FUNDING IS AVAILABLE FOR BOTH POSTDOCTORAL AND GRADUATE
(MSc/PhD) POSITIONS

If you are interested in applying, or want further information, contact
Glenn Milne (
gamilne@uottawa.ca).


Postdoctoral


The group is seeking a postdoctoral researcher with expertise in numerical modelling
applied to geophysical problems. Researchers with experience in one of the
following areas are particularly encouraged to apply: landscape evolution,
ice sheets (past and/or present), ocean dynamics, lithospheric deformation.
Some experience using a high-performance computer
cluster is preferred but
not essential.
 


MSc/PhD


If you have a degree in a quantitative physical science and are interested in the
type of research we do (see Research) then get in touch. People with degrees
in geophysics, physics, applied mathematics and computer science are
encouraged to apply. Here are some projects that would provide a good focus
for an MSc and/or a PhD project.

Sea-level change and land motion in the Mississippi Delta region

The primary aim of this project is to identify and quantify the processes that have
contributed to sea-level change in this region over the past millennia to decades.
A host of observations will be employed, including sea-level, GPS and sediment
compaction to constrain and develop models of the key processes. A major
deliverable of the research is improved estimates of background (secular) sea-level
change in this region over the coming centuries. This work is in collaboration
with
Prof. Tor Tornqvist's group  at Tulane University in New Orleans. For more
information click here.


Constraining the sources of rapid ice melting during the most recent deglaciation

This follows on from previous work (click here). The main focus of the
project will involve using an expanded data base and newly developed 3-D Earth
models to constrain the source distribution of melt water during the most recent
deglaciation. The events at ~19 kyr BP and ~14 kyr BP (Meltwater Pulse IA) will
be the focus of the project. Improving constraints on the source geometry of these
events is the first step towards understanding the forcings and mechanisms
responsible for their occurrence. This understanding will underpin our ability to
determine the possibility of such rapid sea-level events occurring in the future.


Constraining 3-D Earth structure beneath the Canadian Shield

The primary goal of this project is to consider the question: can observations of
present-day land motion, gravity changes and past sea-level changes be used to
infer useful information about the 3-D Earth structure beneath and adjacent to the
Canadian Shield? Conventional studies have inverted these types of data to infer
only variations in viscosity with depth (as described
here). With the recent
development of 3-D isostatic Earth models and the increasing amount geodetic
data with good spatial coverage (GPS and satellite gravity), it is important to consider
the possibility of obtaining useful constraints on lateral variations in lithospheric
thickness and viscosity structure.


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