: материалы временных коллективов / O. V. Gerasimova, O. V. Sidorova // Climate change and their impact on boreal and temperate forests: Abstracts of the International Conference (June 5-7, 2006, Ekaterinburg, Russia). - 2006. - С. 28
Держатели документа:
Институт леса им. В.Н. Сукачева Сибирского отделения Российской академии наук : 660036, Красноярск, Академгородок, 50, стр., 28
Доп.точки доступа:
Sidorova, Ol'ga; Сидорова, Ольга Владимировна; Герасимова, Оксана Владимировна
Имеются экземпляры в отделах:
РСФ (29.01.2008г. (1 экз.) - Б.ц.) - свободны 1
Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН
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Найдено документов в текущей БД: 3
Constructing the tree-ring chronology and reconstructing summertime air temperatures in southern Altai for the last 1500 years
/ V. S. Myglan [et al.] // Geogr. Nat. Resour. - 2012. - Vol. 33, Is. 3. - P200-207, DOI 10.1134/S1875372812030031
. - ISSN 1875-3728
Кл.слова (ненормированные):
Altai Republic -- palaeoclimate -- tree-ring chronologies -- upper timberline -- air temperature -- archaeological evidence -- climate variation -- deciduous tree -- dendrochronology -- paleoatmosphere -- paleoclimate -- reconstruction -- summer -- time series -- tree ring -- treeline -- wood -- Altay [Russian Federation] -- Russian Federation -- Larix -- Larix sibirica
Аннотация: We have constructed and analyzed the 1896-year-long tree-ring chronology for the territory of the Altai Republic. The chronology was based on wood of live trees and remains of trunks of Siberian larch (Larix sibirica Ledeb.) from the upper timberline (2300 m) of the Dzhelo river valley. The chronology agrees well with palaeoclimatic data and reflects the main climatic changes in the northern hemisphere for the last two millennia: an extraordinary decrease in increment after the year 536, "mean secular warming", the "Little Ice Age", and current warming. By calculating the response function between the tree-ring chronology for the Dzhelo and data from weather stations, it was possible to reconstruct the series of June-July air temperature variability for the last 1500 years. The chronology can be used in dating archaeological wood, i. e. in determining the calendar time at which archaeological monuments were constructed. В© 2012 Pleiades Publishing, Ltd.
Scopus
Держатели документа:
Siberian Federal University, Krasnoyarsk, Russian Federation
Altai State University, Barnaul, Russian Federation
Paul Scherrer Institute, Villigen, Switzerland
Доп.точки доступа:
Myglan, V.S.; Zharnikova, O.A.; Malysheva, N.V.; Gerasimova, O.V.; Vaganov, E.A.; Sidorov, O.V.
Кл.слова (ненормированные):
Altai Republic -- palaeoclimate -- tree-ring chronologies -- upper timberline -- air temperature -- archaeological evidence -- climate variation -- deciduous tree -- dendrochronology -- paleoatmosphere -- paleoclimate -- reconstruction -- summer -- time series -- tree ring -- treeline -- wood -- Altay [Russian Federation] -- Russian Federation -- Larix -- Larix sibirica
Аннотация: We have constructed and analyzed the 1896-year-long tree-ring chronology for the territory of the Altai Republic. The chronology was based on wood of live trees and remains of trunks of Siberian larch (Larix sibirica Ledeb.) from the upper timberline (2300 m) of the Dzhelo river valley. The chronology agrees well with palaeoclimatic data and reflects the main climatic changes in the northern hemisphere for the last two millennia: an extraordinary decrease in increment after the year 536, "mean secular warming", the "Little Ice Age", and current warming. By calculating the response function between the tree-ring chronology for the Dzhelo and data from weather stations, it was possible to reconstruct the series of June-July air temperature variability for the last 1500 years. The chronology can be used in dating archaeological wood, i. e. in determining the calendar time at which archaeological monuments were constructed. В© 2012 Pleiades Publishing, Ltd.
Scopus
Держатели документа:
Siberian Federal University, Krasnoyarsk, Russian Federation
Altai State University, Barnaul, Russian Federation
Paul Scherrer Institute, Villigen, Switzerland
Доп.точки доступа:
Myglan, V.S.; Zharnikova, O.A.; Malysheva, N.V.; Gerasimova, O.V.; Vaganov, E.A.; Sidorov, O.V.
Construction of 1772-year tree ring width chronology for altay republic
/ V. S. Myglan [и др.] // Izv. Akad. Nauk Ser. Geogr. - 2009. - Is. 6. - С. 70-77
. - ISSN 0373-2444
Кл.слова (ненормированные):
comparative study -- dating method -- geochronology -- Little Ice Age -- Medieval Warm Period -- paleoclimate -- tree ring -- Altai Mountains -- Larix -- Larix sibirica
Аннотация: For the first time a New 1772-year tree ring width chronology has been built for the Altay Mountain. The living trees and rest of stem wood of Siberian larch (Larix sibirica Ldb) were used from the upper tree line (2300 m) in Gelo valley. This chronology is coincidence with the paleoclimatic data and reflects basic climatic changes in the northern hemisphere for the last two millennia. We revealed extraordinary decreasing of tree radial growth after AD 536, "Medieval warming", "Little Ice Age", and current warming were revealed. The comparative analysis between Gelo and ALT tree ring chronologies has shown a good correlation in tree ring variability while revealing mismatch in response function of June-July air temperature. Such a long term chronology gives the possibility for dating of archeological wood to define the date of construction of archeological monuments.
Scopus
Держатели документа:
Siberian Federal University, Russian Federation
V.N. Sukachev Institute of Forest, SB RAS, Russian Federation
Altay State University, Russian Federation
Доп.точки доступа:
Myglan, V.S.; Ovchinnikov, D.V.; Vaganov, E.A.; Bykov, N.I.; Gerasimova, O.V.; Sidorova, O.V.; Silkin, P.P.
Кл.слова (ненормированные):
comparative study -- dating method -- geochronology -- Little Ice Age -- Medieval Warm Period -- paleoclimate -- tree ring -- Altai Mountains -- Larix -- Larix sibirica
Аннотация: For the first time a New 1772-year tree ring width chronology has been built for the Altay Mountain. The living trees and rest of stem wood of Siberian larch (Larix sibirica Ldb) were used from the upper tree line (2300 m) in Gelo valley. This chronology is coincidence with the paleoclimatic data and reflects basic climatic changes in the northern hemisphere for the last two millennia. We revealed extraordinary decreasing of tree radial growth after AD 536, "Medieval warming", "Little Ice Age", and current warming were revealed. The comparative analysis between Gelo and ALT tree ring chronologies has shown a good correlation in tree ring variability while revealing mismatch in response function of June-July air temperature. Such a long term chronology gives the possibility for dating of archeological wood to define the date of construction of archeological monuments.
Scopus
Держатели документа:
Siberian Federal University, Russian Federation
V.N. Sukachev Institute of Forest, SB RAS, Russian Federation
Altay State University, Russian Federation
Доп.точки доступа:
Myglan, V.S.; Ovchinnikov, D.V.; Vaganov, E.A.; Bykov, N.I.; Gerasimova, O.V.; Sidorova, O.V.; Silkin, P.P.