Hoffmann, Janosch Fabian
Description
In the last two decades, satellite altimetry has given
the scientific community an unprecedented amount of data, which
has substantially increased our understanding of the rate of
change of ice surface height (dH/dt) over glaciated regions. This
can be attributed to better spatial and temporal coverage of
polar regions and the increased accuracy of laser and radar
satellite altimeters. This accuracy is dependent on minimising
errors and reducing the...[Show more] uncertainties of estimates of dH/dt,
which are derived from ice height measurements. There are a
number of different factors that contribute to the overall
uncertainty budget. In this thesis, an alternative method to
crossover and along-track analysis is proposed and is applied to
(ICESat) height measurements. A new method of estimating surface
slope at crossovers is presented and used in conjunction with the
newly proposed along-track method. Particular emphasis is placed
on the formal propagation of interpolation uncertainty and
surface topography bias, which is often given little attention in
the literature. The proposed methods are tested using a number of
simulated datasets for Enderby Land and surrounds in Antarctica.
The simulated datasets are derived from ICESat data, with
different levels of spatially correlated noise applied to each,
dependent on regionally specific ice velocities. Both the error
(the difference between simulated and estimated dH/dt) and the
uncertainty (a function of the interpolation distance and surface
slope) are derived. It was found that the formally propagated
uncertainty made a good approximation of the error and both the
crossover and along-track methods were found to have the lowest
uncertainty and error when using Green's function spline
interpolation. The errors and uncertainties due to interpolation
were an order of magnitude smaller than those obtained from the
slope correction method. The overall uncertainty was found to be
approximately 50% of the ICESat single-shot uncertainty budget,
showing the relative importance of including these
often-overlooked contributors in the final uncertainty budget of
ice height rate estimates from altimetry data. The proposed
methods were then applied to actual ICESat data over part of East
Antarctica, including Enderby, Kemp, MacRobertson and part of
Dronning Maud Lands. The dH/dt results for the study site
generally showed an increase in the rate of change of ice surface
height. Although most of the study site was gaining height, there
were some regions with negative dH/dt estimates, such as directly
behind the grounding line of the Amery Ice Shelf. These negative
rates tend to have little impact on the overall estimates of
dH/dt, as they are localised to very small regions. The positive
rate of height change in the interior was found to be
statistically significant, especially near Dronning Maud Land.
The uncertainties calculated for this study do not include the
ICESat single-shot uncertainty budget, as the focus of the study
was the uncertainty contributions of interpolation and surface
slope bias. The combination of these uncertainties would decrease
the significance of the inland signal, however the large number
of positive dH/dt estimates found in the interior does suggest
that the ice height surface is increasing for this region,
implying a positive mass balance change may be occurring in the
interior of East Antarctica.
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