The role of the Southern Ocean in sea-level change
Project leader: Dr Xuebin Zhang (CSIRO)
Staff, students and associates: Prof Xianyao Chen (OUC); Prof John Church (UNSW); Prof Mat King (UTAS); Dr Yuehua (Veronica) Li (UNSW); Dr Kewei Lyu (CSIRO); Dr Steven Phipps (UTAS); Dr Christopher Watson (UTAS); Miss Jinping Wang (Ocean University of China PhD Student); Mr Jingwei Zhang (UTAS PhD Student).
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Xuebin Zhang: This project is going to address some scientific questions related to the sea level change such as the ocean heat uptake and redistribution in the Southern Ocean, and the contribution of the Antarctic ice sheet to the sea level change
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and regional distribution of sea level and associated underlying dynamic process in the Southern Ocean.
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Oh yeah, it’s a very important question to understand the sea level rise because in the past like two or three decades the research community already made very good progress in understanding and project in sea level changes but a significant gap still exists and the decision maker and the end user, they want much better information than what we can deliver right now.
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The Southern Ocean is one of the few key areas where the heat is up, particularly in the ocean, and secondly warming in the Southern Ocean is critical for the dynamic response of the Antarctic ice sheet.
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I hope through this project we can achieve better understanding and the projecting of the sea level rise, so this information can be used for better mitigation and habitation planning for sea level rise.
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Dr Xuebin Zhang introduces the Southern Ocean sea level change project
Reconciling global mean and regional sea level change in projections and observations
15 February 2021
A study led by Ocean University of China and CSHOR student, Jinping Wang, and published in Nature Communications, finds climate model projections of sea level rise in the early 21st century are in good agreement with sea level data recorded in the corresponding period. Read more at this link.
Prof John Church Elected to the AGU Fellows Class of 2020
18 November 2020
Prof John Church was elected to the AGU Fellows Class of 2020 for his exceptional contribution to the American Geophysical Union’s (AGU’s) Earth and space sciences community. Dr Church is a Professor at UNSW’s Climate Change Research Centre (CCRC), and collaborates with CSHOR’s Southern Ocean and sea-level change.
Sea-level rise is an important climate change research topic. Global mean sea level (GMSL) has been rising according to tide gauge and satellite altimetry observations, and is projected to continue to rise, with a likely range between 0.28 m and 0.98 m by 2100. A larger rise could occur if there is a significantly larger contribution from changes in Antarctic dynamics. Over 100 million people live within a metre of current high tide mark, thus are highly likely to be affected by sea-level rise. Several processes can affect GMSL, including ocean thermal expansion, mass loss of glaciers and ice caps, the Antarctic Ice Sheet and the Greenland Ice Sheet, and changes in the land-water storage.
The Southern Ocean is a key area for improving projections of ocean heat content and sea-level change because: it is one of the key areas where heat enters the ocean, resulting in heat storage in the upper ocean and in the abyssal layers, and contributing to ocean thermal expansion; and a warming ocean is critical to the dynamic response of the Antarctic ice sheet.
Key objectives of the project are to:
- Quantify the amount of heat entering the Southern Ocean and associated sea-level change.
- Separate the impact of wind-induced vs Antarctic freshwater-induced ocean responses, and natural versus anthropogenic forcing in sea level and ocean dynamics in the SO;
- Examine the robustness of the dipole structure of sea-level change (centred at ~50oS) in coarse resolution models to the impacts of meso-scale eddies by comparing coarse-resolution and eddy-resolving model results, and analyse whether there are distinct responses to strengthening vs shifting of westerly winds.
- Refine sea-level projections based on updated observations and projections of the Antarctica Ice Sheet contribution, together with other sea level contributions.
To achieve above objectives, we will use available observations, Climate Model Intercomparison Project (CMIP) models, and an eddy-resolving (1/10o) global ocean model. For the projection of Ice Sheet contribution, we will use either stand-alone or coupled ice sheet modelling from the Ice Sheet Model Intercomparison for CMIP6.
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