We present results of a detailed study of drip rate variations at 12 drip discharge sites in Glory Hole Cave, New South Wales, Australia. Our novel time series analysis, using the wavelet synchrosqueezed transform, reveals pronounced oscillations at daily and sub-daily frequencies occurring in 8 out of the 12 monitored sites. These oscillations were not spatially or temporally homogenous, with different drip sites exhibiting such behaviour at different times of year in different parts of the cave. We test several hypotheses for the cause of the oscillations, including variations in pressure gradients between karst and cave due to cave breathing effects or atmospheric and earth tides, variations in hydraulic conductivity due to changes in vi...
The use of speleothems to reconstruct past climatic and environmental change through chemical proxie...
Investigations of epikarst hydrological characteristics are important for understanding the complex ...
Cave monitoring provides a crucial link between hydrological and climate processes and how they may ...
We present results of a detailed study of drip rate variations at 12 drip discharge sites in Glory H...
The study of how cave drip-water discharge responds to recharge events is fundamental to evaluating ...
Quantifying rainfall recharge thresholds, including their spatial and temporal heterogeneity, is of ...
High-frequency, spatially-dense discharge monitoring was conducted over fifteen months to characteri...
The last two decades have seen a considerable increase in studies using speleothems as archives of p...
Caves provide useful access points for sampling and monitoring of vadose groundwater to better under...
Palaeoclimate research using speleothems has significantly increased over the last decade, owing to ...
Cave drip water response to surface meteorological conditions is complex due to the heterogeneity of...
This study describes the first use of concurrent high-precision temperature and drip rate monitoring...
Drip rate data have been collected at 15 min intervals at six locations in Stump Cross Caverns, N En...
The study of drip rate and seepage water electrical conductivity (hereafter called conductivity) und...
The use of speleothems to reconstruct past climatic and environmental change through chemical proxie...
Investigations of epikarst hydrological characteristics are important for understanding the complex ...
Cave monitoring provides a crucial link between hydrological and climate processes and how they may ...
We present results of a detailed study of drip rate variations at 12 drip discharge sites in Glory H...
The study of how cave drip-water discharge responds to recharge events is fundamental to evaluating ...
Quantifying rainfall recharge thresholds, including their spatial and temporal heterogeneity, is of ...
High-frequency, spatially-dense discharge monitoring was conducted over fifteen months to characteri...
The last two decades have seen a considerable increase in studies using speleothems as archives of p...
Caves provide useful access points for sampling and monitoring of vadose groundwater to better under...
Palaeoclimate research using speleothems has significantly increased over the last decade, owing to ...
Cave drip water response to surface meteorological conditions is complex due to the heterogeneity of...
This study describes the first use of concurrent high-precision temperature and drip rate monitoring...
Drip rate data have been collected at 15 min intervals at six locations in Stump Cross Caverns, N En...
The study of drip rate and seepage water electrical conductivity (hereafter called conductivity) und...
The use of speleothems to reconstruct past climatic and environmental change through chemical proxie...
Investigations of epikarst hydrological characteristics are important for understanding the complex ...
Cave monitoring provides a crucial link between hydrological and climate processes and how they may ...