Eva Sebok

TL;DR: In this article, the authors used distributed temperature sensing (DTS) to map spatial and temporal changes in temperature on a 25 m by 6 m lakebed area in the winter (February), spring (May), and summer (August) of 2012.

TL;DR: In this article, the vertical hydraulic conductivities (Kv) were calculated with in-stream permeameter tests and hydraulic heads were measured to obtain vertical head gradients at eight transects, each comprising five test locations.

TL;DR: In this paper, thermal conductivities and temperature profiles were measured in a coastal lagoon bed where groundwater is known to discharge, and the results showed that the natural variability of sediment thermal conductivity is a parameter to be considered for low flux environments, and it contributes to a better understanding of groundwater-surface water interactions in natural environments.

TL;DR: In this article, the authors combine hy- draulic and tracer methods from point-to-catchment scale to assess the temporal and spatial variability of groundwater discharge in a lowland, groundwater gaining stream in Den- mark.

TL;DR: In this paper, a method is proposed to delineate potential high-groundwater discharge areas and identify deposition-induced temperature anomalies in soft-bedded streams using distributed temperature sensing data.