Troutbrook Cam and sensor
Detailed Description
USGS Trail Camera and air Tidbit temperature shelter attached to a tree looking facing downstream on Trout Brook at Grand Ave near Hackettstown, New Jersey. Having both sensors allows for quick identification of on-site conditions during temperature anomalies. Explore the photos here: Flow Photo Explorer | USGS
Sources/Usage
Public Domain.
Related
Flow Photo Explorer (FPE) Project in New Jersey
The Flow Photo Explorer (FPE) is a database, machine learning, and data visualization platform using timelapse images to develop new approaches for collecting hydrologic data in streams and other waterbodies where traditional monitoring methods are not feasible or cost-prohibitive. The Musconetcong River was chosen to participate in the early study, and we are expanding the work to other rivers.
New Jersey Subbasin Paired Air & Stream Water Temperature Networks
The temperature, water quality, and channel connectivity along headwater stream networks often show highly dynamic spatiotemporal patterns that are tied to localized hydrogeologic and landcover controls. Groundwater exchanges exert a spatially discontinuous influence on streams that reflect, in part, the preferential nature of groundwater discharge as controlled by recharge, topography, and...
Related
Flow Photo Explorer (FPE) Project in New Jersey
The Flow Photo Explorer (FPE) is a database, machine learning, and data visualization platform using timelapse images to develop new approaches for collecting hydrologic data in streams and other waterbodies where traditional monitoring methods are not feasible or cost-prohibitive. The Musconetcong River was chosen to participate in the early study, and we are expanding the work to other rivers.
New Jersey Subbasin Paired Air & Stream Water Temperature Networks
The temperature, water quality, and channel connectivity along headwater stream networks often show highly dynamic spatiotemporal patterns that are tied to localized hydrogeologic and landcover controls. Groundwater exchanges exert a spatially discontinuous influence on streams that reflect, in part, the preferential nature of groundwater discharge as controlled by recharge, topography, and...