Tropical Cyclone Drena, a relatively long lived cyclone lasting from J
anuary 2, 1997 to January 10, 1997, crossed over three well separated
island groups and affected a fourth in the south western Pacific Ocean
during different stages of its life cycle. Midway through its transit
ion into an extra-tropical low, it passed over the eastern edge of Nor
folk Island, an isolated island located in the western Pacific Ocean m
idway between New Zealand and New Caledonia, at 0615 UTC (1745 local)
on January 9, 1997. The tropical cyclone exhibited markedly different
characteristics during each phase of its life cycle, with thick fog be
ing reported during the eye passage at Norfolk Island. Although routin
e global and Australian region numerical models were able to provide t
he operational forecasters with broad scale guidance as to the movemen
t of the tropical cyclone, the level of detail available at these reso
lutions is insufficient to identify the characteristics important to c
ommunities in the tropical cyclone's path. The high resolution numeric
al model (HIRES) developed by the University of New South Wales, was r
un at a resolution of 25 kilometres to investigate the evolution of th
e tropical cyclone from a warm cored, quasi-symmetrical vortex into a
highly asymmetrical mid latitude low pressure system. The model captur
es the observed wind and precipitation structure of the cyclone very w
ell during this crucial transition phase. The comparison extends into
the vertical with a model derived vertical cross section depicting the
key features observed in a sequence of ten specially requested radios
onde flights, released at six hourly intervals, from Norfolk Island wh
ich transect the passage of the tropical cyclone over this remote isla
nd.