Theo dõi
Mark England
Mark England
Senior Research Fellow at University of Exeter, Royal Commission for the Exhibition of 1851 fellow
Email được xác minh tại exeter.ac.uk - Trang chủ
Tiêu đề
Trích dẫn bởi
Trích dẫn bởi
Năm
The recent emergence of Arctic amplification
MR England, I Eisenman, NJ Lutsko, TJW Wagner
Geophysical Research Letters 48 (15), e2021GL094086, 2021
1682021
Tropical climate responses to projected Arctic and Antarctic sea-ice loss
MR England, LM Polvani, L Sun, C Deser
Nature Geoscience 13 (4), 275-281, 2020
143*2020
Nonuniform contribution of internal variability to recent Arctic sea ice loss
M England, A Jahn, L Polvani
Journal of Climate 32 (13), 4039-4053, 2019
1182019
Substantial twentieth-century Arctic warming caused by ozone-depleting substances
LM Polvani, M Previdi, MR England, G Chiodo, KL Smith
Nature Climate Change 10 (2), 130-133, 2020
1022020
Contrasting the Antarctic and Arctic atmospheric responses to projected sea ice loss in the late twenty-first century
M England, L Polvani, L Sun
Journal of Climate 31 (16), 6353-6370, 2018
722018
Robust response of the Amundsen Sea Low to stratospheric ozone depletion
MR England, LM Polvani, KL Smith, L Landrum, MM Holland
Geophysical Research Letters 43 (15), 8207-8213, 2016
522016
Robust Arctic warming caused by projected Antarctic sea ice loss
MR England, LM Polvani, L Sun
Environmental Research Letters 15 (10), 104005, 2020
412020
Modeling the breakup of tabular icebergs
MR England, TJW Wagner, I Eisenman
Science advances 6 (51), eabd1273, 2020
362020
Back to the future: using long-term observational and paleo-proxy reconstructions to improve model projections of Antarctic climate
TJ Bracegirdle, F Colleoni, NJ Abram, NAN Bertler, DA Dixon, M England, ...
Geosciences 9 (6), 255, 2019
362019
Spurious climate impacts in coupled sea ice loss simulations
MR England, I Eisenman, TJW Wagner
Journal of Climate 35 (22), 3801-3811, 2022
232022
Are multi‐decadal fluctuations in Arctic and Antarctic surface temperatures a forced response to anthropogenic emissions or part of internal climate variability?
MR England
Geophysical Research Letters 48 (6), e2020GL090631, 2021
232021
Separating the influences of low-latitude warming and sea ice loss on Northern Hemisphere climate change
S Hay, PJ Kushner, R Blackport, KE McCusker, T Oudar, L Sun, ...
Journal of Climate 35 (8), 2327-2349, 2022
182022
Stronger Arctic amplification from ozone-depleting substances than from carbon dioxide
YC Liang, LM Polvani, M Previdi, KL Smith, MR England, G Chiodo
Environmental Research Letters 17 (2), 024010, 2022
182022
The role of internal variability in twenty‐first‐century projections of the seasonal cycle of Northern Hemisphere surface temperature
V Yettella, MR England
Journal of Geophysical Research: Atmospheres 123 (23), 13,149-13,167, 2018
172018
Troposphere‐stratosphere dynamical coupling in the southern high latitudes and its linkage to the Amundsen Sea
MR England, TA Shaw, LM Polvani
Journal of Geophysical Research: Atmospheres 121 (8), 3776-3789, 2016
142016
Distinguishing the impacts of ozone and ozone-depleting substances on the recent increase in Antarctic surface mass balance
R Chemke, M Previdi, MR England, LM Polvani
The Cryosphere 14 (11), 4135-4144, 2020
102020
The Montreal Protocol is delaying the occurrence of the first ice-free Arctic summer
MR England, LM Polvani
Proceedings of the National Academy of Sciences 120 (22), e2211432120, 2023
92023
Modeled interannual variability of Arctic sea ice cover is within observational uncertainty
C Wyburn-Powell, A Jahn, M R. England
Journal of Climate 35 (20), 6827-6842, 2022
8*2022
Robust anthropogenic signal identified in the seasonal cycle of tropospheric temperature
BD Santer, S Po-Chedley, N Feldl, JC Fyfe, Q Fu, S Solomon, M England, ...
Journal of Climate 35 (18), 6075-6100, 2022
82022
Large contribution of ozone‐depleting substances to global and Arctic warming in the late 20th century
M Sigmond, LM Polvani, JC Fyfe, CJ Smith, JNS Cole, MR England
Geophysical Research Letters 50 (5), e2022GL100563, 2023
62023
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