Time evolution of a deep anticyclone and a steep meander crest. Observe:
The rapid eastward propagation through the region (in contrast to the cyclone/steep trough event).
TITLE PAGE
ABSTRACT
DATA SOURCES
LEVELING AND MAPPING
MEAN FIELDS
DEEP CYCLONES
DEEP ANTICYCLONES
WARM CORE RINGS
TOPOGRAPHIC ROSSBY WAVES
SUMMARY
REFERENCES
FORUM