International audienceThe episodic nature of hydrological flows such as surface runoff and preferential flow is a result of the nonlinearity of their triggering and the intermittency of rainfall. In this paper we examine the temporal dynamics of threshold processes that are triggered by either an infiltration excess (IE) mechanism when rainfall intensity exceeds a specified threshold value, or a saturation excess (SE) mechanism governed by a storage threshold. We use existing and newly derived analytical results to describe probabilistic measures of the time between successive events in each case, and in the case of the SE triggering, we relate the statistics of the time between events (the inter-event time, denoted IET) to the statistics o...
Quantifying rainfall recharge thresholds, including their spatial and temporal heterogeneity, is of ...
Recent studies have shown that rainfall and hydrological extremes do not randomly occur in time, but...
The spatio-temporal variability of rainfall, especially at fine temporal and spatial scales can sign...
International audienceThe episodic nature of hydrological flows such as surface runoff and preferent...
International audienceThe aim of this paper is to illustrate the effects of selected catchment stora...
International audienceTraditional statistical approaches to flood frequency inherently assume homoge...
In this paper we review threshold behaviour in environmental systems, which are often associated wit...
In this paper we review threshold behaviour in environmental systems, which are often associated wit...
International audienceTraditional statistical approaches to flood frequency inherently assume homoge...
The aim of this paper is to explore how rainfall mechanisms and catchment characteristics shape the ...
Understanding the spatial variability of key parameters of flood probability distributions represent...
The dynamic relationships between water flux and storage, together with the associated water ages an...
International audienceHydrologic response in natural catchments is controlled by a set of complex in...
Abstract. Thresholds and hydrologic connectivity associated with runoff processes are a critical con...
Torrential flows like debris flows or debris floods are fast movements formed by a mix of water and ...
Quantifying rainfall recharge thresholds, including their spatial and temporal heterogeneity, is of ...
Recent studies have shown that rainfall and hydrological extremes do not randomly occur in time, but...
The spatio-temporal variability of rainfall, especially at fine temporal and spatial scales can sign...
International audienceThe episodic nature of hydrological flows such as surface runoff and preferent...
International audienceThe aim of this paper is to illustrate the effects of selected catchment stora...
International audienceTraditional statistical approaches to flood frequency inherently assume homoge...
In this paper we review threshold behaviour in environmental systems, which are often associated wit...
In this paper we review threshold behaviour in environmental systems, which are often associated wit...
International audienceTraditional statistical approaches to flood frequency inherently assume homoge...
The aim of this paper is to explore how rainfall mechanisms and catchment characteristics shape the ...
Understanding the spatial variability of key parameters of flood probability distributions represent...
The dynamic relationships between water flux and storage, together with the associated water ages an...
International audienceHydrologic response in natural catchments is controlled by a set of complex in...
Abstract. Thresholds and hydrologic connectivity associated with runoff processes are a critical con...
Torrential flows like debris flows or debris floods are fast movements formed by a mix of water and ...
Quantifying rainfall recharge thresholds, including their spatial and temporal heterogeneity, is of ...
Recent studies have shown that rainfall and hydrological extremes do not randomly occur in time, but...
The spatio-temporal variability of rainfall, especially at fine temporal and spatial scales can sign...