Abstract

Snow water equivalent (SWE) can be measured using low-cost Global Navigation Satellite System (GNSS) sensors with one antenna placed below the snowpack and another one serving as a reference above the snow. The underlying GNSS signal-based algorithm for SWE determination for dry- and wet-snow conditions processes the carrier phases and signal strengths and derives additionally liquid water content (LWC) and snow depth (HS). So far, the algorithm was tested intensively for high-alpine conditions with distinct seasonal accumulation and ablation phases. In general, snow occurrence, snow amount, snow density and LWC can vary considerably with climatic conditions and elevation. Regarding alpine regions, lower elevations mean generally earlier and faster melting, more rain-on-snow events and shallower snowpack. Therefore, we assessed the applicability of the GNSS-based SWE measurement at four stations along a steep elevation gradient (820, 1185, 1510 and 2540 m a.s.l.) in the eastern Swiss Alps during two winter seasons (2018–2020). Reference data of SWE, LWC and HS were collected manually and with additional automated sensors at all locations. The GNSS-derived SWE estimates agreed very well with manual reference measurements along the elevation gradient and the accuracy (RMSE = 34 mm, RMSRE = 11 %) was similar under wet- and dry-snow conditions, although significant differences in snow density and meteorological conditions existed between the locations. The GNSS-derived SWE was more accurate than measured with other automated SWE sensors. However, with the current version of the GNSS algorithm, the determination of daily changes of SWE was found to be less suitable compared to manual measurements or pluviometer recordings and needs further refinement. The values of the GNSS-derived LWC were robust and within the precision of the manual and radar measurements. The additionally derived HS correlated well with the validation data. We conclude that SWE can reliably be determined using low-cost GNSS-sensors under a broad range of climatic conditions and LWC and HS are valuable add-ons.

Highlights

  • The water stored in the seasonal snow cover plays a crucial role in the hydrological cycle in mountain regions and is a key source of fresh water supply

  • Snow water equivalent (SWE) can be measured using low-cost Global Navigation Satellite System (GNSS) sensors with one antenna placed below the snowpack and another one serving as a reference above the snow

  • The derivation of liquid water content (LWC) was robust and the values of LWC were in the range of the manual and upward-looking ground penetrating radar (upGPR) measurements

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Summary

Introduction

The water stored in the seasonal snow cover plays a crucial role in the hydrological cycle in mountain regions and is a key source of fresh water supply. The spatial and temporal distribution of SWE under dry-snow and rather shallow snowpack conditions can be obtained from microwave satellite remote sensing (Larue et al, 2017; Pulliainen and Hallikainen, 2001; Shi and Dozier, 2000) This is, until now, not sufficiently feasible in highly complex alpine terrain due to either low spatial resolution especially of passive microwave sensors or regarding active microwave sensors, due to penetration depth limits, foreshortening, shadowing and layover effects. Combining the GNSS signal attenuation approach of Koch et al (2014) 75 with two-way travel time information derived by an L-band upward-looking ground penetrating radar (upGPR), it was possible to simultaneously derive SWE, HS and LWC for dry- and wet-snow conditions (Schmid, 2015; Schmid et al, 2015). Good accuracy of the GNSS-derived SWE was achieved for the high-alpine site

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