Quantitative reconstruction of Holocene precipitation over Qinghai Tibet Plateau Based on sporopollen data

Quantitative reconstruction of Holocene precipitation over Qinghai Tibet Plateau Based on sporopollen data


The surface palynological data in this dataset are from the East Asian palynological database( http://eapd.sysu.edu.cn/database/ And the surface pollen data of the northeastern margin of the Qinghai Tibet Plateau. The precipitation data of surface soil palynological points were obtained from the annual average precipitation data of 126 meteorological stations in the Qinghai Tibet Plateau and its surrounding areas (Xinjiang, Gansu, Sichuan) from 1950 to 1980 (the data came from China Meteorological Science Data Sharing Service Network) http://www.data.ac.cn/xiazai/ )Because topography has a great impact on climate change, Therefore, in ArcGIS, the uneven distribution of annual precipitation data of meteorological stations is transformed into grid data on the surface of the Qinghai Tibet Plateau by Kriging spatial interpolation method, and the precipitation grid data of the surface palynological point can be regarded as the actual precipitation data of the point. By using the method of transformation function, the representative surface palynological types are selected, and the linear regression between them and modern climate is established. The fossil Palynological Assemblages are substituted into the regression equation to obtain paleoclimate parameters. Using the modern analogy method (MAT), assuming that the relationship between vegetation types and climate in the past is corresponding, we can compare the sporopollen spectrum of the strata indicating vegetation types with that of the present representative soil to reveal the similarity between them. Then we can get the corresponding precipitation data of the strata sporopollen by matrix operation with the modern precipitation data of the corresponding points.


File naming and required software

The data set is stored in Excel format, and contains 14 worksheets, which are the precipitation simulation values in mat, the precipitation simulation values in wapls, the Eastern Integrated precipitation sequence cumulative anomaly, the Eastern Integrated precipitation sequence, the western integrated precipitation sequence cumulative anomaly, the western integrated precipitation sequence, the TOC content of Lake stagger, the oxygen isotope of golingco shell, the TOC content of pumoyongco, the TOC content of Qinghai Lake, the TOC content of Qinghai Lake The core 08-c1 in the north of Zoige, the integrated sequence of precipitation in Zoige, the integrated sequence of precipitation in taruocuo, and the oxygen isotope in Tianmen cave. There are precipitation observation values and precipitation simulation values in mat and wapls; There are years and precipitation data in the worksheets of Eastern precipitation integration series and Western precipitation integration series; There are years and accumulated anomaly data in the worksheets of accumulated anomaly line of integrated precipitation series in the East and accumulated anomaly line of integrated precipitation series in the West; The TOC content in the working tables of Damen lake, pumoyongcuo lake and Qinghai Lake are the percentages of depth and TOC; The chronological and oxygen isotopic data are shown in the oxygen isotopic tables of gelingcuo shell and Tianmen cave; The data of 08-c1 well in the north of Zoige are age and vegetation coverage; There are years and precipitation data in taruo co precipitation integrated series worksheet and Zoige precipitation integrated series worksheet. Data files can be opened with office software or imported into relational database system.


Data Citations Data citation guideline What's data citation?
Cite as:

Hou, G. (2021). Quantitative reconstruction of Holocene precipitation over Qinghai Tibet Plateau Based on sporopollen data. A Big Earth Data Platform for Three Poles, (Download the reference: RIS | Bibtex )

Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.


References literature

1.Ma, Q.F., Zhu, L.P., Lv, X.M., Guo, Y., Ju, J.T., Wang, J.B., Tang, L.Y. (2014). Pollen-inferred Holocene vegetation and climate histories in Taro Co southwestern Tibetan Plateau. Chinese Science Bulletin, (26), 2631-2644. (View Details )

2.Hou, X.Y. Vegetation Atlas of China (1 ∶ 1 million). Beijing, Scientific Publishers. (View Details )

3.Wei, H.C., Ma, H.Z., Zheng, Z., Huang, k.Y., Wang, Z.Y., Zhai, J. (2010). Characteristics of Pollen Assemblages of Surface Samples from The North-Eastern Tibetan Plateau and Their Implications for Vegetation and Climate. Marine Geology & Quaternary Geology, (04), 187-192. (View Details )

4.Lu, C.X, Wang, L., Xie, G.D., leng, Y.F. (2007). Altitude Effect of Precipitation and Spatial Distribution of Qinghai-Tibetan Plateau. Mountain Research, (06), 655-663. (View Details )

5.Hou, G.L., Chong, Y., Xiao, J.Y. (2012). Synthetical Reconstruction of the Precipitation Series of the Qinghai-Tibet Plateau during the Holocene. Progress in Geography, (09), 1117-1123. (View Details )

6.Sun, X.H., Zhao, Y., Li, Q. (2017). Holocene peatland development and vegetation changes in the Zoige Basin, eastern Tibetan Plateau. Scientia Sinica, (09), 1097-1109. (View Details )

7.Xu Qinghai, Li manyue, Zhang Shengrui, Zhang Yahong, Zhang Panpan, Lu Jingyao. (2015). Modem pollen processes of China: Progress and Problems. Scientia Sinica(Terrae), (11), 1661-1682. (View Details )

8.Huang, K.Y., Wei, J.H., Chen, B.S., Zhang, H., Zheng, Z., Cao, L.L., Zheng, Y.W. (2013). Research Progress of Pollen-Based Quantitative Paleoclimate Reconstruction using Modern Analogue Technique. Quaternary Sciences, (06), 1069-1079. (View Details )

9.Yuan, Y.J., Ye,W., Dong, G.R. (2000). Reconstruction and Discussion of 314 a Precipitation in Yili Prefecture Western Tianshan Mountains. Journal of Glaciology and Geocryology, (02), 121-127. (View Details )

10.He, H.Y., Guo, Z.H., Xiao, W.F., Guo, Q.S. (2005). Mapping monthly precipitation for Tibetan Plateau with GIS and multivariate analysis based on DEM data. Acta Ecologica Sinica, 25 (11), 2934-2937. (View Details )

11.Wu, G.X., Liu, Y.M., He, B., etal. Review of the impact of the Tibetan Plateau sensible heat driven air pump on the Asian summer monsoon. Chinese Journal of Atmospheric Sciences, 42(3), 488-504. (View Details )

12.Xu, Q.H., Yue, C. Li, M. Jane Bunting, Liu, J.S. (2010). The effects of training set selection on the relationship between pollen assemblages and climate parameters: Implications for reconstructing past climate. Palaeogeography, Palaeoclimatology, Palaeoecology, 289(1), 123-133. (View Details )

13.Lu, H.Y. (2012). Modern pollen distributions in Qinghai-Tibetan Plateau and the development of transfer functions for reconstructing Holocene environmental changes. Quaternary International, 30(12), 947-966. (View Details )

14.Zheng, Z., Wei,J.H., Huang, K.Y., etal. (2014). East Asian pollen database: Modern pollen distribution and its quantitative relationship with vegetation and climate. Journal of Biogeography, 41(14), 1819-1832. (View Details )

15.Chuan, X.L., Chi,X., Chen,R.X., Ming, X.Y. (2018). Study of modern pollen distribution in the northeastern Indian Ocean and their application to paleoenvironment reconstruction. Review of Palaeobotany and Palynology, 149(13), 151-166. (View Details )


Support Program

Qinghai Provincial Key Laboratory of Geospatial Information Technology and Application Foundation Project (No:2018-006)

National Natural Science Foundation of China, No.41761018 (No:41761018)

Natural Science Foundation Project of Qinghai Provincial Science and Technology Department (No:2017-ZJ-903)

Copyright & License

To respect the intellectual property rights, protect the rights of data authors, expand services of the data center, and evaluate the application potential of data, data users should clearly indicate the source of the data and the author of the data in the research results generated by using the data (including published papers, articles, data products, and unpublished research reports, data products and other results). For re-posting (second or multiple releases) data, the author must also indicate the source of the original data.


License: This work is licensed under an Attribution 4.0 International (CC BY 4.0)


Related Resources
Comments

Current page automatically show English comments Show comments in all languages

Download Follow
Keywords
Geographic coverage
East: 103.55 West: 102.10
South: 32.20 North: 34.05
Details
  • Temporal resolution: 1000 year < x
  • Spatial resolution: -
  • File size: 0.636 MB
  • Views: 2021
  • Downloads: 450
  • Access: Open Access
  • Temporal coverage: 12,000 years ago -- 1,500 years ago
  • Updated time: 2021-05-18
Contacts
: HOU Guangliang  

Distributor: A Big Earth Data Platform for Three Poles

Email: poles@itpcas.ac.cn

Export metadata