scholarly journals 100-th anniversary of the Pacific Science Association

2020 ◽  
pp. 124-146
Author(s):  
В.И. СЕРГИЕНКО ◽  
М.Б. ШТЕЦ
Keyword(s):  
Pacific Ocean ◽  
Pacific Rim ◽  
Pacific Region ◽  
Scientific Organizations ◽  
The Pacific ◽  
History Of ◽  
The Pacific Ocean ◽  
Academy Of Sciences ◽  
Science Association

В статье рассматривается история создания и развития Тихоокеанской научной ассоциации, объединяющей научные организации стран Тихоокеанского региона, а также участие Российской академии наук в ассоциации. Освещается роль ассоциации в международном исследовании Тихого океана и стран Тихоокеанского бассейна. An article considers the history of the establishment and development of the Pacific Science Association, which unites scientific organizations of the Pacific Region countries, and the participation of Russian Academy of Sciences in the Association. The role of the Association in the international exploration of the Pacific Ocean and the Pacific Rim countries is highlighted.

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
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