Tropical mesoscale convective systems (MCSs) were identified from satellite
data using the 85-GHz ice-scattering channel for a La Nina year, and these
MCSs were compared with MCSs identified in the same manner for an El Nino
year in previous work by Mohr and Zipser. The number size, and intensity of
the MCSs were examined for differences between the years in 18 different r
egions. There are well-documented patterns of anomalous precipitation relat
ed to Ef Nino and La Nina, and, in general, the MCS distributions between t
he two years tend to follow these patterns. There were more MCSs in the cen
tral Pacific and eastern Pacific in the El Nino year than in the La Nina ye
ar, and there were fewer MCSs in the "Maritime Continent." The area distrib
utions and median intensities of MCSs were found to be similar in each regi
on during the two years. In contrast, the number and total area of MCSs in
a region changed between the years. The changes between the years in MCS di
stributions showed a strong relationship to differences in an independent e
stimate of rainfall for the two years.