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).

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ABSTRACT:

This repository contains the data used in the paper "Deriving River discharges from GRACE/GRACE-FO total water storage anomalies".

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ABSTRACT:

Interactive map to view SWOT river reaches, USGS gauges, SWOT orbit, and generate, analyze synthetic SWOT data

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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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Resource Resource

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.

Show More
Resource Resource

ABSTRACT:

Interactive map to view SWOT river reaches, USGS gauges, SWOT orbit, and generate, analyze synthetic SWOT data

Show More
Resource Resource

ABSTRACT:

This repository contains the data used in the paper "Deriving River discharges from GRACE/GRACE-FO total water storage anomalies".

Show More
Resource Resource

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).

Show More