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The multiple paired watersheds eliminated the potentially confounding edaphic and topographic influences from changes in hydrological processes related to woody encroachment.
Changes in hydrological processes in large watersheds may heavily impact the dynamics of downstream aquatic ecosystems such as lakes and reservoirs.
To assess the potential role of climate-driven changes in hydrological processes to influence greenhouse-gas emissions, we utilized water isotope tracers to characterize the water balance of thermokarst lakes in Nunavik during three consecutive mid- to late summer sampling campaigns (2012 2014).
Because of uncertainty regarding future changes in hydrological processes in the Yellow River basin, and the lack of feasible engineering measures to mitigate "suspended river" and "hump deposition" problems in the LYR, caution should be exercised with respect to changes in the river training strategy for the LYR.
Hydrological modeling is explored as an operational tool for effective assessment of changes in hydrological processes relating to modification of land cover and climate change.
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Soil moisture is a key variable in hydrological processes.
Understanding the upstream-downstream linkages in hydrological processes is essential for water resources planning in river basins.
His current research areas include interdependent infrastructure system analysis, coupled human-natural system analysis with an emphasis on human interferences in hydrological processes, water-energy-food system modeling and sustainable water resources management (particularly in developing countries).
However, remarkable changes in the hydrological processes in the Yellow River basin, as well as immediate pressure from socio-economic development in the Yellow River basin, make it necessary to consider if there is a possibility to change the river training strategy from wide-river training to narrow-river training.
The change in the scales and locations of spatial pattern of soil water storage indicates the change in the hydrological processes, which can be used to identify the change in the sampling domain.
Despite approximately 500 years of intense land-use change in this biome, the influence of land-use changes on hydrological processes have yet to be investigated in-depth.
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