has been cited by the following article(s):
[1]
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Distributed hydrologic model using GPM-IMERG images in the Huaynamota River Watershed, Nayarit, México
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2020 |
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[2]
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Facultad de Ciencias Químicas Carrera de Ingeniería Industrial
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2019 |
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[3]
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Facultad de Ingeniería
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2019 |
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[4]
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Tropical Andes Radar Precipitation Estimates Need High Temporal and Moderate Spatial Resolution
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2019 |
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[5]
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Efecto de advección sobre la acumulación de lluvia distribuida espacialmente usando imágenes de un radar meteorológico
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2019 |
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[6]
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URBAN FLOOD VULNERABILITY ASSESSMENT OF BHOPAL, MP, INDIA
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International Journal of Civil Engineering and Technology (IJCIET),
2019 |
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[7]
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Análisis del fenómeno subsidencia-inundación mediante InSAR y FLO-2D en la ciudad de Morelia, Michoacán
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2019 |
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[8]
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Statistical assessment and hydrological utility of the latest multi-satellite precipitation analysis IMERG in Ganjiang River basin
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Atmospheric Research,
2016 |
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[9]
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Assimilating Merged Remote Sensing and Ground-Based Snowpack Information for Streamflow Simulation
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2015 |
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[10]
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Remote Sensing and Ground-Based Weather Forcing Data Analysis for Streamflow Simulation
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Hydrology,
2014 |
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[11]
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Assistant Professor (Physics) Department of Basic Science and Humanities Narula Institute of Technology, Agarpara, Kolkata 700109 Email: dhananjay. tripathi …
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[1]
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Tropical Andes Radar Precipitation Estimates Need High Temporal and Moderate Spatial Resolution
Water,
2019
DOI:10.3390/w11051038
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|
[2]
|
Tropical Andes Radar Precipitation Estimates Need High Temporal and Moderate Spatial Resolution
Water,
2019
DOI:10.3390/w11051038
|
|
|
[3]
|
Statistical assessment and hydrological utility of the latest multi-satellite precipitation analysis IMERG in Ganjiang River basin
Atmospheric Research,
2017
DOI:10.1016/j.atmosres.2016.07.020
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[4]
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Remote Sensing and Ground-Based Weather Forcing Data Analysis for Streamflow Simulation
Hydrology,
2014
DOI:10.3390/hydrology1010089
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[5]
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Remote Sensing and Ground-Based Weather Forcing Data Analysis for Streamflow Simulation
Hydrology,
2014
DOI:10.3390/hydrology1010089
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