Novel wireless sensors for in situ measurement of sub-ice hydrologic systems
Bagshaw, E, Lishman, B, Wadham, J, Bowden, J, Burrow, S, Clare, L and Chandler, D (2014). Novel wireless sensors for in situ measurement of sub-ice hydrologic systems. Annals of Glaciology. 55 (65), pp. 41 - 50.
|Authors||Bagshaw, E, Lishman, B, Wadham, J, Bowden, J, Burrow, S, Clare, L and Chandler, D|
Wireless sensors have the potential to provide significant insight into in situ physical and biogeochemical processes in sub-ice hydrologic systems. However, the nature of the glacial environment means that sensor deployment and data return is challenging. We describe two bespoke sensor platforms, electronic tracers or ‘ETracers’, and ‘cryoegg’, for untethered, wireless data collection from glacial hydrologic systems, including subglacial channels. Both employ radio frequencies for data transmission, are designed to endure harsh environmental conditions and can withstand low temperatures, high pressure, turbulence and abrasion. We discuss the design, optimization and field testing of the ETracers and cryoegg, culminating in test deployments beneath the Greenland ice sheet. The small, low-cost ETracers were able to travel through subglacial drainage channels, from where they returned water pressure measurements through 100m of ice, and could measure water depth in crevasses. The larger cryoegg was able to return multi-parameter data from moulins through 500m of wet ice to receivers up to 2km away, and from 12m depth in a proglacial lake to a receiver on the shore. The tests demonstrate that the cryoegg and ETracers are low-power, versatile, robust wireless sensor platforms suitable for glacial environments, which may be used with portable, low-cost receiving equipment.
|Journal||Annals of Glaciology|
|Journal citation||55 (65), pp. 41 - 50|
|Publisher||Cambridge University Press (CUP)|
|Digital Object Identifier (DOI)||doi:10.3189/2014AoG65A007|
|01 Sep 2014|
|Publication process dates|
|Deposited||14 Feb 2017|
|Accepted||01 Sep 2014|
CC BY 4.0
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