Mark England
0000-0003-3882-872X
University of Granada
13 papers found
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Are Multi‐Decadal Fluctuations in Arctic and Antarctic Surface Temperatures a Forced Response to Anthropogenic Emissions or Part of Internal Climate Variability?
Modeling the breakup of tabular icebergs
Distinguishing the impacts of ozone and ozone-depleting substances on the recent increase in Antarctic surface mass balance
Robust Arctic warming caused by projected Antarctic sea ice loss
Tropical climate responses to projected Arctic and Antarctic sea-ice loss
Addendum: Substantial twentieth-century Arctic warming caused by ozone-depleting substances
Substantial twentieth-century Arctic warming caused by ozone-depleting substances
Nonuniform Contribution of Internal Variability to Recent Arctic Sea Ice Loss
Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate
The Role of Internal Variability in Twenty‐First‐Century Projections of the Seasonal Cycle of Northern Hemisphere Surface Temperature
Contrasting the Antarctic and Arctic Atmospheric Responses to Projected Sea Ice Loss in the Late Twenty-First Century
Robust response of the Amundsen Sea Low to stratospheric ozone depletion
Troposphere‐stratosphere dynamical coupling in the southern high latitudes and its linkage to the Amundsen Sea
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