DOI: 10.5194/cp-14-57-2018
Scopus记录号: 2-s2.0-85040740079
论文题名: Autumn-winter minimum temperature changes in the southern Sikhote-Alin mountain range of northeastern Asia since 1529 AD
作者: Ukhvatkina O.N. ; Omelko A.M. ; Zhmerenetsky A.A. ; Petrenko T.Y.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2018
卷: 14, 期: 1 起始页码: 57
结束页码: 71
语种: 英语
Scopus关键词: autumn
; dendrochronology
; El Nino-Southern Oscillation
; global climate
; Northern Hemisphere
; Pacific Decadal Oscillation
; paleoclimate
; proxy climate record
; reconstruction
; solar cycle
; temperature anomaly
; winter
; China
; Japan
; Northeast Asia
; Pacific Ocean
; Pacific Ocean (North)
; Russian Far East
; Russian Federation
; Sikhote-Alin Range
英文摘要: The aim of our research was to reconstruct climatic parameters (for the first time for the Sikhote-Alin mountain range) and to compare them with global climate fluctuations. As a result, we have found that one of the most important limiting factors for the study area is the minimum temperatures of the previous autumn-winter season (August-December), and this finding perfectly conforms to that in other territories. We reconstructed the previous August-December minimum temperature for 485 years, from 1529 to 2014. We found 12 cold periods (1535-1540, 1550-1555, 1643-1649, 1659-1667, 1675-1689, 1722-1735, 1791-1803, 1807-1818, 1822-1827, 1836-1852, 1868-1887, 1911-1925) and seven warm periods (1560-1585, 1600-1610, 1614-1618, 1738-1743, 1756-1759, 1776-1781, 1944-2014). These periods correlate well with reconstructed data for the Northern Hemisphere and the neighboring territories of China and Japan. Our reconstruction has 3-, 9-, 20-, and 200-year periods, which may be in line with high-frequency fluctuations in El Niño-Southern Oscillation (ENSO), the short-term solar cycle, Pacific Decadal Oscillation (PDO) fluctuations, and the 200-year solar activity cycle, respectively. We suppose that the temperature of the North Pacific, expressed by the PDO may make a major contribution to regional climate variations. We also assume that the regional climatic response to solar activity becomes apparent in the temperature changes in the northern part of Pacific Ocean and corresponds to cold periods during the solar minimum. These comparisons show that our climatic reconstruction based on tree ring chronology for this area may potentially provide a proxy record for long-term, large-scale past temperature patterns for northeastern Asia. The reconstruction reflects the global traits and local variations in the climatic processes of the southern territory of the Russian Far East for more than the past 450 years. © Author(s) 2018. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109600
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
There are no files associated with this item.
作者单位: Federal Scientific Center, East Asia Terrestrial Biodiversity Far Eastern Branch, Russian Academy of Sciences, Vladivostok, 690022, Russian Federation
Recommended Citation:
Ukhvatkina O.N.,Omelko A.M.,Zhmerenetsky A.A.,et al. Autumn-winter minimum temperature changes in the southern Sikhote-Alin mountain range of northeastern Asia since 1529 AD[J]. Climate of the Past,2018-01-01,14(1)