Add to ORKGTwo types of hysteresis loops have been observed on Goodwin Creek: those with a greater flow depth for a given discharge on the falling limb of the hydrograph (type 1) and those with a greater flow depth for a given discharge on the rising limb of the hydrograph (type 2). Causes of these 2 loop types are investigated in this paper
Bankfull hydraulic geometry relationships relate bankfull stream dimensions, such as cross-sectional...
This discussion paper has been under review for the journal Hydrology and Earth System Sciences (HES...
2014 S.C. Water Resources Conference - Informing Strategic Water Planning to Address Natural Resourc...
Two types of hysteresis loops have been observed on Goodwin Creek: those with a greater flow depth f...
International audienceThe study of flood dynamics is generally complicated because it requires a lot...
SummarySediment concentration (SC)–water discharge (Q) relations in rivers are typically governed by...
Hydraulic bankfull geometry or regional curves are a useful metric for evaluating stream stability a...
The concentration of suspended sediment and discharge generated during flood events are not normally...
Proceedings of the 2007 Georgia Water Resources Conference, March 27-29, 2007, Athens, Georgia.The r...
Data compiled from standardized procedures for width measurement at established streamflow gaging st...
Differential parametric values associated with bed load sediment transport, that result at the same ...
While most hydrological models reproduce the general flow dynamics, they frequently fail to adequate...
While most hydrological models reproduce the general flow dynamics, they frequently fail to adequate...
I would like to thank the authors for writing this interesting article dealing with unsteady stage-...
While most hydrological models reproduce the general flow dynamics, they frequently fail to adequate...
Bankfull hydraulic geometry relationships relate bankfull stream dimensions, such as cross-sectional...
This discussion paper has been under review for the journal Hydrology and Earth System Sciences (HES...
2014 S.C. Water Resources Conference - Informing Strategic Water Planning to Address Natural Resourc...
Two types of hysteresis loops have been observed on Goodwin Creek: those with a greater flow depth f...
International audienceThe study of flood dynamics is generally complicated because it requires a lot...
SummarySediment concentration (SC)–water discharge (Q) relations in rivers are typically governed by...
Hydraulic bankfull geometry or regional curves are a useful metric for evaluating stream stability a...
The concentration of suspended sediment and discharge generated during flood events are not normally...
Proceedings of the 2007 Georgia Water Resources Conference, March 27-29, 2007, Athens, Georgia.The r...
Data compiled from standardized procedures for width measurement at established streamflow gaging st...
Differential parametric values associated with bed load sediment transport, that result at the same ...
While most hydrological models reproduce the general flow dynamics, they frequently fail to adequate...
While most hydrological models reproduce the general flow dynamics, they frequently fail to adequate...
I would like to thank the authors for writing this interesting article dealing with unsteady stage-...
While most hydrological models reproduce the general flow dynamics, they frequently fail to adequate...
Bankfull hydraulic geometry relationships relate bankfull stream dimensions, such as cross-sectional...
This discussion paper has been under review for the journal Hydrology and Earth System Sciences (HES...
2014 S.C. Water Resources Conference - Informing Strategic Water Planning to Address Natural Resourc...