From climate drivers to Antarctic ice sheet response: Improving accuracy in sea level rise projections

From climate drivers to Antarctic ice sheet response: Improving accuracy in sea level rise projections

From climate drivers to Antarctic ice sheet response: Improving accuracy in sea level rise projections 700 467 Ocean Decade

Lead institution:

Akvaplan-niva – Norway

The Antarctic Ice Sheet (AIS) stores a large amount of freshwater. If melted completely, it would contribute 58 m to global mean sea level rise. According to IPCC AR6, a rise of up to 5 m by 2150 cannot be ruled out under a highemission scenario due to the large uncertainty related to AIS processes. Such a strong increase in sea level would be catastrophic for many low-lying regions worldwide, but how likely is it?

The AIS gains mass mainly through snow accumulation and loses mass through iceberg calving and ocean-induced basal melting of its floating parts. Future projections of AIS mass balance are based on ice sheet model simulations forced by climate model outputs. Climate models can properly project large-scale climate changes but struggle to represent small-scale coastal processes that bring heat to the ice sheet margins. This leads to poor representation of basal melting and thus substantial uncertainties in projections of Antarctica’s contribution to sea level rise. Climate models also suggest compensating mass change under climate warming in Dronning Maud Land: increased basal melting and more snowfall.

This project brings together glaciology and oceanography, sophisticated numerical modelling and statistical analysis techniques to address these two key uncertainties of sea level rise projections:

  1. Our combined approach of ocean model downscaling and statistical emulation enables us to assess future ocean induced AIS mass loss more accurately and thus reduce uncertainties in its contribution to sea level rise
  2. Our regional fine-resolution coupled ice sheet-ocean model enables us to provide improved projections for ice mass balance and ice sheet movement in the Norwegian administrated Dronning Maud Land sector of Antarctica

Our project outcomes will directly contribute to future assessments of ice sheet sea-level contributions and address two of the goals of the Ocean Decade: a predicted ocean and an accessible ocean.

Start Date: 01/01/2024
End Date: 31/12/2027

Lead Contact: Qin Zhou (qin@akvaplan.niva.no)

challenges:
5- Ocean-climate nexus
7- Ocean observations
8- Digital representation of the ocean
type_of_action:
Project

THE OCEAN DECADE

The Science We Need for the Ocean We Want

GET IN TOUCH

NEXT EVENTS

SUBSCRIBE TO OUR NEWSLETTER

OPPORTUNITIES

Join #OceanDecade

Privacy Preferences

When you visit our website, it may store information through your browser from specific services, usually in the form of cookies. Here you can change your Privacy preferences. It is worth noting that blocking some types of cookies may impact your experience on our website and the services we are able to offer.

For performance and security reasons we use Cloudflare
required

Enable/disable Google Analytics tracking code in browser

Enable / disable the use of Google fonts in the browser

Enable/disable embed videos in browser

Privacy policy

Our website uses cookies, mainly from 3rd party services. Define your Privacy Preferences and/or agree to our use of cookies.