Large, long-lived mesoscale convective systems (MCSs) over the United State
s during the 1997-98 El Nino are documented. Two periods of abnormal MCS ac
tivity are identified in 1998: from March to mid-April an unusually large n
umber of quasi-linear MCSs were observed in the Midwest; while quasi-circul
ar MCSs in June-August of 1998 were concentrated near 37 degreesN rather th
an following a seasonal shift similar to that observed in the climatologica
l distribution. Episodic surges of northerly low-level flow were infrequent
in March 1998, thereby leading to an unusually high incidence of quasi-lin
ear MCSs and to precipitation anomalies in the central United States.