This loss in glacier area will result in a reduction in glacier discharge, while the future changes in total discharge are uncertain. We introduced a shared mental model approach with an exploratory case study as a way to overcome persistent barriers in understanding by identifying gaps and overlaps of individual researchers’ perspectives, which improves collaboration in interdisciplinary science. This study investigated the hydrologic responses to wildfires in mountainous regions using a watershed model. I; A method of estimating the form of fine particulates. The study focuses on the solute export from rivers with the purpose of discerning the impacts of anthropic activities and catchment characteristics on water quality. Debris flows are characterized by unsteady flows of water with different content of clay, silt, sand, gravel, and large particles, resulting in a dense moving mixture mass. This model captured the flow and tracer dynamics within each landscape unit quite well, and we could estimate the storage, fluxes and age of water within each.
Comparison of deterministic ensemble Kalman filters for assimilating hydrogeological data, Adv. We quantify net intercatchment groundwater flows in the Meuse basin in a complementary three-step approach through 1 water budget accounting, 2 testing a set of conceptual hydrological models and 3 evaluating against remote sensing actual evaporation data. It has found that the appropriate particle number and maximum evolution number of PSO algorithm are 20 and 30 respectively. The C — Q rating curve ability declined due to enhanced hysteresis effects. Therefore, the Earth system models that neglect lateral transfer underestimate ET in those regions.
This study assesses the potential use of crowdsourced data in hydrological modeling, which are characterized by irregular availability and variable accuracy. ACM, 9, 84—97, https: The sediment regime shifted from two equivalent seasons of sediment delivery to a single major season regime.
We make these gridded global maps dissertatkon available to support diverse stable-isotope applications.
The use of air temperature as an additional variable in a non-parametric model improved the estimation of radar precipitation significantly. Most changes are from climate change; however, vegetation impacts blowing snow, partially compensating the impact of climate change on streamflow. China has suffered some of the effects of global warming, and one of the potential implications of climate warming is the alteration of the temporal—spatial patterns of water resources.
Effects of climate change and human activities on inflow into the Hoabinh Reservoir in the Red River basin, Procedia Environ. Spatiotemporal SWC was decomposed into into three terms spatial forcing, temporal forcing, and interactions between spatial and temporal forcing for near surface and root zone; Empirical orthogonal function indicated that underlying patterns exist in the interaction term at small watershed scales; Estimation of spatially distributed SWC benefits from decomposition of the interaction term; The suggested decomposition of SWC with time stability analysis has potential in SWC downscaling.
Effects of watershed topography, soils, land use, and climate on baseflow hydrology in humid regions: The Arctic has warmed and vegetation has expanded; however, impacts on hydrology are poorly understood.
The high-resolution model allowed for more spatial variability than the low-resolution model. We developed a lecture theatre experiment including some student involvement to illustrate the principles behind this modelling technique.
Here, we examine the challenges in this research field and highlight new perspectives based on interdisciplinary research.
Time-varying storage-water age relationships in a catchment with a Mediterranean climate, Water Resour. It is very likely that the upper Beas basin will get warmer and wetter in the future.
Sediment flux almost doubled every decade. On a national scale, our results confirm the work of prior studies: A negative relationship with imperviousness was identified, which allowed for an efficient catchment classification, thus making weerts H exponent a useful metric to quantitatively assess eeerts impact of catchment imperviousness on streamflow regime.
This study describes how the spatial resolution of hydrological models affects the model results. Thus, it is hypothesized that models can be found, based on simple statistical relationships between low-flow metrics and meteorological states, that can help identify potential low-flow drivers.
This research work focuses on the development of an innovative method for enhancing the predictive capability of macro-scale rainfall—runoff models by means of a geostatistical apporach.
Two methods for detecting and correcting systematic errors bias in groundwater head observations are used leading to improved results compared to standard assimilation methods which ignores any bias.
The contribution of spatial rainfall variability to the total flow variability was found to increase with return periods. Review and evaluation, J. Here I show that seasonal tracer cycles yield strongly biased estimates of mean dkssertation times in nonstationary catchments and, by implication, in real-world catchments.
Results showed that the differences in performance disserrtation from the forcing data were due to compensation effects. We design and implement a theoretical experiment to show that, under low-flow conditions, observed streamflow discrepancies between early and late summer can be attributed to different flow velocities in the river network.
We found that the main contribution to the total flow variability originates from the natural climate variability. Doctoral dissertations in musicology.
The hydrologic processes have been influenced by different climatic factors. The root zone storage capacity S r of the vegetation is an important hydrological parameter.
Jana von Freyberg, Scott T. The influence of land-use changes on soil hydraulic properties: Collected, with weerys introd; by Hubert Foss.
Juli Juli 1 Monat. How isotopic fractionation of snowmelt affects hydrograph separation, Hydrol.