Atmospheric Waves and
Climate Change
Professor Bob Vincent
Abstract
It is
sometimes said that one does not need to go to another planet to study a
different atmosphere. The Earth’s southern hemisphere can be thought of as the
“ocean” planet while the northern hemisphere as the
“land” planet. This land-ocean difference manifests itself in the formation of
an ozone hole in the southern hemisphere but not in the northern hemisphere. It
leads to significant differences in the generation of atmospheric waves, such
as planetary waves and gravity (buoyancy) waves that efficiently transfer
energy and momentum between the lower and upper atmosphere. As climate responds
to rising levels of greenhouse gases there will be changes in wave propagation
and these changes need to be properly incorporated into climate models.
Satellites
are often used to study planetary-scale waves, but investigations of
smaller-scale gravity wave activity on a global basis are more difficult. In
the spring of 2005 a major study of atmospheric gravity waves took place in the
Antarctic lower stratosphere. The Vorcore campaign
used super pressure balloons that float at heights near 18 km for periods of up
to several months. It provides a unique view of gravity wave processes at high
latitudes in the southern hemisphere. In this presentation the way the
atmosphere works is discussed in general terms and results from Vorcore are presented.
Speaker Profile
Bob Vincent obtained his Ph D at the
Professor Vincent is a Fellow of the Australian Academy of
Science since 2004.