During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright bands were observed by the University of BASILicata Raman lidar system (BASIL) during several intensive (IOPs) and special (SOPs) observation periods (among others, 23 July, 15 August, and 17 August 2007). Lidar data were supported by measurements from the University of Hamburg cloud radar MIRA 36 (36 GHz), the University of Hamburg dual-polarization micro rain radars (24.1 GHz) and the University of Manchester UHF wind profiler (1.29 GHz). Results from BASIL and the radars for 23 July 2007 are illustrated and discussed to support the comprehension of the microphysical and scattering processes responsible for the appearance of the lidar and ...
Abstract Measurements of the melting layer were made with radar and lidar, during light rain. At the...
In radar observations of hydrometeors, the 0°C isotherm in the atmosphere (i.e., the freezing level)...
This paper illustrates measurements carried out by the Raman lidar BASIL in the frame of the HD(CP)2...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright b...
Multi-wavelength lidar measurements in the melting layer revealing the presence of dark and bright ...
Multi-wavelength lidar measurements in the melting layer revealing the presence of dark and bright b...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright b...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright b...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark/ bright and ...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark bands were o...
Dual-frequency dual-polarization radar observations of the melting of two ice populations in a strat...
The characterization of the melting layer (ML) is an important task for operational radar meteorolog...
On 11 May 2010, an elevated temperature inversion associated with an approaching warm front produced...
In stratiform rainfall, the melting layer (ML) is often visible in radar observations as an enhanced...
Abstract Measurements of the melting layer were made with radar and lidar, during light rain. At the...
In radar observations of hydrometeors, the 0°C isotherm in the atmosphere (i.e., the freezing level)...
This paper illustrates measurements carried out by the Raman lidar BASIL in the frame of the HD(CP)2...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright b...
Multi-wavelength lidar measurements in the melting layer revealing the presence of dark and bright ...
Multi-wavelength lidar measurements in the melting layer revealing the presence of dark and bright b...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright b...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright b...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark/ bright and ...
During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark bands were o...
Dual-frequency dual-polarization radar observations of the melting of two ice populations in a strat...
The characterization of the melting layer (ML) is an important task for operational radar meteorolog...
On 11 May 2010, an elevated temperature inversion associated with an approaching warm front produced...
In stratiform rainfall, the melting layer (ML) is often visible in radar observations as an enhanced...
Abstract Measurements of the melting layer were made with radar and lidar, during light rain. At the...
In radar observations of hydrometeors, the 0°C isotherm in the atmosphere (i.e., the freezing level)...
This paper illustrates measurements carried out by the Raman lidar BASIL in the frame of the HD(CP)2...