The rain parameters derived from the laser OTT second-generation Particle Size Velocity (Parsivel(2)), the two-dimensional video disdrometer (2DVD), and DZZ5 tipping-bucket rain gauge (RG) during the Integrative Monsoon Frontal Rainfall Experiment (IMFRE) in summer 2018 are compared. The total rainfall amounts observed by Parsivel, 2DVD, and RG during IMFRE were 178.07, 176.76, and 182.5 mm, while their total rainy hours were 113, 113, and 90. The meanD(m)(mass-weighted mean diameter) andLWC(liquid water content) values derived from Parsivel and 2DVD were 1.03 and 1.01 mm and 0.247 and 0.223 g m(-3). The rainy samples from six Parsivel sites over the middle reaches of the Yangtze River during the 2016-2018 Meiyu seasons have been collected ...
Previous studies have reported the large-scale meteorological conditions and dynamic causes of the e...
The East Asian monsoon has a strong seasonal effect on the rainfall regime of Eastern China. In orde...
We investigated the cloud liquid water (CLW) and rain liquid water (RLW) during weak precipitations ...
This study investigates the statistical characteristics of raindrop size distributions (DSDs) in mon...
Raindrop size distribution (DSD) can be used to improve the accuracy of radar quantitative precipita...
Disdrometer observations obtained by an OTT Parsivel2 during the 2017 Great Hunan Flood from 1:00 a....
The South China Sea (SCS) is the largest and southernmost sea in China. Water vapor from the SCS is ...
The seasonal variations of raindrop size distribution (DSD) and rainfall are investigated using thre...
The dataset for the JGR article "Statistical Characteristics of Raindrop Size Distributions and Para...
Using the data of 545 meteorological stations in 1961-2015, according to the rainfall intensity clas...
Understanding the patterns and mechanisms of precipitation variations is important for assessing flo...
Better simulations and predictions of heavy rainfall associated with Meiyu fronts are critical for f...
Understanding rainfall anomalies and their relationship with floods in the Yangtze River Basin (YRB)...
To understand the microphysical characteristics of rainfall in four different climatological regions...
This work for the first time analyzed the vertical structures of the different stages of Meiyu preci...
Previous studies have reported the large-scale meteorological conditions and dynamic causes of the e...
The East Asian monsoon has a strong seasonal effect on the rainfall regime of Eastern China. In orde...
We investigated the cloud liquid water (CLW) and rain liquid water (RLW) during weak precipitations ...
This study investigates the statistical characteristics of raindrop size distributions (DSDs) in mon...
Raindrop size distribution (DSD) can be used to improve the accuracy of radar quantitative precipita...
Disdrometer observations obtained by an OTT Parsivel2 during the 2017 Great Hunan Flood from 1:00 a....
The South China Sea (SCS) is the largest and southernmost sea in China. Water vapor from the SCS is ...
The seasonal variations of raindrop size distribution (DSD) and rainfall are investigated using thre...
The dataset for the JGR article "Statistical Characteristics of Raindrop Size Distributions and Para...
Using the data of 545 meteorological stations in 1961-2015, according to the rainfall intensity clas...
Understanding the patterns and mechanisms of precipitation variations is important for assessing flo...
Better simulations and predictions of heavy rainfall associated with Meiyu fronts are critical for f...
Understanding rainfall anomalies and their relationship with floods in the Yangtze River Basin (YRB)...
To understand the microphysical characteristics of rainfall in four different climatological regions...
This work for the first time analyzed the vertical structures of the different stages of Meiyu preci...
Previous studies have reported the large-scale meteorological conditions and dynamic causes of the e...
The East Asian monsoon has a strong seasonal effect on the rainfall regime of Eastern China. In orde...
We investigated the cloud liquid water (CLW) and rain liquid water (RLW) during weak precipitations ...