<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>27</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Schweingruber, Fritz H.</style></author><author><style face="normal" font="default" size="100%">Kontic, Raymond</style></author><author><style face="normal" font="default" size="100%">Winkler-Seifert, Amanda</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Eine jahrringanalytische Studie zum Nadelbaumsterben in der Schweiz</style></title><secondary-title><style face="normal" font="default" size="100%">Berichte Rapports</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">climate</style></keyword><keyword><style  face="normal" font="default" size="100%">damages</style></keyword><keyword><style  face="normal" font="default" size="100%">environment</style></keyword><keyword><style  face="normal" font="default" size="100%">fir</style></keyword><keyword><style  face="normal" font="default" size="100%">growth</style></keyword><keyword><style  face="normal" font="default" size="100%">growth reduction</style></keyword><keyword><style  face="normal" font="default" size="100%">pollution</style></keyword><keyword><style  face="normal" font="default" size="100%">Switzerland</style></keyword><keyword><style  face="normal" font="default" size="100%">tree ring</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1983</style></year><pub-dates><date><style  face="normal" font="default" size="100%">08/1983</style></date></pub-dates></dates><publisher><style face="normal" font="default" size="100%">Eidgenossische Anstalt fur das Forstliche Versuchswesen</style></publisher><pub-location><style face="normal" font="default" size="100%">Birmensdorf</style></pub-location><abstract><style face="normal" font="default" size="100%">Application of annual ring analysis in investigations of conifer die-back in Switzerland

Obviously unhealthy confiders show abrupt tree-ring growth reductions which are datable without measurements.  By investigation of large amount of samples on different sites in Switzerland we calculated the areal distribution of damaged trees and the damage occurrence within time.  Geographical distribution and time patterns yield to relations between climatic and pollution events.  The heavy damages on fir started in Switzerland 1956.  Approximately 75% of all firs in Switzerland's central plateau show growth reductions.  Local damages exist in the Rhone-valley since 1920. </style></abstract><issue><style face="normal" font="default" size="100%">253</style></issue><notes><style face="normal" font="default" size="100%">Copies of this are available through the Tree Ring Laboratory; please contact the lab for more information. 

This edition of the reports is from the Swiss Federal Institute of Forestry Research. </style></notes></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">LaMarche, V.C.</style></author><author><style face="normal" font="default" size="100%">Fritts, H.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Tree Rings, Glacial Advance, And Climate in The Alps</style></title><secondary-title><style face="normal" font="default" size="100%">Zeitschrift fur Gletscherkunde und Glazialgeologie</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">alps</style></keyword><keyword><style  face="normal" font="default" size="100%">austria</style></keyword><keyword><style  face="normal" font="default" size="100%">climatology</style></keyword><keyword><style  face="normal" font="default" size="100%">environment</style></keyword><keyword><style  face="normal" font="default" size="100%">glacial advance</style></keyword><keyword><style  face="normal" font="default" size="100%">glaciers</style></keyword><keyword><style  face="normal" font="default" size="100%">Switzerland</style></keyword><keyword><style  face="normal" font="default" size="100%">tree ring</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1971</style></year></dates><volume><style face="normal" font="default" size="100%">VII</style></volume><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Ring-width variations in stone pine near upper treeline in the Alps show a high negative correlation with the percentage of advancing glaciers in Austria and Switzerland. The relationship is due to the similarity of climatic models for tree growth and the glacial mass budget. Tree-ring fluctuations during the period 1800-1889, prior to the compilation of glacial statistics show good agreement with historical glacial advances and periods of low summer temperatures, especially around 1820-1855. Tree-ring studies could assist in reconstructing the glacial and climatic history of the Alps, possibly for a period of 1,000 years or more.&lt;/p&gt;</style></abstract><notes><style face="normal" font="default" size="100%">&lt;p&gt;Copies of this are available through the Tree Ring Laboratory; please contact the lab for more information.&lt;/p&gt;</style></notes></record></records></xml>