Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Hannes H. Bauser"'
Publikováno v:
Vadose Zone Journal, Vol 19, Iss 1, Pp n/a-n/a (2020)
Abstract The description of soil water movement at the field scale requires soil hydraulic material properties. These cannot be measured directly and exhibit an intrinsic multiscale heterogeneity. The estimation of soil hydraulic properties through i
Externí odkaz:
https://doaj.org/article/6a9c8c5b4b6b4d2882cf10479def2967
Flow recession analysis, relating discharge Q and its time rate of change −dQ/dt, has been widely used to understand catchment scale flow dynamics. However, data points in the recession plot, the plot of −dQ/dt versus Q, typically form a wide poi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::991de8f17e995c049aa81dc9dce475a0
https://doi.org/10.1002/essoar.10511268.1
https://doi.org/10.1002/essoar.10511268.1
Publikováno v:
Water Resources Research. 55:7275-7293
This data set accompanies the manuscript ‘Velocity Field Estimation on Density-Driven Solute Transport With a Convolutional Neural Network’. Concentration fields are stored as portable pixel maps (.ppm) and flow fields are stored in the Middlebur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e823500847fd06ecd6d9947cd63fa0f7
https://doi.org/10.1029/2019wr024833
https://doi.org/10.1029/2019wr024833
Publikováno v:
Vadose Zone Journal, Vol 19, Iss 1, Pp n/a-n/a (2020)
The description of soil water movement at the field scale requires soil hydraulic material properties. These cannot be measured directly and exhibit an intrinsic multiscale heterogeneity. The estimation of soil hydraulic properties through inverse mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8238cc77d7dd78a56789384999d6f686
https://doi.org/10.1002/vzj2.20040
https://doi.org/10.1002/vzj2.20040
Publikováno v:
Hydrology and Earth System Sciences, Vol 20, Iss 12, Pp 4999-5014 (2016)
The representation of soil water movement exposes uncertainties in all model components. We assess the key uncertainties for the specific hydraulic situation of a 1-D soil profile with TDR (time domain reflectometry)-measured water contents. The unce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bdf958ec0f5b0baa13453e918ea33c99
http://www.hydrol-earth-syst-sci.net/20/4999/2016/hess-20-4999-2016.pdf
http://www.hydrol-earth-syst-sci.net/20/4999/2016/hess-20-4999-2016.pdf