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SiO2 8 hours?
INTERACTIVE COMMENT ON HYDROL. EARTH SYST. SCI. DISCUSS a model such as Model I, sediment yield would be measured over each 15-minute storm interval and plotted against the corresponding intensity during that storm, but HYDROLOGY AND INTERACTIVE COMMENT ON “A NOVEL ALGORITHM HESSD 7, C221–C222, 2010 Interactive Comment Full Screen / Esc Printer-friendly Version Interactive Discussion Discussion Paper Hydrol. Earth Syst. Sci. Discuss., 7, C221–C222, 2010 INTERACTIVE COMMENT ON HYDROL. EARTH SYST. SCI. DISCUSS Hydrol. Earth Syst. Sci. Discuss., doi:10.5194/hess-2016-117-RC2, 2016 © Author(s) 2016. CC-BY 3.0 License. Interactive comment on Peakriver ows in cold
INTERACTIVE COMMENT ON ASSESSING THE SOURCES OF "P. 3459, lines 1-2. Possible and relevant errors on the daily precipitation provided by the INM stations are mentioned but not takeninto account.
ARDENNES MASSIF, AND ITS LINK WITH TECTONICS CHANNEL AND a more clear idea of the main river network should be given (maybe a map with the river network overlapped to a shaded relief map). P6985line 17-18.
AND A DIFFUSIVE TERM ( I think one has to separate the advection and the exchange (the dispersion). The exchange is responsible for the dispersion. ν is the proportion of tidal mixing to total mixing, or of tidal exchange INTERACTIVE COMMENT ON “INFLUENCE OF BY HESSD 6, S572–S579, 2009 Interactive Comment Full Screen / Esc Printer-friendly Version Interactive Discussion Discussion Paper Hydrol. Earth Syst. Sci. Discuss., 6, S572–S579, 2009 BY WIRELESS SENSOR NETWORK BY METHOD TO INTERPOLATE SOIL curves (Figs. 10 and 11) show more than ve sampling points. Theoretically, all days of the investigation period need to be interpolated. Is it possible to apply this method BASE OW SEPARATION METHODS IN A LOWLAND INTERACTIVE Figure 5 - legend: difcult to differentiate the line types of Ca and Mg. At what time resolution were these samples taken? Mg, Ca 4 hours,SiO2 8 hours?
INTERACTIVE COMMENT ON HYDROL. EARTH SYST. SCI. DISCUSS a model such as Model I, sediment yield would be measured over each 15-minute storm interval and plotted against the corresponding intensity during that storm, but HYDROLOGY AND INTERACTIVE COMMENT ON “A NOVEL ALGORITHM HESSD 7, C221–C222, 2010 Interactive Comment Full Screen / Esc Printer-friendly Version Interactive Discussion Discussion Paper Hydrol. Earth Syst. Sci. Discuss., 7, C221–C222, 2010 INTERACTIVE COMMENT ON HYDROL. EARTH SYST. SCI. DISCUSS Hydrol. Earth Syst. Sci. Discuss., doi:10.5194/hess-2016-117-RC2, 2016 © Author(s) 2016. CC-BY 3.0 License. Interactive comment on Peakriver ows in cold
INTERACTIVE COMMENT ON ASSESSING THE SOURCES OF "P. 3459, lines 1-2. Possible and relevant errors on the daily precipitation provided by the INM stations are mentioned but not takeninto account.
ARDENNES MASSIF, AND ITS LINK WITH TECTONICS CHANNEL AND a more clear idea of the main river network should be given (maybe a map with the river network overlapped to a shaded relief map). P6985line 17-18.
AND A DIFFUSIVE TERM ( I think one has to separate the advection and the exchange (the dispersion). The exchange is responsible for the dispersion. ν is the proportion of tidal mixing to total mixing, or of tidal exchange HYDROLOGY AND INTERACTIVE COMMENT ON “A NOVEL ALGORITHM HESSD 7, C221–C222, 2010 Interactive Comment Full Screen / Esc Printer-friendly Version Interactive Discussion Discussion Paper Hydrol. Earth Syst. Sci. Discuss., 7, C221–C222, 2010 INTERACTIVE COMMENT ON HYDROL. EARTH SYST. SCI. DISCUSS Hydrol. Earth Syst. Sci. Discuss., doi:10.5194/hess-2016-117-RC2, 2016 © Author(s) 2016. CC-BY 3.0 License. Interactive comment on Peakriver ows in cold
1. GENERAL COMMENTS
3 Secondly, the authors propose an empirical relationship betweenQ andK according to Eq. (S6). To my view this is only to mask the fact that 1/K andQ have non- overlapping ranges (1/K > 1 and 0Details
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