226
P. Maheras and C. Anagnostopoulou
C w The negative anomaly centre is usually located far to the west of Greece in the
western Mediterranean, western Europe or north Africa (Fig. 16h).
I'
' .,
; ' \ ,~
I "
Fig. 15. Anticyclonic types: Mean winter anomalies (x I 00) calculated from 500 hPa level field data,
1958-1997. Figures run from (a) top left to (f) bottom right
P. Maheras and C. Anagnostopoulou
C w The negative anomaly centre is usually located far to the west of Greece in the
western Mediterranean, western Europe or north Africa (Fig. 16h).
I'
' .,
; ' \ ,~
I "
Fig. 15. Anticyclonic types: Mean winter anomalies (x I 00) calculated from 500 hPa level field data,
1958-1997. Figures run from (a) top left to (f) bottom right