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Seasonality in Na/Cl ratios in precipitation and throughfall samples. Karin Hansen, Anne Thimonier, Peter Waldner , Maria Schmitt, Flurin Sutter, Ülle Napa, Lars Vesterdal, Arne Verstraeten, Sue Benham. ……..an on-going project with preliminary results. Background for this study.
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Seasonality in Na/Cl ratios in precipitation and throughfall samples Karin Hansen, Anne Thimonier, Peter Waldner, Maria Schmitt, Flurin Sutter, Ülle Napa, Lars Vesterdal, Arne Verstraeten, Sue Benham ……..an on-going projectwithpreliminaryresults
Background for this study • Thimonier, A., Schmitt, M., Waldner, P., Schleppi, P. (2008). Seasonality of the Na/Cl ratio in precipitation and implications of canopy leaching in validating chemical analyses of throughfall samples. Atmospheric Environment 42: 9106-9117.
Hypotheses • A portion of Na/Cl ratios in throughfall in Europe fall outside the recommended range of 0.5-1.5; • Leaching of Na and Cl from forest canopies do occur in the autumn or spring; • Leaching is highest from deciduous tree species; • The seasonality in leaching is connected to the distance from the nearest sea.
Research questions • Is there a seasonal pattern to the leaching of Na and Cl? • Can Na and Cl be said to be inert in forest canopies? • Do certain tree species leach more Na or Cl than others? • Is the seasonal pattern in any relation to how far away from the sea the forest stand is situated?
Data used in the study • ICP Forests database • Bulk precipitation (BP) • Throughfall (TF) • Tree species • Criteria implemented on an annual basis • sampling during at least 300 days • gaps between sampling periods < 50 days • Na and Cl values for at least 300 days • Calculated distance to the nearest sea
Statistics The seasonalitywithin the data was analysed by introducingharmonic terms (sine and cosine) in a stepwise regression of the dependent variable x versus time: x = c1 + c2 sin t + c3 cos t + c4 sin 2t + c5 cos 2t + c6 sin 3t + c7 cos 3t + c8 sin 4t + c9 cos 4t + c10 sin 5t + c11 cos 5t Where t=2π/365 * (day of the year) and c1–c11 are regression coefficients.
Determination of distance to the sea • The longitude and latitude as submittedto the ICP Forests Database in the format DDMMSS translatedinto decimal degrees • The Europeancountriesavailable from the EDIT geoplatform (http://edit.csic.es/AdministrativeUnits.html)weremergedto a continentand transformed from polygon to a polyline • Plotcoordinates and country boundaryswere imported into ESRI ArcGIS 10.1 using the WGS1984 coordinatereferencesystem and the distancewascalculatedwith the Analyses Tool'near’.
Some preliminary results – Na/Cl in BP GermanyPlot 1601, R2=0.46 (P<0.0001)
Some preliminary results – Na/Cl in TF FrancePlot 16, R2=0.68 (P<0.0001)
Some preliminary results - TF United KingdomPlot 516, R2=0.64 (P<0.0001)
Somepreliminaryresults and conclusions (1) • For bulk precipitation (BP) • 81 plots (outof 438 plots) hadsignificant (p<0.0001) seasonalpatterns for the Na/Clratio • Explaining from 0-46% of the variation (R2) • For throughfall (TF) • 188 plots(outof 438 plots) hadsignificant (p<0.0001) seasonalpatterns for the Na/Clratio • Explaining from 0-68% of the variation (R2) • Significant seasonality was observed in both bulk precipitation and throughfall Na/Cl ratios • Throughfall showed significant seasonality more often and the explanation of it was stronger than for bulk precipitation
Somepreliminaryresults and conclusions (2) • 63 deciduous ( R2=0.14-0.68) showedsignificant (p<0.0001) seasonalpatterns. • 119 coniferousstands (R2=0-0.55) showedsignificant (p<0.0001) seasonalpatterns. • No straight forward relationship wasobservedbetweentree species groups (deciduous and coniferous) and the seasonalpattern.
Work to be done still (1) • Analysing data will continue during the coming months. • Which plots have and which do not have clear seasonal patterns? • The seasonal patterns are in part hampered by quality problems in data • Weneedtoclearout data withquality problems
Work to be done still (2) • We are looking into the possibilities to calculate a 'direction weighted distance to the sea. • The difficulties are to get information on how to weight the directions to different seas and how to model and include the wind directions as a weight. • Areal data of the wind direction would be needed.
Work to be done still (2) • We will look further into the possibility for different tree species to affect the seasonal pattern in throughfall. • Communication to and feedback from people in charge of deposition measurements in the countries that are included in this study. • Aiming at a publication in the beginning of 2014 (Atmospheric Environment)