Climatic forcing of xylem formation in Qilian juniper on the northeastern Tibetan Plateau

Trees ◽  
2015 ◽  
Vol 30 (3) ◽  
pp. 923-933 ◽  
Author(s):  
Minhui He ◽  
Bao Yang ◽  
Zhangyong Wang ◽  
Achim Bräuning ◽  
Kambiz Pourtahmasi ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Climatic Forcing ◽  
Qilian Juniper ◽  
Northeastern Tibetan Plateau ◽  
Xylem Formation

scholarly journals Tectonic and climatic forcing of chemical weathering intensity in the northeastern Tibetan Plateau since the middle Miocene

CATENA ◽  
2022 ◽  
Vol 208 ◽  
pp. 105785
Author(s):  
Hanjing Fu ◽  
Xing Jian ◽  
Hanghai Liang ◽  
Wei Zhang ◽  
Xiaotian Shen ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Chemical Weathering ◽  
Middle Miocene ◽  
Climatic Forcing ◽  
Northeastern Tibetan Plateau ◽  
Weathering Intensity

scholarly journals Forward modeling analysis of regional scale tree-ring patterns around the northeastern Tibetan Plateau, Northwest China

2013 ◽  
Vol 10 (6) ◽  
pp. 9969-9988 ◽  
Author(s):  
X. Gou ◽  
F. Zhou ◽  
Y. Zhang ◽  
Q. Chen ◽  
J. Zhang
Keyword(s):  
Tibetan Plateau ◽  
Tree Ring ◽  
Tree Growth ◽  
Meteorological Data ◽  
Regional Scale ◽  
Growth Curves ◽  
Northwest China ◽  
Regional Patterns ◽  
Qilian Juniper ◽  
Northeastern Tibetan Plateau

Abstract. The process-based Vaganov–Shashkin (VS) model was used to simulate regional patterns of climate-tree growth relationships linking daily length, temperature and precipitation from meteorological data (AD 1957–2000) over the northeastern Tibetan Plateau (TP). The results exhibit that the leading principle component of the hypothetical growth curves is broadly consistent with that of the actual tree-ring chronologies, demonstrating the interpretability of the simulations as an accurate representation of the climatic controls on tree growth of Qilian Juniper. Output from this model both agrees well with the statistical relationships between tree-ring growth and climate factors as well as observational physiological behavior, i.e. precipitation in June acts as the most contributing role in annual ring formation of Qilian Juniper over the northeastern TP. The non-stationary and nonlinear response of tree growth to climate variability has important implications for calibration of tree-ring records for paleoclimate reconstructions and prediction for forest carbon sequestration.

Wind regime and aeolian landforms on the eastern shore of Qinghai Lake, Northeastern Tibetan Plateau, China

2021 ◽  
Vol 188 ◽  
pp. 104451
Author(s):  
Guangyin Hu ◽  
Zhibao Dong ◽  
Zhengcai Zhang ◽  
Linhai Yang ◽  
Lewei Hao ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Qinghai Lake ◽  
Eastern Shore ◽  
Wind Regime ◽  
Northeastern Tibetan Plateau
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