Response to “Comment on ‘Soil Moisture Response to Snowmelt and Rainfall in a Sierra Nevada Mixed‐Conifer Forest’” | Zendy

Hopmans Jan W. | Zendy; Bales R.C. | Zendy; O'Geen A.T. | Zendy; Hunsaker C.T. | Zendy; Beaudette D. | Zendy; Hartsough P.C. | Zendy; Malazian A. | Zendy; Kirchner P. | Zendy; Meadows M. | Zendy

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Response to “Comment on ‘Soil Moisture Response to Snowmelt and Rainfall in a Sierra Nevada Mixed‐Conifer Forest’”

Author(s) -

Hopmans Jan W.,

Bales R.C.,

O'Geen A.T.,

Hunsaker C.T.,

Beaudette D.,

Hartsough P.C.,

Malazian A.,

Kirchner P.,

Meadows M.

Publication year - 2012

Publication title -

vadose zone journal

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 1.036

H-Index - 81

ISSN - 1539-1663

DOI - 10.2136/vzj2012.0004r

Subject(s) - snowmelt , environmental science , hydrology (agriculture) , forestry , geography , geology , snow , meteorology , geotechnical engineering

We appreciate the comments by [Graham and Hubbert (2012)][1] regarding our finding ([Bales et al., 2011][2]) that water stored in deeper soils and weathered granitic rock (regolith) provides a significant fraction of water for forest evapotranspiration. Our multi-year hydrologic measurements confirm

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