2020
DOI: 10.1016/j.atmosres.2020.105019
|View full text |Cite
|
Sign up to set email alerts
|

Potential use of the GLM for nowcasting and data assimilation

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

1
2
0

Year Published

2021
2021
2023
2023

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 7 publications
(3 citation statements)
references
References 74 publications
1
2
0
Order By: Relevance
“…The IWP values (Figure 5b) were highest in the T4 sub-region, followed by the T3 sub-region. This fact corroborates the importance of this variable for charge generation in storm clouds and the consequent lightning occurrence, since the highest (smallest) densities occurred in the sub-region with the highest (smallest) amount of ice, reinforcing the close relationship between ice content and cloud electrification [14,20,27,35,37,84,96]. The Tukey multiple comparison test (Figure 6b), indicated that the IWC of the T4 sub-region is statistically different from the others (p-value < 0.1) and no significant difference between T1 and T2, and between T1 and T3.…”
Section: Microphysical Properties As a Function Of Lightning Tertilessupporting
confidence: 76%
“…The IWP values (Figure 5b) were highest in the T4 sub-region, followed by the T3 sub-region. This fact corroborates the importance of this variable for charge generation in storm clouds and the consequent lightning occurrence, since the highest (smallest) densities occurred in the sub-region with the highest (smallest) amount of ice, reinforcing the close relationship between ice content and cloud electrification [14,20,27,35,37,84,96]. The Tukey multiple comparison test (Figure 6b), indicated that the IWC of the T4 sub-region is statistically different from the others (p-value < 0.1) and no significant difference between T1 and T2, and between T1 and T3.…”
Section: Microphysical Properties As a Function Of Lightning Tertilessupporting
confidence: 76%
“…Correspondingly, more studies are required to assess the performance of GPM IMERG against other satellite and reanalysis products to find the advantages and limitations of the GPM satellite. Furthermore, other precipitation specific properties such as spatial and temporal heterogeneity, spatial and temporal intermittence, extreme variability and multi-fractal comparisons is necessary to overcome substantial uncertainties rainfall estimations [57][58][59]. Cristiano et al [60] also depicted in their review that the rainfall variability may need wider range of conditions and scenario based in observational datasets for urban hydrological basins, which need proper analysis for development of better hydrological response system with higher sensitivity.…”
Section: Future Studies and Shortcomingsmentioning
confidence: 99%
“…Lightning data assimilation (LDA) has been widely used to improve the intense precipitation forecast worldwide because of the ability of lightning to precisely locate areas of deep convection. Different techniques have been used for LDA as follows: (a) The forcing of water vapour and other hydrometeors, with both nudging [22][23][24][25][26][27][28] and 3D-Var [21,29,30], (b) retrieving the convective precipitation and latent heat profile by lightning and adjusting the initial three-dimensional thermo-dynamic field of NWP models [31,32], (c) retrieving the radar reflectivity by lightning and assimilating it in NWP models [33][34][35][36], and (d) forcing convection through the adjustment of thermo-dynamical fields [37]. Attempts to suppress spurious convection through lightning data assimilation have also been reported in the literature [38].…”
Section: Introductionmentioning
confidence: 99%