The evolution of root-zone moisture capacities after deforestation: a step towards hydrological predictions under change?
dc.contributor.author | Nijzink, R. | en |
dc.contributor.author | Hutton, C. | en |
dc.contributor.author | Pechlivanidis, I. | en |
dc.contributor.author | Capell, R. | en |
dc.contributor.author | Arheimer, B. | en |
dc.contributor.author | Freer, J. | en |
dc.contributor.author | Han, D. | en |
dc.contributor.author | Wagener, T. | en |
dc.contributor.author | McGuire, Kevin J. | en |
dc.contributor.author | Savenije, H. | en |
dc.contributor.author | Hrachowitz, M. | en |
dc.contributor.department | Forest Resources and Environmental Conservation | en |
dc.contributor.department | Virginia Water Resources Research Center | en |
dc.date.accessioned | 2017-02-22T04:17:32Z | en |
dc.date.available | 2017-02-22T04:17:32Z | en |
dc.date.issued | 2016 | en |
dc.description.abstract | The core component of many hydrological systems, the moisture storage capacity available to vegetation, is impossible to observe directly at the catchment scale and is typically treated as a calibration parameter or obtained from a priori available soil characteristics combined with estimates of rooting depth. Often this parameter is considered to remain constant in time. Using long-term data (30–40 years) from three experimental catchments that underwent significant land cover change, we tested the hypotheses that: (1) the root-zone storage capacity significantly changes after deforestation, (2) changes in the root-zone storage capacity can to a large extent explain post-treatment changes to the hydrological regimes and that (3) a time-dynamic formulation of the root-zone storage can improve the performance of a hydrological model. A recently introduced method to estimate catchment-scale root-zone storage capacities based on climate data (i.e. observed rainfall and an estimate of transpiration) was used to reproduce the temporal evolution of root-zone storage capacity under change. Briefly, the maximum deficit that arises from the difference between cumulative daily precipitation and transpiration can be considered as a proxy for root-zone storage capacity. This value was compared to the value obtained from four different conceptual hydrological models that were calibrated for consecutive 2-year windows. It was found that water-balance-derived root-zone storage capacities were similar to the values obtained from calibration of the hydrological models. A sharp decline in root-zone storage capacity was observed after deforestation, followed by a gradual recovery, for two of the three catchments. Trend analysis suggested hydrological recovery periods between 5 and 13 years after deforestation. In a proof-of-concept analysis, one of the hydrological models was adapted to allow dynamically changing root-zone storage capacities, following the observed changes due to deforestation. Although the overall performance of the modified model did not considerably change, in 51% of all the evaluated hydrological signatures, considering all three catchments, improvements were observed when adding a time-variant representation of the root-zone storage to the model. In summary, it is shown that root-zone moisture storage capacities can be highly affected by deforestation and climatic influences and that a simple method exclusively based on climate data can not only provide robust, catchment-scale estimates of this critical parameter, but also reflect its timedynamic behaviour after deforestation. | en |
dc.format.extent | 4775 - 4799 page(s) | en |
dc.format.mimetype | application/pdf | en |
dc.identifier.doi | https://doi.org/10.5194/hess-20-4775-2016 | en |
dc.identifier.orcid | McGuire, Kevin J. [0000-0001-5751-3956] | en |
dc.identifier.uri | http://hdl.handle.net/10919/75114 | en |
dc.identifier.volume | 20 | en |
dc.language.iso | en | en |
dc.relation.uri | http://www.hydrol-earth-syst-sci.net/20/4775/2016/ | en |
dc.rights | In Copyright | en |
dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | en |
dc.title | The evolution of root-zone moisture capacities after deforestation: a step towards hydrological predictions under change? | en |
dc.title.serial | Hydrology and Earth System Sciences | en |
dc.type | Article - Refereed | en |
dc.type.dcmitype | Text | en |
pubs.organisational-group | /Virginia Tech | en |
pubs.organisational-group | /Virginia Tech/All T&R Faculty | en |
pubs.organisational-group | /Virginia Tech/Natural Resources & Environment | en |
pubs.organisational-group | /Virginia Tech/Natural Resources & Environment/CNRE T&R Faculty | en |
pubs.organisational-group | /Virginia Tech/Natural Resources & Environment/Water Resources Research Center | en |
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