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Vladimir Byshev, Anatoly Gusev, Victor Neiman and Alexandra Sidorova
A Specific feature of the present-day climate dynamics consists in its multidecadal oscillations with a period of about 20?60 years, and intradecadal disturbances with time scales of 2?8 years. The period of 1940?1999 was distinctive due to the two?phase...
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Andrey V. Pnyushkov, Genrikh V. Alekseev and Alexander V. Smirnov
We investigated liquid freshwater content (FWC) in the upper 100 m layer of the Arctic Ocean using oceanographic observations covering the period from 1990 through 2018. Our analysis revealed two opposite tendencies in freshwater balance?the freshening i...
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Peter C. Chu and Chenwu Fan
This paper identifies world thermocline weakening and provides an improved estimate of upper ocean warming through replacement of the upper layer with the fixed depth range by the isothermal layer, because the upper ocean isothermal layer (as a whole) ex...
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Victoria L. Ford, Nan D. Walker and Iam-Fei Pun
The 2014 Northeast Pacific hurricane season was highly active, with above-average intensity and frequency events, and a rare landfalling Hawaiian hurricane. We show that the anomalous northern extent of sea surface temperatures and anomalous vertical ext...
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Jiagen Li, Liang Sun, Yuanjian Yang and Hao Cheng
We introduce a novel method to accurately evaluate the satellite-observed sea surface temperature (SST) cooling induced by typhoons with complex tracks, which is widely used but only roughly calculated in previous studies. This method first records the t...
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Francesco Ragone, Andrea Meli, Anna Napoli and Claudia Pasquero
The Western Mediterranean Sea is often subject to intense winds, especially during the winter season. Intense winds induce surface cooling associated with anomalous ocean heat loss, upwelling and diapycnal mixing. In this study we investigate the overall...
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Marcos Tonelli, Fernanda Marcello, Bruno Ferrero and Ilana Wainer
Water transformation around Antarctica is recognized to significantly impact the climate. It is where the linkage between the upper and lower limbs of the Meridional Overturning Circulation (MOC) takes place by means of dense water formation, which may b...
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Meer Mohammed Ali, Neetu Singh, Manchikanti Suresh Kumar, Yangxing Zheng, Mark Bourassa, Chandra Mohan Kishtawal and Chandu Venkateswara Rao
The thermal energy needed for the development of hurricanes and monsoons as well as any prolonged marine weather event comes from layers in the upper oceans, not just from the thin layer represented by sea surface temperature alone. Ocean layers have dif...
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