Mark Collier
Mark Collier
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Cited by
Cited by
The CSIRO Mk3 climate system model
HB Gordon, LD Rotstayn, JL McGregor, MR Dix, EA Kowalczyk, ...
CSIRO Atmospheric Research technical paper 60, 130, 2002
The ACCESS coupled model: description, control climate and evaluation
D Bi, M Dix, S Marsland, S O'Farrell, H Rashid, P Uotila, A Hirst, ...
Australian Meteorological and Oceanographic Journal 63 (1), 41-64, 2013
Aerosol-and greenhouse gas-induced changes in summer rainfall and circulation in the Australasian region: a study using single-forcing climate simulations
LD Rotstayn, SJ Jeffrey, MA Collier, SM Dravitzki, AC Hirst, JI Syktus, ...
Atmospheric Chemistry and Physics 12 (14), 6377-6404, 2012
Biotic and human vulnerability to projected changes in ocean biogeochemistry over the 21st century
C Mora, CL Wei, A Rollo, T Amaro, AR Baco, D Billett, L Bopp, Q Chen, ...
PLoS Biology 11 (10), e1001682, 2013
Improved simulation of Australian climate and ENSO‐related rainfall variability in a global climate model with an interactive aerosol treatment
LD Rotstayn, MA Collier, MR Dix, Y Feng, HB Gordon, SP O'Farrell, ...
International Journal of Climatology: A Journal of the Royal Meteorological …, 2010
Australia’s CMIP5 submission usingthe CSIRO-Mk3. 6 model
S Jeffrey, L Rotstayn, M Collier, S Dravitzki, C Hamalainen, ...
Australian Meteorological and Oceanographic Journal 63 (1), 1-13, 2013
The CSIRO Mk3. 5 climate model
HB Gordon, S O'Farrell, M Collier, M Dix, L Rotstayn, E Kowalczyk, T Hirst, ...
CSIRO and Bureau of Meteorology, 2010
The CSIRO-Mk3. 6.0 Atmosphere-Ocean GCM: participation in CMIP5 and data publication
MA Collier, SJ Jeffrey, LD Rotstayn, KK Wong, SM Dravitzki, C Moseneder, ...
International congress on modelling and simulation–MODSIM, 2691-2697, 2011
The ACCESS coupled model: documentation of core CMIP5 simulations and initial results
M Dix, P Vohralik, D Bi, H Rashid, S Marsland, S O'Farrell, P Uotila, T Hirst, ...
Australian Meteorological and Oceanographic Journal 63 (1), 83-99, 2013
Plex: Towards reliability using pretrained large model extensions
D Tran, J Liu, MW Dusenberry, D Phan, M Collier, J Ren, K Han, Z Wang, ...
arXiv preprint arXiv:2207.07411, 2022
Projected effects of declining aerosols in RCP4. 5: unmasking global warming?
LD Rotstayn, MA Collier, A Chrastansky, SJ Jeffrey, JJ Luo
Atmospheric Chemistry and Physics 13 (21), 10883-10905, 2013
Implementing neural turing machines
M Collier, J Beel
Artificial Neural Networks and Machine Learning–ICANN 2018: 27th …, 2018
Comparison of observed and multimodeled trends in annual extremes of temperature and precipitation
D Kiktev, J Caesar, LV Alexander, H Shiogama, M Collier
Geophysical Research Letters 34 (10), 2007
Climate models without preindustrial volcanic forcing underestimate historical ocean thermal expansion
JM Gregory, D Bi, MA Collier, MR Dix, AC Hirst, A Hu, M Huber, R Knutti, ...
Geophysical Research Letters 40 (8), 1600-1604, 2013
The CSIRO Mk3 Climate System Model, Technical Paper No. 60
HB Gordon, LD Rotstayn, JL McGregor, MR Dix, EA Kowalczyk, ...
CSIRO Atmospheric Research, Aspendale, Victoria, Australia, 2002
WMO global annual to decadal climate update: a prediction for 2021–25
L Hermanson, D Smith, M Seabrook, R Bilbao, F Doblas-Reyes, ...
Bulletin of the American Meteorological Society 103 (4), E1117-E1129, 2022
Why does aerosol forcing control historical global-mean surface temperature change in CMIP5 models?
LD Rotstayn, MA Collier, DT Shindell, O Boucher
Journal of Climate 28 (17), 6608-6625, 2015
Sigma-coordinate calculation of topographically forced baroclinicity around Antarctica
KJE Walsh, I Simmonds, M Collier
Dynamics of atmospheres and oceans 33 (1), 1-29, 2000
Simulated enhancement of ENSO-related rainfall variability due to Australian dust
LD Rotstayn, MA Collier, RM Mitchell, Y Qin, SK Campbell, SM Dravitzki
Atmospheric Chemistry and Physics 11 (13), 6575-6592, 2011
CMIP5 datasets from the ACCESS1. 0 and ACCESS1. 3 coupled climate models
M Collier, P Uhe
Centre for Australian weather and Climate Research, 2012
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Articles 1–20