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UNSW02: STRATOSPHERIC INFLUENCE ON EDDY DRIVEN JET POSITION

August 6, 2020 1:20 pm Published by Comments Off on UNSW02: STRATOSPHERIC INFLUENCE ON EDDY DRIVEN JET POSITION

This project proposes a process-based approach to tackling the question of how the stratosphere and the troposphere are coupled. By employing a hierarchy of circulation models, it will put several basic mechanisms to the test.

ANU03: Understanding ocean heat transport to the Antarctic continental shelf

August 6, 2020 1:17 pm Published by Comments Off on ANU03: Understanding ocean heat transport to the Antarctic continental shelf

This project investigates access pathways of the relatively warm water to the continental shelf by analysing output from a coupled ocean – sea ice model. The student will gain experience in polar oceanography and in the analysis and visualisation of large numerical datasets using python.

UTas01: Understanding polar stratospheric cloud interactions

July 20, 2019 1:00 am Published by Comments Off on UTas01: Understanding polar stratospheric cloud interactions

In this project, you will use unique data collected during the Antarctic winter to understand the interactions between PSCs, the tropopause, and very cold cirrus clouds which are present in the upper troposphere. You will also determine how small-scale changes in stratospheric winds influence the occurrence, composition and brightness of PSCs.

UNSW12: How well can we reconstruct past ocean circulation?

July 19, 2019 12:00 pm Published by Comments Off on UNSW12: How well can we reconstruct past ocean circulation?

There is compelling evidence that under different climate states (e.g. glacial-interglacial cycles), the Atlantic Ocean has experienced significant water mass reorganisations and circulation changes. This project aims to better constrain these variations, using models able to simulate proxy variations.

UNSW11: Understanding Marine Heatwaves

July 19, 2019 11:00 am Published by Comments Off on UNSW11: Understanding Marine Heatwaves

In this project we will look at one of the two following questions: Do marine heatwaves occur preferentially in certain seasons, and if so why? Do marine heatwaves produce a consistent response in ocean primary production?