The performance of three automatic depression tracking schemes developed by
Terry & Atlas (1996), Murray C Simmonds (1991a) and Konig et al. (1993) wh
en applied! over one month are assessed. The schemes respectively identify
depressions by (a) locating the innermost closed contour in a PMSL field (b
) finding maximal in the curvature in a bi-cubic Spline fitted to the PMSL
data and (c) performing a gridpoint search to identify a minimum in a PMSL
field The largest number of depressions was found by the Murray and Simmond
s scheme, with the Atlas and Terry scheme finding the least. The Murray and
Simmonds scheme also found the largest number of tracks, with the other tw
o having comparable numbers of tracks. Two possible explanations for the di
fferences in the number of tracks are considered. Firstly, the cdse where o
ne or more centres identified by one scheme as corresponding to a single tr
ack are not found by the other schemes. Secondly, the cdse where a Single t
rack found by one scheme is split into two or more tracks by the other sche
mes. All three techniques had a similar latitude of cyclogenesis, although
the Atlas and Terry and Konig et al. schemes found more lows dt high latitu
des as a result of using data On a latitude/longitude grid. The longest mea
n track length was found with the Konig et al. scheme. A comparison of the
PMSL fields with satellite imagery shows that the major NWP centres have tr
ouble producing reliable analyses around the Antarctic because of the lack
of data.