Modelling raindrop size distribution (DSD) is a fundamental issue to connect remote sensing observations with reliable precipitation products for hydrological applications. To date, various standard probability distributions have been proposed to build DSD models. Relevant questions to ask indeed are how often and how good such models fit empirical data, given that the advances in both data availability and technology used to estimate DSDs have allowed many of the deficiencies of early analyses to be mitigated. Therefore, we present a comprehensive follow-up of a previous study on the comparison of statistical fitting of three common DSD models against 2D-Video Distrometer (2DVD) data, which are unique in that the size of individual drops i...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Modelling raindrop size distribution (DSD) is a fundamental issue to connect remote sensing observat...
It is widely acknowledged that a thorough characterization of the raindrop size distribution (DSD) m...
It is widely acknowledged that a thorough characterization of the raindrop size distribution (DSD) m...
It is widely acknowledged that a thorough characterization of the raindrop size distribution (DSD) m...
The raindrop size distribution (DSD) is fundamental for quantitative precipitation estimation (QPE) ...
The adequacy of the gamma model to describe the variability of raindrop size distributions (DSD) is ...
The present study utilizes nine years of measurements taken from a Joss–Waldvogel disdrometer (JWD)....
International audienceThe gamma distribution is often used to characterize raindrop size distributio...
International audienceThe gamma distribution is often used to characterize raindrop size distributio...
International audienceThe gamma distribution is often used to characterize raindrop size distributio...
The main challenges of measuring precipitation are related to the spatio-temporal variability of the...
none3siThe NASA's Global Precipitation Measurement (GPM) mission dual-frequency precipitation radar ...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Modelling raindrop size distribution (DSD) is a fundamental issue to connect remote sensing observat...
It is widely acknowledged that a thorough characterization of the raindrop size distribution (DSD) m...
It is widely acknowledged that a thorough characterization of the raindrop size distribution (DSD) m...
It is widely acknowledged that a thorough characterization of the raindrop size distribution (DSD) m...
The raindrop size distribution (DSD) is fundamental for quantitative precipitation estimation (QPE) ...
The adequacy of the gamma model to describe the variability of raindrop size distributions (DSD) is ...
The present study utilizes nine years of measurements taken from a Joss–Waldvogel disdrometer (JWD)....
International audienceThe gamma distribution is often used to characterize raindrop size distributio...
International audienceThe gamma distribution is often used to characterize raindrop size distributio...
International audienceThe gamma distribution is often used to characterize raindrop size distributio...
The main challenges of measuring precipitation are related to the spatio-temporal variability of the...
none3siThe NASA's Global Precipitation Measurement (GPM) mission dual-frequency precipitation radar ...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...
Skewness–kurtosis (β3−β4) and L-skewness–L-kurtosis (τ3−τ4) planes are proposed here as diagnostic t...