Skip to main content

Thermal infrared and photogrammetric data collected by drone for hydrogeologic characterization around two US Geological Survey Next Generation Water Observing Systems stream gage locations near Claryville, NY, USA

Dates

Publication Date
Start Date
2019-10-08
End Date
2019-10-10

Citation

Briggs, M.A., Dawson, C.B., White, E.A., Gazoorian, C.L., Hare, D.K., and Lane, J.W., 2020, Thermal infrared and photogrammetric data collected by drone for hydrogeologic characterization around two US Geological Survey Next Generation Water Observing Systems stream gage locations near Claryville, NY, USA: U.S. Geological Survey data release, https://doi.org/10.5066/P9FIZTPU.

Summary

The U.S. Geological Survey (USGS) collected low-altitude (typically 200-350 ft above land surface) airborne thermal infrared, and visual imagery data via a multirotor, small unoccupied aircraft system (UAS or ‘drone’) deployed along the river corridor encompassing two U.S. Geological Survey Next Generation Water Observing Systems (NGWOS) stream gage locations near Claryville, NY, USA. One site is the West Branch Neversink River at Claryville, NY (USGS station number 01434498) and the Neversink River at Claryville, NY (USGS station number 01435000). Beginning in summer 2019 these stations serve as groundwater/surface water instrumentation ‘test beds’ for the NGWOS program. Data collected at the sites include water electrical conductivity, [...]

Contacts

Attached Files

Click on title to download individual files attached to this item.

West_Branch_visible_ortho.jpg thumbnail 1.65 MB image/jpeg
West_Branch_apparent_thermal.jpg thumbnail 1.96 MB image/jpeg
thermal_infrared_data.zip 215.48 MB application/zip
7.84 GB application/zip
README.txt 659 Bytes text/plain

Purpose

There are multiple purposes for this drone-based data collection. At a high level, the data are used to support the characterization of lateral exchanges of groundwater and surface water along the river corridor. More specifically, the thermal data can be used to indicate groundwater discharge locations due to inherent differences in groundwater and surface water temperatures during most times of day in October at these locations. Thermal data can also be used to map larger scale warming of river water during the day above natural impoundments such as beaver dams and gravel bars, adding to the heterogenous ‘thermalscape’ of the river corridor. Visual data are used to infer surface water levels, bank structure, and lateral hydrologic gradients. Additionally, both the visible-light and thermal orthomosaics are useful as a time-specific georeferenced map of the river corridor upon which point-scale spatial data can be visualized.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9FIZTPU

Item Actions

View Item as ...

Save Item as ...

View Item...