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Since that the Newtonian approach is hardly achievable due to limitation of either observations or knowledge of mechanisms, there have been repeated calls to capture the hydrologic system in Darwinian approach for hydrological change prediction or explanation.
This paper uses a hydrological model to detect the hydrological change caused by urbanization.
Urbanization causes hydrological change and increases stormwater runoff volumes, leading to flooding, erosion, and the degradation of instream ecosystem health.
This regional hydrological change was consistent with the 20th century hydroclimatic trends observed in southeastern South America.
Available information on expected regional climate change and a modelling study on hydrological change suggested that adaptation of water management will be required until 2050.
A more reliable alternative might be to conceptualize deep groundwater below the coastal plains a hydrodynamically stagnant zone, responding gradually to landscape and hydrological change on geologic timescales.
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We explain Holocene hydrological changes through analysis of changing zonal climatic influences linked to Congo Air Boundary (CAB) and Intertropical Convergence Zone (ITCZ) dynamics, the effects of which filter into the region via complex drainage basin dynamics.
This paper proposes a modeling framework able to analyze the alterations in watershed hydrology induced by two recurrent drivers for hydrological changes: climate change and urbanization.
On the one hand, climate change-driven hydrological changes are catastrophically altering the landscape.
The Indian government argued that hydrological changes had diverted Ganges water from the port of Kolkata over the preceding century and resulted in the deposition of silt and the intrusion of saline seawater.
We were dismayed, however, that although the article focused on recent hydrological changes to the Boiling Lake, it barely acknowledged that Dominica is comprised of at least nine potentially active volcanic centers, giving it one of the highest concentrations of potentially active volcanoes in the world.
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