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Reconstruction Dataset of Yearly Mean Temperature in June-July at Western Sichuan Plateau of China using Tree-ring Width (1383-2005)


LI Jinjian1ZHANG Yu1SHAO Xuemei2LI Mingqi2
1 School of Atmospheric Sciences,ChengduUniversity of Information Technology,Chengdu 610225,China2 Institute of Geographic Sciences andNatural Resources Research,ChineseAcademy of Sciences,Beijing100101,China

DOI:10.3974/geodb.2022.02.03.V1

Published:Feb. 2022

Visitors:1672       Data Files Downloaded:27      
Data Downloaded:53.36 MB      Citations:

Key Words:

Tree ring,Western Sichuan Plateau,Temperature,1383-2005,

Abstract:

The Picea balfouriana tree rings from Baiyu County (99.81°E,31.15°N), Western Sichuan Plateau were collected in October 2017, and the standardized chronology was calculated after processing the tree ring width chronology with ARSTAN and COFFECHA programs. The authors reconstructed yearly summer (June-July) mean temperature back to 1383 for the region based on a significant positive correlation between the standard chronology and summer temperature. The dataset includes: (1) geo-location data of the sample site; (2) reconstruction data of yearly mean temperature in Western Sichuan Plateau from June to July over the period of 1383-2005; (3) the mean meteorological temperature data of Western Sichuan Plateau from June to July during 1962-2005; (4) some photos. The dataset is archived in .shp, .xlsx and .jpg data formats, and consists of 9 data files with data size of 2.10 MB (Compressed into one file with 1.97 MB). The analysis paper based on the dataset was published at International Journal of Climatology (2021).

Foundation Item:

Ministry of Science and Technology of P. R. China (2017YFA0603302);

Data Citation:

LI Jinjian, ZHANG Yu, SHAO Xuemei, LI Mingqi. Reconstruction Dataset of Yearly Mean Temperature in June-July at Western Sichuan Plateau of China using Tree-ring Width (1383-2005)[J/DB/OL]. Digital Journal of Global Change Data Repository, 2022. https://doi.org/10.3974/geodb.2022.02.03.V1.

References:

[1] Kaser, G., Hardy, D. R., M?lg, T., et al. Modern glacier retreat on Kilimanjaro as evidence of climate change: observations and facts [J]. International Journal of Climatology, 2004, 24: 329-339.
     [2] Fritts, H. C. Tree rings and climate [M]. London: Academic Press, 1976, 30-265.
     [3] Cook, E. R., Kairiukstis, L. A. Methods of dendrochronology - applications in the environmental sciences [M]. Dordrecht: Kluwer Academic Publishers, 1990: 97-214.
     [4] Holmes, R. L. Computer-assisted quality control in tree-ring dating and measurement [J]. Tree-Ring Bulletin, 1983, 44: 69-75.
     [5] Cook, E. R. A time series analysis approach to tree ring standardization [D]. Tuscon: University of Arizona, 1985: 20-240.
     [6] Harris, I., Osborn, T. J., Jones, P., et al. Version 4 of the CRU TS monthly high-resolution gridded multivariate climate dataset [J]. Scientific Data, 2020, 7(1): 1-18.
     [7] Liang, E. Y., Shao, X. M., Qin, N. S. Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau [J]. Global and Planetary Change, 2008, 61(3): 313-320.
     [8] Fan, Z. X., Br?uning, A., Yang, B., et al. Tree ring density-based summer temperature reconstruction for the central Hengduan Mountains in southern China [J]. Global and Planetary Change, 2009, 65: 1-11.
     [9] Shao, X. M., Fan, J. M. Past climate on west Sichuan Plateau as reconstructed from ring-widths of dragon Spruce [J]. Quaternary Sciences, 1999, 19(1): 81-89.
     [10] Wang, J., Yang, B., Ljungqvist, F. C. A millennial summer temperature reconstruction for the eastern Tibetan Plateau from tree-ring width [J]. Journal of Climate, 2015, 28(13): 5289-5304.
     [11] Yu, S. L., Yuan, Y. J., Wei, W. S., et al. Reconstructed mean temperature in Mearkang, west Sichuan in July and its detection of climatic period signal [J]. Plateau Meteorology, 2012, 31(1): 193-200.
     [12] Zhu, H. F., Shao, X. M., Yin, Z. Y., et al. August temperature variability in the southeastern Tibetan Plateau since AD 1385 inferred from tree rings [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 305(1-4): 84-92.
     [13] Duan, J. P., Zhang, Q. B. A 449 year warm season temperature reconstruction in the southeastern Tibetan Plateau and its relation to solar activity [J]. Journal of Geophysical Research: Atmospheres, 2014, 119(20): 11578-11592.
     [14] Li, Z. S., Liu, G. H., Gong, L., et al. Tree ring-based temperature reconstruction over the past 186 years for the Miyaluo Natural Reserve, western Sichuan Province of China [J]. Theoretical and Applied Climatology, 2015, 120(3-4): 495-506.
     [15] Yang, B., Bra?uning, A., Shi, Y. F. Late Holocene temperature fluctuations on the Tibetan Plateau [J]. Quaternary Science Reviews, 2003, 22(21): 2335-2344.
     [16] Xu, P., Zhu, H. F., Shao, X. M., et al. Tree ring-dated fluctuation history of Midui Glacier since the Little Ice Age in the Southeastern Tibetan Plateau [J]. Science China Earth Sciences, 2012, 55(4): 521-530.
     [17] Xu, X. K., Yi, C. L. Little Ice Age on the Tibetan Plateau and its bordering mountains: evidence from moraine chronologies [J]. Global and Planetary Change, 2014, 116: 41-53.
     

Data Product:

ID Data Name Data Size Operation
1 TemReconWSCP_1383-2005.rar 2023.81KB
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