M
Matthew H. England
Researcher at University of New South Wales
Publications - 306
Citations - 20531
Matthew H. England is an academic researcher from University of New South Wales. The author has contributed to research in topics: Ocean current & Thermohaline circulation. The author has an hindex of 66, co-authored 283 publications receiving 17309 citations. Previous affiliations of Matthew H. England include Purdue University & Centre national de la recherche scientifique.
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Response of Southern Ocean Convection and Abyssal Overturning to Surface Buoyancy Perturbations
TL;DR: In this paper, the authors explore how buoyancy-driven modulations in the abyssal overturning circulation affect Southern Ocean temperature and salinity in an eddy-permitting ocean model and find that the modeled surface ocean south of 50°S cools and freshens in response to enhanced surface freshwater fluxes.
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Contribution of tropical instability waves to ENSO irregularity
TL;DR: In this article, the authors investigate the influence of tropical instability waves (TIWs) on ENSO using a hybrid coupled model coupled to a simple atmosphere, and they find that TIWs can induce a spread in the forecast amplitude of the Nino 3 SST anomaly 6-months after a given sequence of WWBs.
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A Region of Enhanced Northward Antarctic Intermediate Water Transport in a Coupled Climate Model
TL;DR: In this paper, a global coupled model is used to examine pathways of freshwater transport in the Southern Ocean, showing that meridional freshwater flows distributed nonuniformly around the globe, including in the upper ocean.
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Global and Regional Climate Response to Late Twentieth-Century Warming over the Indian Ocean
TL;DR: In this article, the global and regional climate response to a warming of the Indian Ocean is examined in an ensemble of atmospheric general circulation model experiments, where the increase in tropical SST is found to drive enhanced convection throughout the troposphere.
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The 1970's shift in ENSO dynamics: A linear inverse model perspective
TL;DR: In this paper, linear inverse models (LIMs) are constructed from tropical sea surface temperature (SST), thermocline depth, and zonal wind stress anomalies from the periods 1958-1977 and 1978-1997.