Callaghan and Bonell introduce the main features of the tropical atmospheric circulation as a step towards linking different synoptic-scale, rain-producing phenomena, their associated rainfall characteristics and the subsequent impacts on runoff hydrology.
Sonja GermerChristopher NeillAlex V. KruscheHelmut Elsenbeer
Boris RewaldPanagiotis MichopoulosLise DalsgaardDavey L. JonesDouglas L. Godbold
Shengping WangZhiqiang ZhangGe SunSteven G. McnultyManliang Zhang