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SED5, C562–C571, 2013
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Solid Earth Discuss., 5, C562–C571, 2013www.solid-earth-discuss.net/5/C562/2013/© Author(s) 2013. This work is distributed underthe Creative Commons Attribute 3.0 License.
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Interactive comment on “Seasonal changes of thesoil hydrological and erosive response incontrasted Mediterranean eco-geomorphologicalconditions at patch scale” byM. A. Gabarrón-Galeote et al.
M. A. Gabarrón-Galeote et al.
Received and published: 30 September 2013
According to the suggestion made by Professor Artemi Cerdà, the following improve-ments were done in the manuscript:
1. The suggestions of the referee concerning to the abstract were followed and henceit was shortened and displayed in one paragraph.
2. The expression “hydrological behavior” was removed when it appeared in themanuscript and it was substituted by “runoff generation”
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3. The last objective: “iv) to assess the influence of SWR on the soil hydrological anderosive response”, was deleted and it was incorporated to the first one.
4. Regarding the references suggested by the referee, most of them have been in-cluded. In some case it was not possible to find the combination of authors and dateproposed (e.g. Granged et al., 2013; Bodí et al., 2011b), but in this case anotherreference of the same author has been added.
5. A third season, called “dry season”, was added to the analysis. During this seasonno runoff was detected so only in results regarding soil water repellency some modifi-cations were done. However, the values corresponding to this season were added tothe tables and figures when it was possible. Moreover, some lines were added to thetext in order to highlight that this season was taken into account and an explanationfor the absence of runoff was added. Six times along the text, in the point 5.2, thereferee suggested to change transition into dry season. In my opinion, the sentenceseffectively refer to the transition season, so no change was added.
6. In the table 3 the values of rainfall, Intensity and maximum intensity has beenchanged. In the previous version only the events that generated runoff were takeninto account. In the new version the total values for all the events in the season weredisplayed.
7. The figures were modified and colors were added. The scale of the y-axis of Fig3 was changed to linear. The new manuscript is attached. Unfortunately I am notacquainted with Latex, so a doc version has been added.
Please also note the supplement to this comment:http://www.solid-earth-discuss.net/5/C562/2013/sed-5-C562-2013-supplement.pdf
Interactive comment on Solid Earth Discuss., 5, 1423, 2013.
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Discussion PaperFig. 1. Fig 1. Location of the experimental area and general view of both north and south-facinghillslopes
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Fig. 2. Fig 2. Daily precipitation (P), mean intensity (I) and maximum intensity (Imax) duringthe study period.
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Fig. 3. Fig 3. SWR measured on every microenvironment and season. Error bars repre-sent standard deviation. NIS: North-facing inter-shrub; NSC: North-facing shrub-covered; SIS:South-facing inter-shrub; SSC: S
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Fig. 4. Fig 4. Mean values of runoff rate and coefficient in every microenvironment and sea-son. Error bars represent standard deviation. NIS: North-facing inter-shrub; NSC: North-facingshrub-covered; SIS: So
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Fig. 5. Fig 5. Relation between Imax and runoff rate in every microenvironment. NIS: North-facing inter-shrub; NSC: North-facing shrub-covered; SIS: South-facing inter-shrub; SSC:South-facing shrub-covered.
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Fig. 6. Fig 6. Relation between runoff coefficient and precipitation. NIS: North-facing inter-shrub; NSC: North-facing shrub-covered; SIS: South-facing inter-shrub; SSC: South-facingshrub-covered.
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Fig. 7. Fig 7. Relation between runoff coefficient and Imax. NIS: North-facing inter-shrub; NSC:North-facing shrub-covered; SIS: South-facing inter-shrub; SSC: South-facing shrub-covered.
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Fig. 8. Fig 8. Mean values of sediment concentration and soil loss in every microenvironmentand season. Error bars represent standard deviation. NIS: North-facing inter-shrub; NSC:North-facing shrub-covered
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