This paper documents the development of an interactive web map designed to communicate geographic research using three different technologies: the Extensible Markup Language (XML), the Google Maps API for Flash, and ActionScript 3.0. These technologies are used in conjunction with geospatial data related to a research study involving the use of Synthetic Aperture Radar (SAR) in monitoring hydro...

The aim of this work is the development of an integrated Data Based Mechanistic (DBM) rainfall-flow/flow-routing model of the Upper River Narew catchment and the river reach between Bondary and Suraż suitable for scenario analysis. The modelling tool developed is formulated in MATLAB-SIMULINK language. It has a flexible, modular structure that can easily be extended by adding new features, such...

The variation of hydrological conditions in the basin affects original stable state basin, and change eco-hydrological also plays a decisive role stability basin. In this manuscript, Indicators Hydrologic Alteration (IHA) was used to diagnose watershed from perspective, new diagnostic method proposed current study, which extraction most relevant indicators based on similar year sensitive index ...

Drought is a complex phenomenon with high spatial and temporal variability. Water scarcity has become growing problem in Slovenia recent decades. Therefore, the variability of hydrological drought was investigated this study by analysing Standardized Streamflow Index (SSI). Monthly discharge data series from 46 gauging stations for period 1961–2016 were used to calculate SSI values at five diff...

Using the conformal invariance of the SL(2, IR) ⊗ SO(1, 1) d−2 /SO(1, 1) coset models we calculate the conformally exact metric and dilaton, to all orders in the 1/k expansion. We consider both vector and axial gauging. We find that these cosets represent two different space–time geometries: (2d black hole)⊗IR d−2 for the vector gauging and (3d black string)⊗IR d−3 for the axial one. In particu...

ABSTRACT Maximum flows are often estimated from flood frequency analysis, by means of the statistical fitting a theoretical probability distribution to maximum annual flow data. However, because limitations imposed practice at-site measurement, empirical models applied as rating curve for estimating streamflow. These curves approximations actual and incorporate different sources uncertainty, es...