TY - JOUR
T1 - Predicting Ellenberg's soil moisture indicator value in the Bavarian Alps using additive georegression
AU - Häring, Tim
AU - Reger, Birgit
AU - Ewald, Jörg
AU - Hothorn, Torsten
AU - Schröder, Boris
PY - 2013/1
Y1 - 2013/1
N2 - Questions: Can forest site characteristics be used to predict Ellenberg indicator values for soil moisture? Which is the best averaged mean value for modelling? Does the distribution of soil moisture depend on spatial information? Location: Bavarian Alps, Germany. Methods: We used topographic, climatic and edaphic variables to model the mean soil moisture value as found on 1505 forest plots from the database WINALPecobase. All predictor variables were taken from area-wide geodata layers so that the model can be applied to some 250 000 ha of forest in the target region. We adopted methods developed in species distribution modelling to regionalize Ellenberg indicator values. Therefore, we use the additive georegression framework for spatial prediction of Ellenberg values with the R-library mboost, which is a feasible way to consider environmental effects, spatial autocorrelation, predictor interactions and non-stationarity simultaneously in our data. The framework is much more flexible than established statistical and machine-learning models in species distribution modelling. We estimated five different mboost models reflecting different model structures on 50 bootstrap samples in each case. Results: Median R2 values calculated on independent test samples ranged from 0.28 to 0.45. Our results show a significant influence of interactions and non-stationarity in addition to environmental covariates. Unweighted mean indicator values can be modelled better than abundance-weighted values, and the consideration of bryophytes did not improve model performance. Partial response curves indicate meaningful dependencies between moisture indicator values and environmental covariates. However, mean indicator values <4.5 and >6.0 could not be modelled correctly, since they were poorly represented in our calibration sample. The final map represents high-resolution information of site hydrological conditions. Conclusions: Indicator values offer an effect-oriented alternative to physically-based hydrological models to predict water-related site conditions, even at landscape scale. The presented approach is applicable to all kinds of Ellenberg indicator values. Therefore, it is a significant step towards a new generation of models of forest site types and potential natural vegetation. Ellenberg soil moisture indicator values have been used to predict soil hydrological conditions in the Bavarian Alps following the approach of predictive vegetation mapping. Additive georegression has been used as modeling approach. Indicator values offer an effect-oriented alternative to physically-based hydrological models to predict water related site conditions, even on landscape scale.
AB - Questions: Can forest site characteristics be used to predict Ellenberg indicator values for soil moisture? Which is the best averaged mean value for modelling? Does the distribution of soil moisture depend on spatial information? Location: Bavarian Alps, Germany. Methods: We used topographic, climatic and edaphic variables to model the mean soil moisture value as found on 1505 forest plots from the database WINALPecobase. All predictor variables were taken from area-wide geodata layers so that the model can be applied to some 250 000 ha of forest in the target region. We adopted methods developed in species distribution modelling to regionalize Ellenberg indicator values. Therefore, we use the additive georegression framework for spatial prediction of Ellenberg values with the R-library mboost, which is a feasible way to consider environmental effects, spatial autocorrelation, predictor interactions and non-stationarity simultaneously in our data. The framework is much more flexible than established statistical and machine-learning models in species distribution modelling. We estimated five different mboost models reflecting different model structures on 50 bootstrap samples in each case. Results: Median R2 values calculated on independent test samples ranged from 0.28 to 0.45. Our results show a significant influence of interactions and non-stationarity in addition to environmental covariates. Unweighted mean indicator values can be modelled better than abundance-weighted values, and the consideration of bryophytes did not improve model performance. Partial response curves indicate meaningful dependencies between moisture indicator values and environmental covariates. However, mean indicator values <4.5 and >6.0 could not be modelled correctly, since they were poorly represented in our calibration sample. The final map represents high-resolution information of site hydrological conditions. Conclusions: Indicator values offer an effect-oriented alternative to physically-based hydrological models to predict water-related site conditions, even at landscape scale. The presented approach is applicable to all kinds of Ellenberg indicator values. Therefore, it is a significant step towards a new generation of models of forest site types and potential natural vegetation. Ellenberg soil moisture indicator values have been used to predict soil hydrological conditions in the Bavarian Alps following the approach of predictive vegetation mapping. Additive georegression has been used as modeling approach. Indicator values offer an effect-oriented alternative to physically-based hydrological models to predict water related site conditions, even on landscape scale.
KW - Boosting
KW - Mboost
KW - Non-stationarity
KW - Predictive vegetation mapping
KW - Site ecology
KW - Species distribution modelling
UR - http://www.scopus.com/inward/record.url?scp=84872419143&partnerID=8YFLogxK
U2 - 10.1111/j.1654-109X.2012.01210.x
DO - 10.1111/j.1654-109X.2012.01210.x
M3 - Article
AN - SCOPUS:84872419143
SN - 1402-2001
VL - 16
SP - 110
EP - 121
JO - Applied Vegetation Science
JF - Applied Vegetation Science
IS - 1
ER -