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Dynamic meteorology

A comparison of two identification and tracking methods for polar lows

, , , &
Article: 17196 | Received 29 Jun 2011, Accepted 02 Jan 2012, Published online: 08 Feb 2012

Figures & data

Fig. 1.  Unfiltered MSLP field on 06:00 14 October 1993 (hPa).

Fig. 2.  NOAA 11/AVHRR channel 4 thermal infrared for 1529 UTC 14 October 1993 (from www.sat.dundee.ac.uk/).

Fig. 3.  Bandpass filtered MSLP fields on 06:00 14 October 1993 (hPa): (a) digital filter, (b) DCT, and detected minima: red by KH and green by MZ.

Fig. 4.  Bandpass filtered 850 hPa relative vorticity fields on 06:00 14 October 1993 (10−5 s−1): (a) digital filter and (b) DCT.

Table 1. Numbers of tracks resulting from different combinations between MZ and KH (October 1993 to September 1995)

Fig. 5.  Overlapping tracks in October 1993 for combination 5 (blue) and combination 7 (red) of .

Table 2. Number N o of overlapping tracks, probability P o for overlapping tracks and ratio P m of non-overlapping tracks for different combinations in using combination 1 as a reference

Table 3. Number N o of overlapping tracks, probability P o for overlapping tracks and ratio P m of non-overlapping tracks for different combinations in using combination 7 as a reference

Table 4. Numbers of retained potential polar lows after applying the respective criteria in Section 2.4 in October 1993 to September 1995

Fig. 6.  Tracks of potential polar lows after applying criteria to combination 1 (red with points) of KH and combination 7 of MZ in October 1993 (blue).