Convection along the Coast of Northern Peru during 1983: Spatial and Temporal Variation of Clouds and Rainfall

Abstract

Streamflow and historical records indicate that flooding in northern Peru was more severe during 1983 than during any year since 1891. A case study of the meteorological conditions along the northwest coast of South America from 10°S to 10°N during 1982–83 is presented. Station rainfall and satellite-derived outgoing infrared observations are used to deduce the structure and time evolution of convection in this region. Substantial rainfall amounts were first observed along the western slopes of the Andes Mountains and coastal plain of southern Ecuador during November and December 1982, and it continued to rain in this region through June 1983. In northern Peru, the onset of the rains along the coastal plain was delayed until January 1983 and ended abruptly during mid-June 1983. Convective activity was much greater along the coastal strip than over the eastern equatorial Pacific to the cast of 100°W until May-June 1983. In addition, cloudiness was strongly modulated on the diurnal time scale, with... Abstract Streamflow and historical records indicate that flooding in northern Peru was more severe during 1983 than during any year since 1891. A case study of the meteorological conditions along the northwest coast of South America from 10°S to 10°N during 1982–83 is presented. Station rainfall and satellite-derived outgoing infrared observations are used to deduce the structure and time evolution of convection in this region. Substantial rainfall amounts were first observed along the western slopes of the Andes Mountains and coastal plain of southern Ecuador during November and December 1982, and it continued to rain in this region through June 1983. In northern Peru, the onset of the rains along the coastal plain was delayed until January 1983 and ended abruptly during mid-June 1983. Convective activity was much greater along the coastal strip than over the eastern equatorial Pacific to the cast of 100°W until May-June 1983. In addition, cloudiness was strongly modulated on the diurnal time scale, with...