eCite Digital Repository

What causes the spread of model projections of ocean dynamic sea-level change in response to greenhouse gas forcing?

Citation

Couldrey, MP and Gregory, JM and Boeira Dias, F and Dobrohotoff, P and Domingues, CM and Garuba, O and Griffies, SM and Haak, H and Hu, A and Ishii, M and Jungclaus, J and Kohl, A and Marsland, SJ and Ojha, S and Saenko, OA and Savita, A and Shao, A and Stammer, D and Suzuki, T and Todd, A and Zanna, L, What causes the spread of model projections of ocean dynamic sea-level change in response to greenhouse gas forcing?, Climate Dynamics, 56, (1-2) pp. 155-187. ISSN 0930-7575 (2020) [Refereed Article]


Preview
PDF
Pending copyright assessment - Request a copy
7Mb
  

DOI: doi:10.1007/s00382-020-05471-4

Abstract

Sea levels of different atmosphere–ocean general circulation models (AOGCMs) respond to climate change forcing in different ways, representing a crucial uncertainty in climate change research. We isolate the role of the ocean dynamics in setting the spatial pattern of dynamic sea-level (ζ) change by forcing several AOGCMs with prescribed identical heat, momentum (wind) and freshwater flux perturbations. This method produces a ζ projection spread comparable in magnitude to the spread that results from greenhouse gas forcing, indicating that the differences in ocean model formulation are the cause, rather than diversity in surface flux change. The heat flux change drives most of the global pattern of ζ change, while the momentum and water flux changes cause locally confined features. North Atlantic heat uptake causes large temperature and salinity driven density changes, altering local ocean transport and ζ. The spread between AOGCMs here is caused largely by differences in their regional transport adjustment, which redistributes heat that was already in the ocean prior to perturbation. The geographic details of the ζ change in the North Atlantic are diverse across models, but the underlying dynamic change is similar. In contrast, the heat absorbed by the Southern Ocean does not strongly alter the vertically coherent circulation. The Arctic ζ change is dissimilar across models, owing to differences in passive heat uptake and circulation change. Only the Arctic is strongly affected by nonlinear interactions between the three air-sea flux changes, and these are model specific.

Item Details

Item Type:Refereed Article
Keywords:sea-level rise, ocean heat uptake, climate change, climate modeling
Research Division:Earth Sciences
Research Group:Climate change science
Research Field:Climate change processes
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Understanding climate change
Objective Field:Climate change models
UTAS Author:Boeira Dias, F (Mr Fabio Boeira Dias)
UTAS Author:Dobrohotoff, P (Dr Peter Dobrohotoff)
UTAS Author:Domingues, CM (Dr Catia Domingues)
UTAS Author:Marsland, SJ (Mr Simon Marsland)
UTAS Author:Savita, A (Mr Abhishek Savita)
ID Code:143558
Year Published:2020
Deposited By:Oceans and Cryosphere
Deposited On:2021-03-24
Last Modified:2021-04-28
Downloads:0

Repository Staff Only: item control page