OS003-0010
Multi-model ensemble projections of sea-level using the Ice-Sheet and Sea-Level System Model probabilisticframework and CMIP5/CMIP6 outputs.

Monday, 7 December 2020
Poster
Eric Y Larour1, Nicole Schlegel2, Surendra Adhikari3, Erik Roman Ivins4, Lambert Caron5, Thomas Frederikse1 and Mathieu Morlighem6, (1)NASA Jet Propulsion Laboratory, Pasadena, CA, United States, (2)NASA Jet Propulsion Laboratory, Pasadena, United States, (3)California Institute of Technology, Jet Propulsion Laboratory, Pasadena, CA, United States, (4)JPL/Caltech, Pasadena, CA, United States, (5)Jet Propulsion Laboratory, Pasadena, CA, United States, (6)University of California - Irvine, Irvine, CA, United States
Abstract:
There is currently a strong need to update probabilistic sea-level projections to adopt the new
simulation outputs from CMIP6. There is indeed a large multi-model ensemble that can be used towards
better constraining the uncertainty in 21st century projections, in particular as it relates
to dynamic and thermo-steric sea-level change. In addition, multiple MIP (Modeling Inter-comparison
Projects) have propagated CMIP5/CMIP6 results in areas required to understand the barystatic components
of sea-level change, in particular GlacierMIP2 for glaciers and ISMIP6 for polar ice sheets. Here we
present a massive high-spatial and temporal resolution multi-model ensemble analysis of sea-level change
patterns over the 21st century that combines dynamic and thermo-steric sea-level from CMIP5/6 with
barystatic signals from ISMIP6, GlacierMIP2 and GIA statistics. We rely on the ISSM (Ice-Sheet
and Sea-Level System Model) probabilistic SLPS (Sea-Level Projection System) to compute .3 degree lat/long
sea-level change fingerprints at yearly time scales to provide sea-level statistics for the whole
world for the entire 21st century. We quantify the impact of our approach against more classical approaches
that do not rely on a MME approach or on comprehensive sea-level fingerprinting that is coherent both
in time and space.

This work was performed at the California Institute of Technology's Jet Propulsion Laboratory under a contract with
the National Aeronautics and Space Administration's Cryosphere Science Program.