Description Usage Arguments Author(s) References
View source: R/TopoSUB_POSTcritSWC_fc_wp.R
Calculation of critical soil moisture levels dependent on soil parameterization, in particular on field capacity and wilting point (for details see Allen et al. 2010, Jasper et al. 2007).
1 | TopoSUB_POSTcritSWC_fc_wp(data, dry_thres = 30)
|
data |
zoo object of soil oisture data for X cluster centroids, coloumns correspond to the IDs in the listpoints file. |
dry_thres |
threshold defining severity of dryness, default = 30: 30 percent (severe dryness) of field capacity; 50: 50 percent (moderate dryness) of field capacity. |
Johannes Brenner, johannesbrenner@gmail.com
Allen, C. D., Macalady, A. K., Chenchouni, H., Bachelet, D., Mcdowell, N., Vennetier, M., <e2><80><a6> Cobb, N. (2010). A global overview of drought and heat-induced tree mortality reveals emerging climate change risks for forests. Forest Ecology and Management, 259(4), 660<e2><80><93>684. doi: 10.1016/j.foreco.2009.09.001
Jasper, K., Calanca, P., & Fuhrer, J. (2006). Changes in summertime soil water patterns in complex terrain due to climatic change. Journal of Hydrology, 327(3-4), 550<e2><80><93>563. doi: 10.1016/j.jhydrol.2005.11.061
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