"Analysis of Fluctuations in the Stream Water Level during the Dry Seasons in Forested Areas" . . "Dvo\u0159\u00E1kov\u00E1, \u0160\u00E1rka" . . "Scientia Agriculturae Bohemica" . . . . "[378FA61A5AC1]" . "Analysis of Fluctuations in the Stream Water Level during the Dry Seasons in Forested Areas" . . "2"^^ . "Analysis of Fluctuations in the Stream Water Level during the Dry Seasons in Forested Areas"@en . . . "S" . "4" . "2"^^ . "CZ - \u010Cesk\u00E1 republika" . . . "Analysis of Fluctuations in the Stream Water Level during the Dry Seasons in Forested Areas"@en . . "0" . . . "RIV/60460709:41310/10:49039" . "246400" . . . . . "41" . "RIV/60460709:41310/10:49039!RIV11-MSM-41310___" . "drought, fluctuation levels, evaporation, forest respiration, dynamics of fluctuations, Thomson V Notched weir, discharge"@en . "41310" . "1211-3174" . "This is a description of temporal variation and development of stream flow in the open landscape, in the long-term summer droughts. The water level was scanned continuously several times a minute for several consecutive years. The analysis shows that the water discharge in the stream can be clearly divided into two components, a tributary to surface water and groundwater. While the surface component has a clear daily period, a component of groundwater is declining continuously, almost linearly. In the stream surface component adds to the total water discharge a gradual effect mini-peak levels at sunset and a sharp decline at sunrise. Time of culmination and its overall size with the ongoing drought days is developing. The peak always comes later and is still less pro-nounced."@en . "This is a description of temporal variation and development of stream flow in the open landscape, in the long-term summer droughts. The water level was scanned continuously several times a minute for several consecutive years. The analysis shows that the water discharge in the stream can be clearly divided into two components, a tributary to surface water and groundwater. While the surface component has a clear daily period, a component of groundwater is declining continuously, almost linearly. In the stream surface component adds to the total water discharge a gradual effect mini-peak levels at sunset and a sharp decline at sunrise. Time of culmination and its overall size with the ongoing drought days is developing. The peak always comes later and is still less pro-nounced." . . "7"^^ . "Zeman, Josef" . .