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Holistic versus monomeric strategies for hydrological modelling of human-modified hydrosystems
Holistic versus monomeric strategies hydrological modelling human-modified
2011/3/15
The modelling of human-modified basins that are inadequately measured constitutes a challenge for hydrological science. Often, models for such systems are detailed and hydraulics-based for only one pa...
Changes in streamflow and sediment discharge and the response to human activities in the middle reaches of the Yellow River
Changes in streamflow sediment discharge
2011/1/7
The changes in streamflow and sediment discharge in the middle reaches of the Yellow River are a focus. In this paper, based on the precipitation, streamflow and sediment discharge series data (1950–2...
HYDROCHEMICAL CHARACTERISTICS OF THE JORDAN AND YARMOUK RIVERS：EFFECTS OF NATURAL AND HUMAN ACTIVITIES
Water chemistry HYDROCHEMICAL CHARACTERISTICS Jordan Rivers Yarmouk Rivers
2009/10/13
Water chemistry was used to assist in understanding the effect of human and natural activities on the Jordan and Yarmouk Rivers. Eighty-eight water samples were collected from different locations alon...
A GENERALIZATION OF CLARK’S IUH FOR FLATLAND AREAS WITH STRONG HUMAN INTERVENTIONS
Instantaneous Unit Hydrograph hydrological parameters geomorphologic characteristics
2009/10/13
We present an improvement of Clark's Instantaneous Unit Hydrograph (IUH), which we call the "GAIUH", linking hydrological parameters and geomorphologic characteristics of flatland basins with strong h...
Dynamics of resource production and utilisation in two-component biosphere-human and terrestrial carbon systems
terrestrial carbon systems biosphere-human production-utilisation
2009/5/7
This paper analyses simple models for "production-utilisation" systems, reduced to two state variables for producers and utilisers, respectively. Two modes are distinguished: in "harvester" systems th...
Effects of human activities on the Yangtze River suspended sediment flux into the estuary in the last century
riverine sediment flux human activities
2009/3/11
The surface erosion area in the Yangtze River basin increased from 364×103 km2 in the 1950s to 707×103 km2 in 2001 due to a great increase in population. Based on the regression relationship between s...
