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Statistics on tropical convective storms observed by radar
(1996-10-01)
Convective storm rainfall is of special importance to urban hydrological studies due to its temporal and spatial variability. Although dense networks of recording rain gauges can be employed to characterize such rainfall, ...
Statistics on tropical convective storms observed by radar
(1996-10-01)
Convective storm rainfall is of special importance to urban hydrological studies due to its temporal and spatial variability. Although dense networks of recording rain gauges can be employed to characterize such rainfall, ...
Numerical simulation of the diurnal cycle of rainfall in SW Amazon basin during the 1999 rainy season: the role of convective trigger function
(Theoretical and Applied Climatology, 2012-02-07)
Using convective available potential energy (CAPE) and dew-point temperature to characterize rainfall-extreme events in the Southcentral Andes
(Molecular Diversity Preservation International, 2019-07-08)
The interactions between atmosphere and steep topography in the eastern south-central Andes result in complex relations with inhomogenous rainfall distributions. The atmospheric conditions leading to deep convection and ...
Diurnal cycle of raindrops size distribution in a valley of the Peruvian central andes
(MDPI, 2020)
In the Central Andes of Peru, convective and stratiform rainfall occurs, frequently associated with convective storms. The raindrop size distributions (RSD), measured by a Parsivel-2 optical disdrometer, were characterized ...
A Model for the Relationship between Rainfall, GNSS-Derived Integrated Water Vapour, and CAPE in the Eastern Central Andes
(Multidisciplinary Digital Publishing Institute, 2021-09)
Atmospheric water vapour content is a key variable that controls the development of deep convective storms and rainfall extremes over the central Andes. Direct measurements of water vapour are challenging; however, recent ...
Atmospheric circulation types controlling rainfall in the Central American Isthmus
(2022)
Rainfall mechanisms in the Central American Isthmus are controlled by complex
physical interactions across spatial and temporal scales, which are reflected on the
dynamics of atmospheric circulation patterns affecting ...