of Northern Spain as a Major Risk Factor for Forest Disease Patrick Schratz ([email protected]) November 7, 2016 Department of GIScience, University of Jena
It is important to swirl and sniff the wine, to unpack the complex bouquet and to appreciate the experience. Gulping the wine doesn’t work. ” Daniel B. Wright, 2003 P. Schratz November 7, 2016 1 / 36
affected by invasive pathogenic agents such as Diplodia pinea, Fusarium circinatum or Mycosphaerella spp. • Those pathogenic agents cause diseases like diplodia blight, pitch canker and needle blight resulting in forest decline (Iturritxa et al., 2014) P. Schratz November 7, 2016 2 / 36
affected by invasive pathogenic agents such as Diplodia pinea, Fusarium circinatum or Mycosphaerella spp. • Those pathogenic agents cause diseases like diplodia blight, pitch canker and needle blight resulting in forest decline (Iturritxa et al., 2014) • Wounds at trees are ”potential entry points for these diseases” (Smith et al., 2002) P. Schratz November 7, 2016 2 / 36
of pathogenic agents and subsequently forest decline Approach of this study: • Link surveyed ”hail damage to trees” to environmental variables to improve the understanding of forest decline in the Basque Country P. Schratz November 7, 2016 3 / 36
of pathogenic agents and subsequently forest decline Approach of this study: • Link surveyed ”hail damage to trees” to environmental variables to improve the understanding of forest decline in the Basque Country • Usage of linear and non-linear statistical learning methods to identify risk areas of hail damage to trees P. Schratz November 7, 2016 3 / 36
2015) of Bilbao, San Sebastian and Vitoria (Spain) showing mean temperature (°C, left) and total precipitation (mm/m2, right) by month. Data source: World Meteorological Organization (2016) P. Schratz November 7, 2016 6 / 36
2009-2012 • Variables • Hail damage [True/False] • Latitude, Longitude • Tree age [years] • Tree species • Year of acquisition • Evaluator information • Pathogenic agent [True/False] P. Schratz November 7, 2016 8 / 36
2009-2012 • Variables • Hail damage [True/False] • Latitude, Longitude • Tree age [years] • Tree species • Year of acquisition • Evaluator information • Pathogenic agent [True/False] Atlas Climatico Data Set • Long term observations (1951-1999) of meteorological stations • Spatial resolution: 200 m P. Schratz November 7, 2016 8 / 36
2009-2012 • Variables • Hail damage [True/False] • Latitude, Longitude • Tree age [years] • Tree species • Year of acquisition • Evaluator information • Pathogenic agent [True/False] Atlas Climatico Data Set • Long term observations (1951-1999) of meteorological stations • Spatial resolution: 200 m • Variables • Min/mean/max temperature (.1 °C) • Precipitation amount (.1 mm/m2) • PISR amount (kW/m2) • Data source: Ninyerola et al. (2005) P. Schratz November 7, 2016 8 / 36
years of daily observations • Stations • Bilbao • San Sebastian • Vitoria • Data source: World Meteorological Organization (2016) P. Schratz November 7, 2016 9 / 36
years of daily observations • Stations • Bilbao • San Sebastian • Vitoria • Data source: World Meteorological Organization (2016) • Variables • Min/mean/max temperature (.1 Fahrenheit) • Mean wind speed (.1 knots) • Precipitation amount (.01 inches) • Occurrence of hail P. Schratz November 7, 2016 9 / 36
years of daily observations • Stations • Bilbao • San Sebastian • Vitoria • Data source: World Meteorological Organization (2016) • Variables • Min/mean/max temperature (.1 Fahrenheit) • Mean wind speed (.1 knots) • Precipitation amount (.01 inches) • Occurrence of hail Digital Elevation Model • Spatial resolution: 25 m • Point density: 2 points/m • Data source: Euskadi (2013) P. Schratz November 7, 2016 9 / 36
Hail damage to trees • Type ’binomial’ -> Logit link function • Predictors (”Fixed effects”) • Minimum Temperature • Precipitation • Tree age • PISR P. Schratz November 7, 2016 12 / 36
Hail damage to trees • Type ’binomial’ -> Logit link function • Predictors (”Fixed effects”) • Minimum Temperature • Precipitation • Tree age • PISR • Grouping Structures ( = ”Mixed effects”) • Spatial Autocorrelation • Random effects • Evaluator information • Year of Aquisition P. Schratz November 7, 2016 12 / 36
density plots (spinograms here) of hail occurrence in relation to various climatic variables (daily observations) for the time period of 1973 - 2015 (November - April) of Vitoria. Y-axis shows the probability of hail occurrence for a given group of x. X-axis grouping according to histogram distribution of x. Temperature in °C, Precipitation in mm/m2, Wind Speed in km/h. P. Schratz November 7, 2016 16 / 36
scatterplots of predictors: Temperature (minimum), Precipitation amount, potential incoming solar radiation, elevation and tree age. P. Schratz November 7, 2016 18 / 36
and GLMM. Percentage increase of odds in parentheses. GLMM GAM Risk area Low High Very High Low High Very High Very Low 10.90 (990) 50.22 (4922) 125.36 (12436) 3.07 (207) 17.70 (1670) 154.94 (15394) Low - 4.60 (360) 11.50 (1050) - 5.77 (477) 50.47 (4947) High - 2.50 (150) - 8.76 (776) P. Schratz November 7, 2016 32 / 36
November - April • No long term increase of hail frequency • ~3x more hail in southern part of Basque Region (Vitoria) than at coast P. Schratz November 7, 2016 33 / 36
November - April • No long term increase of hail frequency • ~3x more hail in southern part of Basque Region (Vitoria) than at coast Statistical Modeling • Precipitation and temperature best predictors P. Schratz November 7, 2016 33 / 36
November - April • No long term increase of hail frequency • ~3x more hail in southern part of Basque Region (Vitoria) than at coast Statistical Modeling • Precipitation and temperature best predictors • Low importance of predictor ’tree age’ P. Schratz November 7, 2016 33 / 36
November - April • No long term increase of hail frequency • ~3x more hail in southern part of Basque Region (Vitoria) than at coast Statistical Modeling • Precipitation and temperature best predictors • Low importance of predictor ’tree age’ • No importance of predictor ’PISR’ P. Schratz November 7, 2016 33 / 36
November - April • No long term increase of hail frequency • ~3x more hail in southern part of Basque Region (Vitoria) than at coast Statistical Modeling • Precipitation and temperature best predictors • Low importance of predictor ’tree age’ • No importance of predictor ’PISR’ • Hail frequency != Hail intensity/damage P. Schratz November 7, 2016 33 / 36
November - April • No long term increase of hail frequency • ~3x more hail in southern part of Basque Region (Vitoria) than at coast Statistical Modeling • Precipitation and temperature best predictors • Low importance of predictor ’tree age’ • No importance of predictor ’PISR’ • Hail frequency != Hail intensity/damage • Model performances: ’poor’ to ’fair’ P. Schratz November 7, 2016 33 / 36
November - April • No long term increase of hail frequency • ~3x more hail in southern part of Basque Region (Vitoria) than at coast Statistical Modeling • Precipitation and temperature best predictors • Low importance of predictor ’tree age’ • No importance of predictor ’PISR’ • Hail frequency != Hail intensity/damage • Model performances: ’poor’ to ’fair’ • Highest risk areas of hail damage to trees in nothern part of Basque Country P. Schratz November 7, 2016 33 / 36
compare results • Integrate more climatic variables (e.g. wind speed) • Investigate non-convergence of spatial GAMM • Include biological variables representing tree properties • Tree health • Tree species P. Schratz November 7, 2016 34 / 36
compare results • Integrate more climatic variables (e.g. wind speed) • Investigate non-convergence of spatial GAMM • Include biological variables representing tree properties • Tree health • Tree species • Compare risk areas of hail damage to trees with risk areas of severe hail P. Schratz November 7, 2016 34 / 36
the assessment of prediction rules in remote sensing: the R package sperrorest. In 2012 IEEE International Geoscience and Remote Sensing Symposium (pp. 5372–5375). doi:10.1109/IGARSS.2012.6352393 Euskadi. (2013). LiDAR based 25m digital elevation model of the Basque region. Retrieved from ftp://ftp.geo.euskadi.net/lidar Fielding, A. H. (2007). Cluster and classification techniques for the biosciences. Iturritxa, E., Mesanza, N., & Brenning, A. (2014). Spatial analysis of the risk of major forest diseases in Monterey pine plantations. Plant Pathology, 64(4), 880–889. doi:10.1111/ppa.12328 James, G., Witten, D., Hastie, T., & Tibshirani, R. (2013). An introduction to statistical learning. Springer. Ninyerola, M., Pons, X., & Roure, J. (2005). Atlas climático digital de lapenínsula ibérica. metodología y aplicaciones en bioclimatología y geobotánica. Universidad Autónoma de Barcelona, Bellaterra. P. Schratz November 7, 2016 35 / 36
The role of latent Sphaeropsis Sapinea infections in post-hail associated die-back of Pinus Patula. Forest Ecology and Management, 164(1-3), 177–184. doi:10.1016/s0378-1127(01)00610-7 Snijders, T. & Bosker, R. (1991). An introduction to basic and advanced multilevel modelling. SAGE Publications Ltd, Thousand Oaks, CA. World Meteorological Organization. (2016). National Climatic Data Center (NCDC): Global Summary of [the] Day (GSOD) database [online accessed: 15/06/2016]. Retrieved from http://www7.ncdc.noaa.gov/CDO/cdoselect.cmd?datasetabbv= GSOD&countryabbv=&georegionabbv= Zuur, A. F., Ieno, E. N., Walker, N. J., Saveliev, A. A., & Smith, G. M. (2008). Mixed effects models and extensions in ecology with R. Springer. P. Schratz November 7, 2016 36 / 36
arara - https://github.com/cereda/arara (v3.0) Presentation mode: pdfpc - https://github.com/pdfpc/pdfpc (v.4.0.3) Created using the L ATEX beamer class P. Schratz November 7, 2016 36 / 36
long term hail distribution within the Basque Country • nner-yearly • Inter-yearly • Explore relations of environmental variables associated with hail • Temperature • Precipitation • Wind Speed Data set info: GSOD - Bilbao, San Sebastian, Vitoria - 43 years of daily observations - Hail / No hail
Inflation Factors • Pearson Correlations • Descriptive overview of variables Data set info: Atlas Climatico - SpRes: 200 m - Min. temperature - Precipitation - PISR Data set info: Tree Survey - 1168 observations - Hail damage to trees (T/F) - Tree age - Evaluator information - Year of aquisition
of GLM & GAM • Evaluate and account for sp. autocorrelation Random effects • Check for magnitude of random effects of GLM & GAM • Random intercept and StDev • Intraclass correlation • Evaluate and account for grouping structures
• Prediction area: Basque Country • Spatial Resolution: 200 m (Atlas Climatico data set) • Fix variables not available for prediction: Tree age • Prediction using population mean intercept Risk areas • Classify prediction area into risk areas • Risk levels: • Very-Low • Low • High • Very-High • Risk-level classification based on probability quartiles • Calculate odds ratios between risk areas
of numerical variables. Precipitation in m/m2, Temperature in °C, PISR in hW/m2, Tree Age in years. Statistics show Sample Size (n), Minimum (Min), 25% Quantile (q1 ), Median (~ x), Mean (~ x), 75% Quantile (q3 ), Maximum (Max), Inner-quartile range (IQR) and NA Count (#NA). Variable n Min q1 ~ x x q3 Max s IQR #NA precip 1168 0.047 0.119 0.138 0.132 0.146 0.152 0.019 0.028 0 temp 1168 0.917 3.250 3.983 3.964 4.783 6.917 1.080 1.533 0 srad 1168 0.009 0.012 0.014 0.014 0.014 0.018 0.002 0.002 0 age 1168 1.000 9.000 16.000 17.732 22.000 48.000 11.752 13.000 0
occur • odds = probability 1−probability • probability = odds 1+odds • Probability : [0, 1] • Odds : [−∞, +∞] Examples: • If the odds are 9:1 against you to reach the bus in time, this means you will miss the bus with a probability of 90% (in 9 of 10 cases). • Odds = 9/10 1−9/10 = 9 = 9:1 • Probability = 9/1 1+9/1 = 9 10 = 0.9
the predictor. The thick line represents the fitted regression line while the labeled lines represent the variation introduced by a random effect with 9 levels. Source: Zuur et al. (2008) • A random effect can be characterized as a grouping structure within variables which is assumed to rely on randomness. • This randomness can, for example, be introduced by different persons who collected survey data or by different acquisition locations/dates of data of the same type.
(Snijders & Bosker, 1991) • Quantifies correlation among the random effect groups • The higher the correlation, the higher the need to account for the random effect structure in the model d2 d2+σ2 , where d is the intercept standard deviation and σ the standard deviation of the residuals of the random effect