Global Navigation Satellite Systems (GNSS) contribute to various Earth observation applications. The present study investigates the potential and limitations of the Global Positioning System (GPS) to estimate in situ water equivalents of the snow cover (snow water equivalent, SWE) by using buried GPS antennas. GPS-derived SWE is estimated over three seasons (2015/16–2017/18) at a high Alpine test site in Switzerland. Results are validated against state-of-the-art reference sensors: snow scale, snow pillow, and manual observations. SWE is estimated with a high correspondence to the reference sensors for all three seasons. Results agree with a median relative bias below 10 % and are highly correlated to the mean of the three ...
The Global Positioning System continuously transmits L-band signals to support real-time navigation ...
Thousands of Global Positioning System (GNSS) receivers worldwide record signals sent by satellites ...
The amount of liquid water in snow characterizes the wetness of a snowpack. Its temporal evolution p...
Global Navigation Satellite Systems (GNSS) contribute to various Earth observation applications. The...
An extensive amount of water is stored in snow covers, which has a high impact on flood development ...
Information on snowpack properties is highly relevant for avalanche warning systems, flood predictio...
Global navigation satellite system (GNSS) refractometry enables automated and continuous in situ sno...
Observations from a submerged GNSS antenna underneath a snowpack need to be analyzed to investigate ...
The temporal evolution of Alpine snowpacks is important for assessing water supply, hydropower gener...
Moisture content in the soil and snow in the alpine environment is an important factor, not only for...
The availability of in situ snow water equivalent (SWE), snowmelt and run-off measurements is still ...
Geodetic-quality GPS systems can be used to measure average snow depth in the ∼1000 m2 area around t...
Monitoring seasonal snow cover properties is critical for properly managing natural hazards such as ...
Snow water equivalent (SWE) is an important variable in describing global seasonal snow cover. Tradi...
The amount of water stored in snowpack is the single most important measurement for the management o...
The Global Positioning System continuously transmits L-band signals to support real-time navigation ...
Thousands of Global Positioning System (GNSS) receivers worldwide record signals sent by satellites ...
The amount of liquid water in snow characterizes the wetness of a snowpack. Its temporal evolution p...
Global Navigation Satellite Systems (GNSS) contribute to various Earth observation applications. The...
An extensive amount of water is stored in snow covers, which has a high impact on flood development ...
Information on snowpack properties is highly relevant for avalanche warning systems, flood predictio...
Global navigation satellite system (GNSS) refractometry enables automated and continuous in situ sno...
Observations from a submerged GNSS antenna underneath a snowpack need to be analyzed to investigate ...
The temporal evolution of Alpine snowpacks is important for assessing water supply, hydropower gener...
Moisture content in the soil and snow in the alpine environment is an important factor, not only for...
The availability of in situ snow water equivalent (SWE), snowmelt and run-off measurements is still ...
Geodetic-quality GPS systems can be used to measure average snow depth in the ∼1000 m2 area around t...
Monitoring seasonal snow cover properties is critical for properly managing natural hazards such as ...
Snow water equivalent (SWE) is an important variable in describing global seasonal snow cover. Tradi...
The amount of water stored in snowpack is the single most important measurement for the management o...
The Global Positioning System continuously transmits L-band signals to support real-time navigation ...
Thousands of Global Positioning System (GNSS) receivers worldwide record signals sent by satellites ...
The amount of liquid water in snow characterizes the wetness of a snowpack. Its temporal evolution p...