Zobrazeno 1 - 10
of 145
pro vyhledávání: '"W.E. Bardsley"'
Autor:
Ali Shokri, W.E. Bardsley
Publikováno v:
Advances in Water Resources. 92:299-315
Hydrological and hydrogeological investigation of drained land is a complex and integrated procedure. The scale of drainage studies may vary from a high-resolution small scale project through to comprehensive catchment or regional scale investigation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8daae8a220d50a809f256c6c2ac0f02c
https://doi.org/10.1016/j.advwatres.2016.04.013
https://doi.org/10.1016/j.advwatres.2016.04.013
Publikováno v:
Environmental Modelling & Software. 72:33-43
A formalised means of simplifying hydrological models concurrent with calibration is proposed for use when nonlinear models can be initially formulated as over-parameterised constrained absolute deviation regressions of nonlinear expressions. This pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0ef5a038ed4b7c920d528b4c76197da
https://doi.org/10.1016/j.envsoft.2015.06.008
https://doi.org/10.1016/j.envsoft.2015.06.008
Autor:
W.E. Bardsley
Publikováno v:
Hydrological Processes. 30:3730-3732
Multicomponent probability distributions such as the two-component Gumbel distribution are sometimes applied to annual flood maxima when individual floods are seen as belonging to different classes, depending on physical processes or time of year. Ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::903b72c4702b0af2bb523fae0928ca25
https://doi.org/10.1002/hyp.10886
https://doi.org/10.1002/hyp.10886
Autor:
W.E. Bardsley
Publikováno v:
Stochastic Environmental Research and Risk Assessment. 30:1059-1061
One mechanism giving rise to the hypergeometric distribution is the number of matches in a random reordering of a sequence of forecasts of binary events. This provides a simple means of invalidating a time series of binary forecasts if in fact the fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::50e3d6facd1db955c97f58b2c76b99c7
https://doi.org/10.1007/s00477-015-1071-z
https://doi.org/10.1007/s00477-015-1071-z
Autor:
W.E. Bardsley
Publikováno v:
Hydrological Processes. 27:2851-2856
Checking the predictive worth of an environmental model inevitably includes a goodness of fit metric to quantify the degree of matching to recorded data, thereby giving a measure of model performance. Considerable analysis and discussion have taken p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc172421837bb9294344ef6d40a5749d
https://doi.org/10.1002/hyp.9914
https://doi.org/10.1002/hyp.9914
Autor:
H. Vavae, W.E. Bardsley
Publikováno v:
Natural Resources Research. 18:277-283
For the Tuvalu Island group in the western Pacific, a simple graphical method is proposed as a means of forecasting whether rainfall totals for the next 1, 2,…,6 months will be below average. The method is based on scatter plots where the points ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f9c6bee735c6ea83177e0c038384511d
https://doi.org/10.1007/s11053-009-9104-2
https://doi.org/10.1007/s11053-009-9104-2
Autor:
Jennifer Purdie, W.E. Bardsley
Publikováno v:
Journal of Hydrology. 338:57-62
The standard means of establishing predictive ability in hydrological models is by finding how well predictions match independent validation data. This matching may not be particularly good in some situations such as seasonal flow forecasting and the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec22332eeaa35cd5f396149a6b0ebb26
https://doi.org/10.1016/j.jhydrol.2007.02.019
https://doi.org/10.1016/j.jhydrol.2007.02.019
Autor:
David I. Campbell, W.E. Bardsley
Publikováno v:
Journal of Hydrology. 335:240-246
Summary Field studies have demonstrated that ground surface rainfall accumulation can be detected at depth by synchronous increases in static confined groundwater pore pressures. This opens the way for “geological weighing lysimeters” providing d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5215521a7948d58042c300130252a693
https://doi.org/10.1016/j.jhydrol.2006.11.014
https://doi.org/10.1016/j.jhydrol.2006.11.014
Autor:
W.E. Bardsley
Publikováno v:
Advances in Water Resources. 30:113-117
It may sometimes be desirable to introduce bounds into probability distributions to formalise the presence of upper or lower physical limits to data to which the distribution has been applied. For example, an upper bound in raindrop sizes might be re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19560ece8730a9167410eb4f4329d500
https://doi.org/10.1016/j.advwatres.2006.03.003
https://doi.org/10.1016/j.advwatres.2006.03.003
Autor:
Ali Shokri, W.E. Bardsley
Publikováno v:
Journal of Irrigation and Drainage Engineering. 141
The Hooghoudt equation is widely used as a simple means of specifying drain spacing when designing networks of parallel drains in drainage systems, based on estimating the maximum water table height between two drains. It is shown via comparison with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fda0376b5fb6ced8141d6f6a5a452aa0
https://doi.org/10.1061/(asce)ir.1943-4774.0000835
https://doi.org/10.1061/(asce)ir.1943-4774.0000835