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In this paper, we introduce a lightweight temporal perturbation based scheme, where sensor readings are buffered and disordered to obfuscate the temporal information of the original sensor measurement stream with differential privacy.
When these changes occur, the LSE output falls a little behind the measurement stream, but since the normal execution speed is about twice the reporting rate of 60 samples per second, it can quickly catch up.
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It is worth noting that this standard provides the option to include analogue and digital values into the measurement streams.
Thus, there is compelling evidence from several measurement streams to show that the terrestrial ecosystem sink is persistent and large [e.g., 7, 37] and that most of this has been into forests including in the tropics [e.g., 40].
To make the comparisons more meaningful, for all tracking methods, the same random measurements streams were used.
Ultrasonic river gauging is based on the continuous measurement of stream velocity at chosen depths by recording the difference in time for sound pulses sent obliquely across the river in opposite direction.
Length measurements at stream locations (mid-eye to hypural plate, MEHP) were designed to prevent measurement error associated with altered morphology (extended kype and dorsal ventral elongation), related to sexual maturation (Blair et al. 1993).
In concrete terms, 68 measurements of stream discharge and bed load transport rate were carried out at a location, near the basin outlet.
For this study, we characterized the annual transfers of dissolved inorganic carbon (DIC) along the groundwater-stream-river continuum based on DIC concentrations, stable isotope composition and measurements of stream discharges.
In the framework of diploma theses elaborated in the Division of Hydraulic Engineering, Department of Civil Engineering, Democritus University of Thrace, measurements of stream discharge and bed load transport rate were carried out at the outlet of the mountain part of Nestos River basin (northeastern Greece).
Tracer measurements of stream and spring discharge and groundwater-surface water exchange were combined with synoptic sampling of water isotopic and geochemical composition in order to characterize and quantify contributions to streamflow from different groundwater reservoirs.
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