Построение тысячелетних древесно-кольцевых хронологий Koksu и Tara для территории Алтая

800x600 The work presents two new 1000-year tree-ring chronologies: Tara (AD 795-2011, the South Chui Range) and Koksu (AD 588-2011, the Katun Range). The calculation of the response function shows that the dominating factor for the radial growth of the tree-ring chronology Koksu is June and July temperature, for Tara is June temperature. The strong correlation between Koksu chronology and meteorological station record in the Northern Mongolia and China at a distance of 300 or more kilometers from the sites of sample collection illustrates summer temperature change at least on a regional scale. At the same time Tara chronology is weakly sensitive to changes in summer temperatures and may be used for dating of geomorphologic, historical and climatic events. Normal 0 false false false RU X-NONE X-NONE /* Style Definitions */ table.MsoNormalTable {mso-style-name:"Обычная таблица"; mso-tstyle-rowband-size:0; mso-tstyle-colband-size:0; mso-style-noshow:yes; mso-style-priority:99; mso-style-parent:""; mso-padding-alt:0cm 5.4pt 0cm 5.4pt; mso-para-margin:0cm; mso-para-margin-bottom:.0001pt; mso-pagination:widow-orphan; font-size:10.0pt; font-family:"Calibri","sans-serif"; mso-bidi-font-family:"Times New Roman";}