by ZAMG, FMI and IM
There are many definitions of MCS in literature. One frequently used definition is: A deep convective system which is considerably larger than an individual thunderstorm; it is often marked by an extensive middle-to-upper tropospheric stratiform anvil cloud several hundred kilometres wide. One special case of MCS is the so-called MCC (Mesoscale Convective Complex), which is a huge quasi-circular MCS that lasts about 10 hours. MCCs are frequent in many parts of the world as the US, South America, Africa, Western Pacific and India, but are relatively rare in Europe, where only an average of around 5 MCC form every warm season. In the chapters discussing convective weather features, conceptual models of two different scales will be studied: