Journal of the Royal Society of New Zealand abstracts
A.P. Sturman*, P. D. Tyson+, and P. C.
D'Abreton+
Kinematic trajectory modelling is used in a preliminary examination of
inter-regional transport of air within the Southern Hemisphere. In particular,
the westerly zonal transport of air in the lower troposphere from southern
Africa and Australia to New Zealand is determined for January and July, using
both forward and backward trajectories originating or ending up in the 850-800
hPa layer respectively. Mean transport plumes are derived from swarms of
individual trajectories, and the results show that in winter around 22% of air
originating over the central interior of South Africa reaches the central
Tasman Sea south of New Zealand. In summer the amount is insignificant owing to
seasonal changes in the position of major circulation features. In contrast,
both summer and winter low-level air transport from southeastern and
southwestern Australia and adjacent oceans to New Zealand is substantial, with
83% of all low-level air parcels from the Sydney area in summer passing over
central New Zealand 5 days later. In winter the transport plume passes over the
northern part of the North Island within 3 days. Back trajectories show that in
some seasons two distinct paths are followed by air arriving at Christchurch
and Auckland, from the west-northwest and southwest. Analysis of the vertical
structure of the transport plumes arriving in New Zealand shows that the
westerly air reaching Auckland in the 850-800 hPa layer does so in a subsiding
airstream throughout the year, whereas that arriving in the same layer over
Christchurch experiences only minor subsidence en route from Australia and the
ocean to the south. This descending motion is related to the dominance of
anticyclonic circulation, particularly over the northern section of the New
Zealand region.
Keywords: Trajectory analysis, atmospheric circulation, air movement, New
Zealand, Africa, Australia
(c) Journal of The Royal Society of New Zealand,
Volume 27, Number 4, December 1997, pp 485-498
PDF file of entire paper: medium quality (1009K); (scanned from paper original: notes about this process)
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