Transformations in hydrological resilience: Unraveling the impact of landscape hydric potential on flood dynamics: A case study, Drwinka catchment (Poland).

Flooding remains a critical issue in urban catchments, driven by complex interactions between land use changes, hydrological dynamics, and environmental factors. This study aims to investigate how modifications in Landscape Hydric Potential (LHP) affect flood behavior in the Drwinka River catchment in Krakow, Poland. Given the rapid urbanization and its impacts on hydrological systems, understanding these changes is essential for effective flood management and mitigation.

Rich north, poor south - Regionalization of European water retention: The landscape hydric potential concept.

Natural water retention varies greatly across Europe. Understanding the key ecosystem factors that affect the quantity, quality, availability, and spatiotemporal distribution of water resources is essential for effective landscape management. This study presents the Landscape Hydric Potential (LHP) index of Europe, which serves as an indicator of the natural environment's ability to infiltrate and retain water.

Exploiting satellite data for total direct runoff prediction using CN-based MSME model.

This paper explores the potential to enhance the functionality of the modified Sahu-Mishra-Eldho model (MSME-CN) using indirect soil moisture measurements derived from satellite data. The current version of the MSME-CN model is not applicable in ungauged watersheds due to the necessity of calibrating the crucial parameter α, which reflects soil saturation, based on measured rainfall-runoff events. We hypothesize that the Normalized Difference Vegetation Index (NDVI) can serve as an indirect indicator of soil moisture to assess the soil saturation parameter α in the MSME model.

Link between hydric potential and predictability of maximum flow for selected catchments in Western Carpathians.

This study aimed to determine the link between a hydric potential of catchments (LHP) and the predictability (P) of maximum flow of selected rivers in southern Poland (within the Upper Vistula basin) and Slovakia. The LHP method refers to the ability of ecosystems to slow down runoff and retain water. The LHP method is focused on the analysis of the following indicators, shaping the geosphere at the catchment scale: hydrogeological conditions, soil conditions, meteorological conditions, geomorphological conditions, and land use.