
Regional Sea Level Changes Projected by the NASA/GISS
Atmosphere-Ocean Model
Gary L. Russell, Vivien Gornitz, and James R. Miller
2000: Climate Dynamics, 16 (10-11), 789-797
Abstract
Sea level has been rising for the past century, and
inhabitants of the Earth's coastal regions will want to
understand and predict future sea level changes. In this study
we present results from new simulations of the Goddard Institute
for Space Studies (GISS) global atmosphere-ocean model from 1950
to 2099. Model results are compared with observed sea level
changes during the past 40 years at 17 coastal stations around
the world. Using observed levels of greenhouse gases between
1950 and 1990 and a compounded 0.5% annual increase in CO2 after
1990, model projections show that global sea level measured from
1950 will rise by 61 mm in the year 2000, by 212 mm in 2050, and
by 408 mm in 2089. By 2089, two thirds of the global sea level
rise will be due to thermal expansion and one third will be due
to ocean mass changes. The spatial distribution of sea level rise
is different than that projected by rigid lid ocean models.
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