Hydrological signals in tilt and gravity residuals at Conrad Observatory (Austria)

نویسندگان

چکیده

Abstract. The superconducting gravimeter (SG) GWR C025 has monitored the time variation in gravity at Conrad Observatory (Austria) since autumn 2007. Two tiltmeters have operated continuously spring 2016, namely a 5.5 m long interferometric water level tiltmeter and Lippmann-type 2D pendulum tilt sensor. co-located co-oriented set up enables wide range of investigations because tilts are sensitive to both geometrical solid Earth deformations potential changes. tide-free residuals SG clearly reflect and/or deformation effects associated with short- long-term environmental processes reveal complex transport process observatory site. Water accumulation on terrain surface causes short-term (a few hours) which imaged by N–S residuals. Long-term (> days/weeks) variations occur frequently after long-lasting rain, heavy rain or rapid snowmelt. Gravity same hydrological but different physical causes. gravitational effect mass transport, while modelling results exclude purely source observed tilts. Tilt show response loading instead. Tilts can be strongly affected strain–tilt coupling (cavity effect). signals much stronger than those E–W component, is most probably due cavity 144 tunnel being oriented an direction.

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ژورنال

عنوان ژورنال: Hydrology and Earth System Sciences

سال: 2021

ISSN: ['1607-7938', '1027-5606']

DOI: https://doi.org/10.5194/hess-25-217-2021