DOI: 10.1016/j.gloplacha.2016.04.010
论文题名: Reconstruction of biological drought conditions during the past 2847 years in an alpine environment of the northeastern Tibetan Plateau, China, and possible linkages to solar forcing
作者: Yin Z.-Y. ; Zhu H. ; Huang L. ; Shao X.
刊名: Global and Planetary Change
ISSN: 0921-8181
出版年: 2016
卷: 143 起始页码: 214
结束页码: 227
语种: 英语
英文关键词: Droughts
; Northeastern Tibetan Plateau
; Tree ring widths
; Water balance modeling
Scopus关键词: Atmospheric thermodynamics
; Drought
; Forestry
; Solar energy
; Solar radiation
; Transfer functions
; Water management
; Moisture conditions
; Negative correlation
; Northeastern tibetan plateaux
; Oxygen stable isotopes
; Thornthwaite water balance models
; Tree-ring chronologies
; Tree-ring width
; Water balance models
; Moisture
; alpine environment
; data set
; drought
; Little Ice Age
; moisture content
; oxygen
; paleoclimate
; reconstruction
; solar activity
; solar power
; stable isotope
; tree ring
; water budget
; China
; Qaidam Basin
; Qinghai
; Qinghai-Xizang Plateau
; Juniperus
英文摘要: In this study we reconstructed the moisture condition of the eastern Qaidam Basin of the northeastern Tibetan Plateau based on a 3585-year tree ring chronology. The growth environment of Qilian juniper (Sabina przewalskii Kom.) on the mountains in the eastern Qaidam Basin was first determined by comparing precipitation and temperature estimates from two spatial datasets (PRISM and World Climate). Moisture balance was calculated as the sum of simulated moisture deficit (negative) and surplus using a modified Thornthwaite water balance model, and used as a proxy of biological drought conditions. Using data during 1956–2005, we established the transfer function to reconstruct a 2847-year series of January–June moisture balance (843 BCE–2004 CE). With an adjusted R2 value of 0.654 of the transfer function and strong performance in validation, the reconstructed January–June moisture balance can be considered an excellent indicator of biological drought conditions for the study region. The reconstructed series showed strong correlations with reconstructed PDSI in the monsoon Asian region, representing a region of 10° latitudes by 20° longitudes. Using the reconstructed series, we identified centennial-scale dry periods since 843 BCE: 381–277 BCE, 425–520 CE, 1108–1212 CE, 1428–1516 CE, and 1634–1743 CE. Additionally it had statistically significant negative correlations with a monsoon intensity proxy based on oxygen stable isotope from southwestern China (Dongge Cave). Further analyses identified significant relationships with solar activity, especially during the last 700 years. We confirmed the ~ 200-year cyclic pattern in the reconstructed moisture balance series, which matched the known 210-year de Vries solar cycle and peaked during the Little Ice Age. However, the cyclic patterns of the reconstructed moisture balance series and solar activity were decoupled for the period prior to approx. 1300 CE. © 2016 Elsevier B.V.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84976543221&doi=10.1016%2fj.gloplacha.2016.04.010&partnerID=40&md5=860407b8796f3c3d6bdf4a86ed3a4d3b
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11648
Appears in Collections: 全球变化的国际研究计划 气候变化与战略
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作者单位: Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
Recommended Citation:
Yin Z.-Y.,Zhu H.,Huang L.,et al. Reconstruction of biological drought conditions during the past 2847 years in an alpine environment of the northeastern Tibetan Plateau, China, and possible linkages to solar forcing[J]. Global and Planetary Change,2016-01-01,143.