Bhavya Duvvuri
Northeastern University
Subject Areas: | Hydrology, Remote sensing |
Recent Activity
ABSTRACT:
This study assesses river discharges derived using remote sensing and hydrologic modeling approaches throughout the CONUS. The remote sensing methods rely on total water storage anomalies (TWSA) from the GRACE and GRACE-FO satellites and water surface elevations from altimetry satellites (i.e., JASON-2/3 and Sentinel-3) to estimate discharge. Surface and subsurface runoff from two Land Surface Models (LSM), NOAH and CLSM, are routed using the Hillslope River Routing model to determine discharge. The LSMs are part of NASA’s Global Land Data Assimilation System (GLDAS).
ABSTRACT:
This repository contains the data used in the paper "Deriving River discharges from GRACE/GRACE-FO total water storage anomalies".
ABSTRACT:
Interactive map to view SWOT river reaches, USGS gauges, SWOT orbit, and generate, analyze synthetic SWOT data
ABSTRACT:
Interactive map to view SWOT river reaches, USGS gauges, SWOT orbit, and generate, analyze synthetic SWOT data using the jupyter notebooks and data (compressed folder) in this resource.
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Created: Aug. 26, 2020, 6:56 p.m.
Authors: Duvvuri, Bhavya
ABSTRACT:
Interactive map to view SWOT river reaches, USGS gauges, SWOT orbit, and generate, analyze synthetic SWOT data using the jupyter notebooks and data (compressed folder) in this resource.

Created: Feb. 16, 2021, 5 p.m.
Authors: Duvvuri, Bhavya
ABSTRACT:
Interactive map to view SWOT river reaches, USGS gauges, SWOT orbit, and generate, analyze synthetic SWOT data

Created: Jan. 13, 2023, 6:12 p.m.
Authors: Duvvuri, Bhavya · Beighley, Edward
ABSTRACT:
This repository contains the data used in the paper "Deriving River discharges from GRACE/GRACE-FO total water storage anomalies".

Created: July 11, 2024, 3:03 p.m.
Authors: Duvvuri, Bhavya · Beighley, Edward
ABSTRACT:
This study assesses river discharges derived using remote sensing and hydrologic modeling approaches throughout the CONUS. The remote sensing methods rely on total water storage anomalies (TWSA) from the GRACE and GRACE-FO satellites and water surface elevations from altimetry satellites (i.e., JASON-2/3 and Sentinel-3) to estimate discharge. Surface and subsurface runoff from two Land Surface Models (LSM), NOAH and CLSM, are routed using the Hillslope River Routing model to determine discharge. The LSMs are part of NASA’s Global Land Data Assimilation System (GLDAS).