神农架地区树轮δ18O序列的气候指示意义

doi:10.18306/dlkxjz.2018.07.008

Abstract

Abstract:

In this study, a stable oxygen isotope chronology from tree-ring cellulose (δ¹⁸O) in Bashan fir(Abies forrestii) from Mt. Shennongjia in Hubei Province was correlated with meteorology records of the Badong meteorological station, circulation index data, and sea surface temperature of the South China Sea (SST). The chronology spans the time period of 1790-2011. The results indicate that the tree-ring δ¹⁸O chronology is closely correlated with local climate factors. The tree-ring δ¹⁸O chronology has a significantly positive correlation with March to April monthly mean temperature, has a significantly negative correlation with June to July monthly mean precipitation and June to July monthly mean relative humidity. Meanwhile, the tree-ring δ¹⁸O chronology has a significantly positive correlation with February to March area index of the northern hemisphere subtropical high (5E-360), September area index of the South China Sea subtropical high (100E-120E), January polar vortex area index of the Pacific Ocean (Zone 2, 150E-120W), and April to May sea surface temperature of the South China Sea (SST). A significantly negative correlation was found between the tree-ring δ¹⁸O chronology and January southern oscillation index (SOI). These indicate that the tree-ring δ¹⁸O chronology records at a large scale of atmospheric circulation information.This study is helpful to further understand the potential value of tree ring stable oxygen isotopes in the past climate change studies in Mt.Shennongjia, and provide a scientific basis for further research on climate reconstruction.

Key words: tree-ring, stable oxygen isotope, precipitation, sea surface temperature of the South China Sea (SST), circulation index

Fangfang ZHANG, Yonghong ZHENG, Guoyan PAN, Shuai YUAN, Fanxi KONG, Yongdong QI, Dan WANG. Climatic significance of tree-ring δ¹⁸O in Shennongjia Mountain[J].PROGRESS IN GEOGRAPHY, 2018, 37(7): 946-953.

Figures/Tables 11

Fig.1

Tab. 1

Fig.2

Fig.3

Tab.2

Fig.4

Fig.5

Fig.6

Fig.7

Fig.8

Fig.9

References 31

[1]	安文玲, 刘晓宏, 陈拓, 等. 2009. 云南丽江树轮δ18O记录的大气环流变化信息[J]. 地理学报, 64(9), 1103-1112.
	[An W L, Liu X H, Chen T, et al.2009. Atmosphere circulation information recorded in tree-ring δ18O at Lijiang, Yunnan Province[J]. Acta Geographica Sinica, 64(9), 1103-1112.]
[2]	陈秋艳, 勾晓华, 张军周, 等. 2015. 树轮宽度指示的神农架地区过去172年的冬春季温度变化[J]. 第四纪研究, 35(5): 1145-1154.
	[Chen Q Y, Gou X H, Zhang J Z, et al.2015. Tree-ring indicated of winter-spring temperature in Shennongjia Mountain area of central China over the past 172 years[J]. Quaternary Sciences, 35(5): 1145-1154.]
[3]	陈瑶, 勾晓华, 刘文火, 等. 2017. 亚洲树轮稳定氧同位素研究进展[J]. 冰川冻土, 39(2): 308-316.
	[Chen Y, Gou X H, Liu W H, et al.2017. Advances in tree-ring stable oxygen isotope study in Asia[J]. Journal of Glaciology and Geocryology, 39(2): 308-316.]
[4]	黄嘉佑, 刘舸, 赵昕奕. 2004. 副高、极涡因子对我国夏季降水的影响[J]. 大气科学, 28(4), 517-526. doi: 10.3878/j.issn.1006-9895.2004.04.04
	[Huang J Y, Liu G, Zhao X Y.2004. The inflence of subtropical high index and polar vortex index on the summertime precipitation in China[J]. Chinese Journal of Atomosphere Science, 28(4), 517-526.] doi: 10.3878/j.issn.1006-9895.2004.04.04
[5]	平凡, 唐细坝, 高守亭, 等. 2014. 长江和淮河流域汛期洪涝大气环流特征的比较[J]. 中国科学: 地球科学, 44(4): 766-782.
	[Ping F, Tang X B, Gao S T, et al.2014. A comparative study of the atmospheric circulations associated with rainy-season floods between theYangtze and Huaihe River Basins[J]. Science China: Earth Sciences, 44(4): 766-782.]
[6]	史婷婷, 陈植华, 张卫. 2012. 湖北宜昌香溪河流域环境同位素特征及其水循环意义[J]. 地质科技情报, 31(6): 161-167.
	[Shi T T, Chen Z H, Zhang W.2012. Characteristics of environmengtal isotopes in Xiangxi River Basin of Yichang Hubei Provice and its significance for hydrological cycle[J]. Geological Science and Technology Information, 31(6): 161-167.]
[7]	王建, 赵业思, 商志远, 等. 2016. 马尾松树轮不同组分稳定碳同位素的差异及其对气候变化响应的初步研究[J]. 地理科学, 36(8): 1261-1268.
	[Wang J, Zhao Y S, Shang Z Y, et al.2016. Diverse stable carbon isotope ratios in tree-ring components of pinus massoniana with their climate sensitivities[J]. Scientia Geographica Sinica, 36(8): 1261-1268.
[8]	吴绍洪, 潘韬, 戴尔阜. 2006. 植物稳定同位素研究进展与展望[J]. 地理科学进展, 25(3): 1-11. doi: 10.3969/j.issn.1007-6301.2006.03.001
	[Wu S H, Pan T, Dai E F.2016. The progress and prospect of stable isotopes in plants[J]. Progress in Geography, 25(3): 1-11.] doi: 10.3969/j.issn.1007-6301.2006.03.001
[9]	Bose T, Sengupta S, Chakraborty S, et al.2016. Reconstruction of soil water oxygen isotope values from tree ring cellulose and its implications for paleoclimate studies[J]. Quaternary International, 425: 387-398. doi: 10.1016/j.quaint.2016.07.052
[10]	Burk R L, Stuiver M.1981. Oxygen isotope ratios in trees reflect mean annual temperature and humidity[J]. Science, 211: 1417-1419. doi: 10.1126/science.211.4489.1417 pmid: 17731182
[11]	Dang H S, Zhang Y J, Zhang K R, et al.2013. Climate-growth relationships of subalpine fir (Abies fargesii) across the altitudinal range in the Shennongjia Mountains, central China[J]. Climatic Change, 117(4): 903-917. doi: 10.1007/s10584-012-0611-5
[12]	Dang H S, Zhang Y J, Zhang K R, et al.2014. Disturbance dynamics and history of an old-growth subalpine fir (Abies fargesii) forest in central China[J]. Plant Ecology, 215(10): 1111-1121. doi: 10.1007/s11258-014-0370-7
[13]	Duffy J E, Mccarroll D, Barnes A, et al.2017. Short-lived juvenile effects observed in stable carbon and oxygen isotopes of UK oak trees and historic building timbers[J]. Chemical Geology, 472, 1-7. doi: 10.1016/j.chemgeo.2017.09.007
[14]	Epstein S, Thompson P, Yapp C J.1977. Oxygen and Hydrogen Isotopic Ratios in Plant Cellulose[J]. Science, 198: 1209-1215. doi: 10.1126/science.198.4323.1209 pmid: 17741685
[15]	Helle G, Schleser G H.2004. Interpreting climate proxies from tree-rings[M]//Fischer H, Kumke T, Lohmann G et al. The climate in historical times: Towards a synthesis of holocene proxy data and climate models. Berlin, Germany: Springer: 129-148.
[16]	Hou X Y, Shi J F, Li L L, et al.2015. Growth respones of Abies fargesii to climate in Shennongjia Mount of Hubei Province, southeatern China[J]. Chinese Journal of Applied Ecology, 26(3): 689-696.
[17]	Lavergne A, Daux V, Villalba R, et al.2017. Improvement of isotope-based climate reconstructions in Patagonia through a better understanding of climate influences on isotopic fractionation in tree rings[J]. Earth and Planetary Science Letters, 459: 372-380. doi: 10.1016/j.epsl.2016.11.045
[18]	Liu X H, Qin D H, Shao X M, et al.2003. Variation and abrupt change of precipitation in Nyingchi Prefecture of Tibet Autonomous Region in past 350 years[J]. Journal of Glaciology & Geocryology, 25(4): 375-379.
[19]	Liu X H, Shao X M, Liang E Y, et al.2009. Climatic significance of tree-ring δ18O in the Qilian Mountains, northwestern China and its relationship to atmospheric circulation patterns[J]. Chemical Geology, 268(1): 147-154. doi: 10.1016/j.chemgeo.2009.08.005
[20]	Liu X H, Shao X M, Wang L L, et al.2007. Climatic significance of the stable carbon isotope composition of tree-ring cellulose: Comparison of Chinese hemlock (Tsuga chinensis Pritz) and alpine pine (Pinus densata Mast) in a temperate-moist region of China[J]. Science in China: Earth Sciences, 50(7): 1076-1085. doi: 10.1007/s11430-007-0043-7
[21]	Liu X H, Xu G B, Grießinger J, et al.2014. A shift in cloud cover over the southeastern Tibetan Plateau since 1600: Evidence from regional tree-ring δ18O and its linkages to tropical oceans[J]. Quaternary Science Reviews, 88: 55-68. doi: 10.1016/j.quascirev.2014.01.009
[22]	Liu Y, Cai Q F, Liu W G, et al.2008. Monsoon precipitation variation recorded by tree-ring δ18O in arid Northwest China since AD 1878[J]. Chemical Geology, 252(1): 56-61. doi: 10.1016/j.chemgeo.2008.01.024
[23]	Liu Z F, Tian L D, Chai X R, et al.2008. A model-based determination of spatial variation of precipitation δ18O over China[J]. Chemical Geology, 249(1): 203-212. doi: 10.1016/j.chemgeo.2007.12.011
[24]	Loader N J, Mccarroll D, Barker S, et al.2017. Inter-annual carbon isotope analysis of tree-rings by laser ablation[J]. Chemical Geology, 466: 323-326. doi: 10.1016/j.chemgeo.2017.06.021
[25]	Loader N J, Robertson I, Mccarroll D.2003. Comparison of stable carbon isotope ratios in the whole wood, cellulose and lignin of oak tree-rings[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 196(3): 395-407. doi: 10.1016/S0031-0182(03)00466-8
[26]	Roden J S, Lin G H, Ehleringer J R.2000. A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose[J]. Geochimica et Cosmochimica Acta, 64(1): 21-35. doi: 10.1016/S0016-7037(99)00195-7
[27]	Waterhouse J S, Switsur V R, Barker A C, et al.2002. Oxygen and hydrogen isotope ratios in tree rings: How well do models predict observed values[J]. Earth and Planetary Science Letters, 201(2): 421-430. doi: 10.1016/S0012-821X(02)00724-0
[28]	Wynn P M, Loader N J, Fairchild I J.2014. Interrogating trees for isotopic archives of atmospheric sulphur deposition and comparison to speleothem records[J]. Environmental Pollution, 187(8): 98-105. doi: 10.1016/j.envpol.2013.12.017
[29]	Xu C X, Zheng H Z, Nakatsuka T, et al.2013. Oxygen isotope signatures preserved in tree ring cellulose as a proxy for April-September precipitation in Fujian, the subtropical region of southeast China[J]. Journal of Geophysical Research Atmospheres, 118(23): 12805-12815. doi: 10.1002/2013JD019803
[30]	Xu C X, Zheng H Z, Nakatsuka T, et al.2016. Inter- and intra-annual tree-ring cellulose oxygen isotope variability in response to precipitation in Southeast China[J]. Trees, 30(3): 785-794. doi: 10.1007/s00468-015-1320-2
[31]	Zheng Y H, Shao X M, Lu F, et al.2016. February-May temperature reconstruction based on tree-ring widths of Abies fargesii from the Shennongjia area in central China[J]. International Journal of Biometeorology, 60(8), 1175-1181. doi: 10.1007/s00484-015-1111-x

Climatic significance of tree-ring δ¹⁸O in Shennongjia Mountain

RichHTML

PDF (PC)

Like

Knowledge

Abstract

Cite this article

share this article

Figures/Tables 11

References 31

Related Articles 15

Metrics

Comments

Recommended 10

[1]	Ming XU, Yuli SHI, Bin WANG. Reconstruction of high resolution monthly precipitation data of the Tibetan Plateau [J]. PROGRESS IN GEOGRAPHY, 2018, 37(7): 923-932.
[2]	Yanxin ZHU, Yanfang SANG. Spatial variability in the seasonal distribution of precipitation on the Tibetan Plateau [J]. PROGRESS IN GEOGRAPHY, 2018, 37(11): 1533-1544.
[3]	Xiaojie WEN, Shunbo YAO, Minjuan ZHAO. Coordinating the development of urbanization and vegetation coverage based on precipitation [J]. PROGRESS IN GEOGRAPHY, 2018, 37(10): 1352-1361.
[4]	Yuhan GUO, Zhonggen WANG, Yuliang WU. Comparison of applications of different reanalyzed precipitation data in the Lhasa River Basin based on HIMS model [J]. PROGRESS IN GEOGRAPHY, 2017, 36(8): 1033-1039.
[5]	Yungang LI, Jiaonan HE, Xue LI. Hydrological and meteorological droughts in the Red River Basin of Yunnan Province based on SPEI and SDI Indices [J]. PROGRESS IN GEOGRAPHY, 2016, 35(6): 758-767.
[6]	Xi HUANG, Zhonggen WANG, Yanfang SANG, Moyuan YANG, Xiaocong LIU, Tongliang GONG. Precision of data in three precipitation datasets of the Yarlung Zangbo River Basin [J]. PROGRESS IN GEOGRAPHY, 2016, 35(3): 339-348.
[7]	ZHAO Shikun, PANG Shuoguang, WEN Rong, LIU Zhongfang. Influence of below-cloud secondary evaporation on stable isotope composition in precipitation in the Haihe River Basin, China [J]. PROGRESS IN GEOGRAPHY, 2015, 34(8): 1031-1038.
[8]	DING Jingyi, ZHAO Wenwu, WANG Jun, FANG Xuening. Scale effect of the impact on runoff of variations in precipitation/vegetation： taking northern Shaanxi loess hilly-gully region as an example [J]. PROGRESS IN GEOGRAPHY, 2015, 34(8): 1039-1051.
[9]	CAO Yongqiang, LIU Jiajia, GAO Lu. Distribution and trend analysis of heavy precipitation days in Liaoning Province [J]. PROGRESS IN GEOGRAPHY, 2015, 34(8): 1052-1060.
[10]	Shuangshuang LI, Saini YANG, Xianfeng LIU. Spatiotemporal variability of extreme precipitation in north and south of the Qinling-Huaihe region and influencing factors during 1960-2013 [J]. PROGRESS IN GEOGRAPHY, 2015, 34(3): 354-363.
[11]	Tao JI, Hua YANG, Rui LIU, Tairong HE, Jianfeng WU. Applicability analysis of the TRMM precipitation data in the Sichuan-Chongqing region [J]. PROGRESS IN GEOGRAPHY, 2014, 33(10): 1375-1386.
[12]	Yanjiao WANG, Feng YAN. Regional differentiation and decadal change of precipitation in China in 1960-2010 [J]. PROGRESS IN GEOGRAPHY, 2014, 33(10): 1354-1363.
[13]	WANG Yanjun, WANG Suiji, Su Teng. Quantification of impacts of precipitation and human activities on runoff changes in different sections of Songhua River during 1955-2010 [J]. PROGRESS IN GEOGRAPHY, 2014, 33(1): 65-75.
[14]	MA Jinhui, QU Chuang, ZHANG Haixiao, XIA Yanqiu. Spatial downscaling of TRMM precipitation data based on DEM in the upstream of Shiyang River Basin during 2001-2010 [J]. PROGRESS IN GEOGRAPHY, 2013, 9(9): 1423-1432.
[15]	ZHAO Na, YUE Tianxiang, WANG Chenliang. Surface modeling of seasonal mean precipitation in China during 1951-2010 [J]. PROGRESS IN GEOGRAPHY, 2013, 32(1): 49-58.

Climatic significance of tree-ring δ18O in Shennongjia Mountain

RichHTML

PDF (PC)

Like

Knowledge

Abstract

Cite this article

share this article

Figures/Tables 11

References 31

Related Articles 15

Metrics

Comments

Recommended 10

Climatic significance of tree-ring δ¹⁸O in Shennongjia Mountain