Recent Intensification Of Wind-driven Circulation In The Pacific And The Ongoing Warming Hiatus Pdf

recent intensification of wind-driven circulation in the pacific and the ongoing warming hiatus pdf

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The wind stress is a measure of momentum transfer due to the relative motion between the atmosphere and the ocean.

Recent intensification of wind-driven circulation in the Pacific and the ongoing warming hiatus

The formation of the ozone hole over the second half of the twentieth century is well understood to have resulted from increased anthropogenic emissions of halogenated trace gases such as chlorofluorocarbons [see Solomon for a review]. Pressing concerns about potentially harmful levels of surface UV radiation from a thinning ozone layer resulted in the signing of the Montreal Protocol, an international ban on emissions of ozone-depleting substances ODS , which went into effect in , with several subsequent amendments. Moreover, it is well known that ODS are powerful greenhouse gases Velders et al. In this paper we show that the considerable radiative forcing of ODS may have played a crucial role in determining trends in sea surface temperature SST , sea level pressure SLP , and circulation patterns in the tropical Indo-Pacific Ocean over the period — The Indo-Pacific Ocean is characterized by a cold tongue in the eastern side of the Pacific Ocean and a warm pool that straddles the Indian and Pacific Oceans. This east—west gradient in SST is responsible for the overturning Walker circulation, with air rising over the warm pool and descending over the cold tongue. The Walker circulation affects wind stress, ocean dynamics, and clouds, and it can thus have major climatic impacts.

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Recent intensification of wind-driven circulation in the Pacific and the ongoing warming hiatus · Supplemental Presentations · Figures from this paper · Figures.


Global warming hiatus contributed weakening of the Mascarene High in the Southern Indian Ocean

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All data used in this research are freely available and may be downloaded from the links given in the methods section. The codes used for all the analyses are freely available on request to the corresponding author. Apart from its large influence on African and Australian weather patterns, it also helps in driving the inter-hemispheric circulation between the Indian Ocean in the south and subcontinental landmass in the north. Using observations and reanalysis products, this study for the first time investigates recent warming trend observed in the MH region during the Global Warming Hiatus GWH period —

Acceleration of global mean ocean circulation under the climate warming

Recent work has demonstrated the important role of the Indian Ocean in modulating global climate variability SanchezGomez et al.

Introduction

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Brandon L.

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Recent studies have identified Pacific decadal variability as a major driver of periods of rapid and slower global mean surface air temperature change.

Coablabaclet

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This hiatus could persist for much of the present decade if the trade wind trends continue, however rapid warming is expected to resume once the.

Marcel P.

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Request PDF | Recent intensification of wind-driven circulation in the Pacific and the ongoing warming hiatus | Despite ongoing increases in.

Aya D.

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The system can't perform the operation now.

Charlotte W.

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