Member Since 2002
Matthew H. England
Professor and Deputy Director, CMSI, University of New South Wales
AGU Research
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Freshwater forcing from Greenland and Antarctica
FORCINGS, RESPONSES, AND FEEDBACKS IN THE EARTH SYSTEM III POSTER
global environmental change | 09 december 2024
Kenneth Mankoff, Julie Arblaster, Jonathan L. Bamb...
Increasing rates of freshwater fluxes from the Greenlandic and Antarctic ice sheets and ice shelves affect regional and global oceanographic propertie...
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Closing the Loops on Southern Ocean Dynamics: From the Circumpolar Current to Ice Shelves and From Bottom Mixing to Surface Waves
REVIEWS OF GEOPHYSICS
30 july 2024
Luke Bennetts, Callum J. Shakespeare, Catherine A....
A holistic review is given of the Southern Ocean dynamic system, in the context of the crucial role it plays in the global climate and the profound...
Subsurface Warming of the West Antarctic Continental Shelf Linked to El Niño‐Southern Oscillation
GEOPHYSICAL RESEARCH LETTERS
08 april 2024
Maurice Huguenin, Ryan Holmes, Paul Spence, Matthe...
Recent observations suggest that El Niño–Southern Oscillation (ENSO) impacts basal melting of West Antarctic ice shelves, yet sparse oce...
Oceanic rafting of floating debris and organisms to Antarctic coasts from Southern Hemisphere landmasses
MARINE ECOSYSTEMS ACROSS SCALES OF SPACE, TIME, AND BIOLOGY III ORAL
marine ecology and biodiversity | 22 february 2024
Hannah Dawson, Adele K. Morrison, Matthew H. Engla...
Antarcticas marine environment is no longer considered isolated from the rest of the global ocean. Recent research has demonstrated that there are via...
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Recent acceleration in global ocean heat accumulation by mode and intermediate waters using Argo measurements
THE OCEAN IN THE EARTH’S ENERGY AND WATER CYCLES I POSTER
climate and ocean change | 22 february 2024
Zhi Li, Matthew H. England, Sjoerd Groeskamp
The ocean absorbs >90% of anthropogenic heat in the Earth system, moderating global atmospheric warming. However, it remains unclear how this heat ...
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On the link between bottom water production and Weddell Gyre strength
VARIABILITY, CIRCULATION, AND TRANSFORMATION IN THE OPEN SOUTHERN OCEAN I ORAL
high latitude environments | 22 february 2024
Julia Neme, Matthew H. England, Andrew M. Hogg, He...
The Weddell Gyre is one of the dominant features of the Southern Ocean circulation and its dynamics have been linked to processes of climatic relevanc...
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Drivers of the largest ever recorded marine heat wave in the North Atlantic
MARINE HEAT WAVES IN A CHANGING WORLD I ORAL
climate and ocean change | 21 february 2024
Matthew H. England, Stefan Rahmstorf, Andrew E. Ki...
North Atlantic ocean circulation and temperature patterns fundamentally control global and regional climate across all time scales, from synoptic to m...
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Wind– and sea-ice–driven interannual variability of Antarctic Bottom Water formation
ICE-OCEAN INTERACTIONS, CIRCULATION, AND TRANSFORMATIONS AROUND THE ANTARCTIC MARGINS IV ORAL
high latitude environments | 21 february 2024
Christina Schmidt, Adele K. Morrison, Matthew H. E...
Antarctic Bottom Water (AABW) is a major component of the global overturning circulation, originating around the Antarctic continental margin. In rece...
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