[1]周 莹,马 龙*,刘廷玺,等.杜松树轮年表记录的192 a阴山地区最低气温变化[J].山地学报,2021,(3):316-326.[doi:10.16089/j.cnki.1008-2786.000598]
 ZHOU Ying,MA Long*,LIU Tingxi,et al.Changes of Minimum Temperature Recorded by Juniperus. Tree Ring Chronology during 192a in the Yinshan Mountains Area of China[J].Mountain Research,2021,(3):316-326.[doi:10.16089/j.cnki.1008-2786.000598]
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杜松树轮年表记录的192 a阴山地区最低气温变化
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2021年第3期
页码:
316-326
栏目:
山地环境
出版日期:
2021-07-10

文章信息/Info

Title:
Changes of Minimum Temperature Recorded by Juniperus. Tree Ring Chronology during 192a in the Yinshan Mountains Area of China
文章编号:
1008-2786-(2021)3-316-11
作者:
周 莹马 龙*刘廷玺黄 星孙柏林
内蒙古农业大学 水利与土木建筑工程学院,呼和浩特 010018
Author(s):
ZHOU Ying MA Long* LIU Tingxi HUANG Xing SUN Bolin
College of Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Hohhot 010018, China
关键词:
树轮年表 气候变化 杜松 阴山地区
分类号:
P467
DOI:
10.16089/j.cnki.1008-2786.000598
文献标志码:
A
摘要:
利用树木年轮重建长历史气候因子并揭示其变化规律,可充分弥补现代实测数据的不足。本研究在内蒙古阴山地区采集杜松树种样本,经过运用ARSTAN程序去除生长趋势,采用双权重平均法合成年表,建立了192 a内蒙古阴山地区杜松(Juniperus rigida S. et Z.)树木年轮标准化年表,分析了杜松生长与气候因子变化间的响应关系,重建了年平均最低气温序列。结果表明:(1)三类气温对杜松生长影响均呈显著负相关,其中最低气温尤为显著;(2)相对湿度、降水对杜松径向生长影响相对较弱;(3)192 a以来该地区平均最低气温出现了三次突变和两次停滞,经历了五个偏暖期(1825—1829年、1870—1887年、1894—1918年、1934—1945年、1981—2016年)以及四个偏冷期(1829—1870年、1887—1894年、1918—1934年、1945—1981年),存在2 a、11 a和30 a的变化周期,与ENSO、太阳黑子活动等周期较为接近。本研究丰富了树轮年表库,并为区域长期气候变化以及生态环境问题的应对提供了参考。

参考文献/References:

[1] KERHOULAS L P, KANE J M. Sensitivity of ring growth and carbon allocation to climatic variation vary within ponderosa pine trees [J]. Tree Physiology, 2012,32(1): 14-23. DOI: 10.1093/treephys/tpr112
[2] DIAZ H F, TRIGO R, HUGHES M K, et al. Spatial and temporal characteristics of climate in medieval times revisited [J]. Bulletin of American Meteorological Society, 2011,92(11):1487-1500. DOI: 10.1175/BAMS-D-10-05003.1
[3] LI B, CHEN Y, SHI X, et al. Temperature and precipitation changes in different environments in the arid region of northwest China [J]. Theoretical and Applied Climatology, 2013, 112(3-4): 589-596. DOI: 10.1007/s00704-012-0753-4
[4] 王婷,于丹,李江风,等. 树木年轮宽度与气候变化关系研究进展[J]. 植物生态学报,2003, 27(1):23-33. [WANG Ting, YU Dan, LI Jiangfeng, et al. Advances in research on the relationship between climate change and tree-ring width [J]. Acta Phytoecologica Sinica, 2003, 27(1):23-33] DOI: 10.17521/cjpe.2003.0004
[5] PEARLJ K, ANCHUKAITIS K J, DONNELLY J P, et al. A late Holocene subfossil Atlantic white cedar tree-ring chronology from the northeastern United States [J]. Quaternary Science Reviews, 2020, 228:106104. DOI: 10.1016/j.quascirev.2019.106104
[6] PERONE A, LOMBARDI F, MARCHETTI M, et al. Evidence of solar activity and El Niño signals in tree rings of Araucaria araucana and A. angustifolia in South America [J]. Global and Planetary Change, 2016, 145:1-10. DOI: 10.1016/j.gloplacha.2016.08.004
[7] MUIGG B, SEIM A, TEGEL W, et al. Tree rings reveal dry conditions during Charlemagne's Fossa Carolina construction in 793 CE [J]. Quaternary Science Reviews, 2020, 227:106040. DOI: 10.1016/j.quascirev.2019.106040
[8] BUNTGEN U, ESPER J, FRANK D C, et al. A 1052-year tree-ring proxy for Alpine summer temperatures [J]. Climate Dynamics, 2005, 25(2-3):141-153. DOI: 10.1007/s00382-005-0028-1
[9] WILES G C, SOLOMINA O, D'ARRIGO R, et al. Reconstructed summer temperatures over the last 400 years based on larch ring widths: Sakhalin Island, Russian Far East [J]. Climate Dynamics, 2014, 45(1-2):397-405. DOI: 10.1007/s00382-014-2209-2
[10] LEAL S, EAMUS D, GRABNER M, et al. Tree rings of Pinus nigra from the Vienna basin region(Austria)show evidence of change in climatic sensitivity in the late 20th century [J]. Canadian Journal of Forest Research, 2008, 38(4):744-759. DOI: 10.1139/X07-189
[11] BARBER V A, JUADY G P, FINNEY B P. Reduced growth of Alaskan white spruce in the twentieth century from temperature-induced drought stress [J]. Nature, 2000, 405(6787): 668-673.
[12] KULLMAN L. 20th century climate warming and tree-limit rise in the southern Scandes of Sweden [J]. A Journal of the Human Environment, 2001, 30(2):72-80. DOI: 10.1579/0044-7447-30.2.72
[13] SANCHEZ-SALGUREO R, NAVARRO-CERRILLO R M, CAMARERO J J, et al. Selective drought-induced decline of pine species in southeastern Spain [J]. Climatic Change, 2012, 113(3-4):767-785. DOI: 10.1007/s10584-011-0372-6
[14] VITALI V, BUNTGEN U, BAUHUS J. Silver fir and Douglas fir are more tolerant to extreme droughts than Norway spruce in south-western Germany [J]. Global Change Biology, 2017,23(12):5108-5119. DOI: 10.1111/gcb.13774
[15] LARA A, VILLALBA R, URRUTIA R. A 400-year tree-ring record of the Puelo River summer-fall streamflow in the valdivian rainforest eco-region, Chile [J]. Climatic Change, 2008, 86(3-4):331-356. DOI: 10.1007/s10584-007-9287-7
[16] HUGHES M K, SCHWEINGRUBER F H, CARTWRIGHT D, et al. July-August temperature at Edinburgh between 1721 and 1975 from tree-ring density and width data [J]. Nature, 1984,308(5957):341-344. DOI: 10.1038/308341a0
[17] ZHANG Y, WILMKING M. Divergent growth responses and increasing temperature limitation of Qinghai spruce growth along an elevation gradient at the northeast Tibet Plateau [J]. Forest Ecology and Management, 2010, 260(6): 1076-1082. DOI: 10.1016/j.foreco.2010.06.034
[18] D'AUBETERRE G, FAVILLIER A, MAINIERI R, et al. Tree-ring reconstruction of snow avalanche activity: Does avalanche path selection matter?[J]. Science of the Total Environment, 2019, 684(20):496-508. DOI: 10.1016/j.scitotenv.2019.05.194
[19] BUCKLEY B M, UMMENHOFER C C, D'ARRIGO R D, et al. Correction to: Interdecadal Pacific Oscillation reconstructed from trans-Pacific tree rings: 1350—2004 CE [J]. Climate Dynamics, 2019, 53:5137. DOI: 10.1007/s00382-019-04928-5
[20] SONTI N F, HALLETT R A, GRIFFIN K L, et al. White oak and red maple tree ring analysis reveals enhanced productivity in urban forest patches [J]. Forest Ecology and Management, 2019,453:117626. DOI: 10.1016/j.foreco.2019.117626
[21] 秦莉,袁玉江,喻树龙,等. 新疆赛里木湖流域过去373年降水变化的树轮记录[J]. 生态学报,2017,37(4):1084-1092. [QIN Li, YUAN Yujiang, YU Shulong. et al. Tree-ring-based precipitation variability over the past 373 years in the Sayram Lake Basin, Tianshan Mountains [J]. Acta Ecologica Sinica, 2017, 37(4):1084-1092] DOI: 10.5846/stxb201604270801
[22] 陈峰,魏文寿,袁玉江,等. 基于多点树轮序列的1768—2006年甘肃降水量变化[J]. 中国沙漠,2013,33(5):1520-1526. [CHEN Feng, WEI Wenshou, YUAN Yujiang, et al. Variation of annual precipitation during 1768—2006 in Gansu inferred from multi-site tree-ring chronologies [J]. Journal of Desert Research, 2013, 33(5): 1520-1526] DOI:10.7522/j.issn.1000-694X.2013.00218
[23] YIN H, LIU H, HUANG L, et al. Reconstruction of October mean temperature since 1796 in Wuying based on tree ring data [J]. Advances in Climate Change Research, 2010,1(2):100-106. DOI: 10.3724/SP.J.1248.2010.00100
[24] 刘洪滨,邵雪梅. 采用秦岭冷杉年轮宽度重建陕西镇安1755年以来的初春温度[J]. 气象学报,2000,58(2):223-233. [LIU Hongbin, SHAO Xuemei. Reconstruction of early-spring temperature at Zhenan from 1755 using tree ring chronology [J]. Acta Meteorologica Sinica, 2000,58(2):223-233] DOI: 10.11676/qxxb2000.023
[25] 马龙,刘廷玺,寇志强,等. 科尔沁沙地榆树生长与水文气象因子的关系及气候重建[J]. 冰川冻土,2007,29(5): 802-807. [MA Long, LIU Tingxi, KOU Zhiqiang. et al. Relationship of elm growth and hydrometeorological factors of Horqin sandy land and climatic series reconstruction [J]. Journal of Glaciology and Geocryoligy, 2007,29(5):802-807] DOI: 10.3969/j.issn.1000-0240.2007.05.019
[26] 段媛. 不同海拔太白红杉年轮对气候响应差异及气温重建[D]. 西安: 西北大学,2016:33. [DUAN Yuan. The difference response to climate of Larix chinensis at difference altitudes and temperature reconstruction [D]. Xi'an: Northwest University, 2016:33]
[27] 赵学鹏,白学平,李俊霞,等. 气候变暖背景下不同海拔长白落叶松对气候变化的响应[J]. 生态学杂志,2019,38(3):637-647. [ZHAO Xuepeng, BAI Xueping, LI Junxia, et al. Response of Larix olgensis at different elevations to climate change in the context of climate warming [J]. Chinese Journal of Ecology, 2019, 38(3):637-647] DOI: 10.13292/j.1000-4890.201903.021
[28] LI J, GOU X, COOK E R, et al. Tree-ring based drought reconstruction for the central Tien Shan area in northwest China [J]. Geophysical Research Letters, 2006, 33:L07715. DOI: 10.1029/2006GL025803
[29] 桑卫国,王云霞,苏宏新,等. 天山云杉树轮宽度对梯度水分因子的响应[J]. 科学通报,2007,52(19):2292-2298. [SANG Weiguo, WANG Yunxia, SU Hongxin, et al. Response of spruce ring width to gradient water factor in Tianshan Mountain [J]. Chinese Science Bulletin, 2007,52(19):2292-2298] DOI: 10.3321/j.issn:0023-074x.2007.19.014
[30] 高娜,李书恒,白红英,等. 秦岭牛背梁自然保护区巴山冷杉(Abies fargesii)树轮宽度对气候变化响应的分离效应[J]. 生态学杂志,2016,35(8):2056-2065. [GAO Na, LI Shuheng, BAI Hongying, et al. Response divergence of Abies fargesii tree-ring widths to climate variation in the Niubeiliang Nature Reserve of the Qinling Mountains [J]. Chinese Journal of Ecology, 2016, 35(8):2056-2065] DOI: 10.13292/j.1000-4890.201608.025
[31] 鲁瑞洁,夏虹. 腾格里沙漠南缘油松树轮宽度变化及其对气候因子的响应[J]. 中国沙漠, 2006,26(3):399-402. [LU Ruijie, XIA Hong. Response of contemporary tree ring width of pinus tabulaeformis to climate change at south margin of Tengger Desert, China [J]. Journal of Desert Research, 2006,26(3):399-402] DOI: 10.3321/j.issn:1000-694X.2006.03.015
[32] 王梦麦,戴君虎,白洁,等. 利用树木年轮重建六盘山地区1900年以来的干湿变化[J]. 古地理学报,2009,11(3):355-360. [WANG Mengmai, DAI Junhu, BAI Jie, et al. Reconstruction of humidity changes from tree rings in Liupan Mountains area since 1900 [J]. Journal of Palaeogeography, 2009, 11(3):355-360]
[33] 朱娜. 秦岭南坡油松年轮δ13C变化及与气候因子的关系研究[D]. 西安: 西北农林科技大学,2019:88-90. [ZHU Na. Research on the change of δ13C of Pinus tabulaeformis on the southern of Qinling Mountains and its relationship with climatic factors [D]. Xi'an: Northwest Agriculture & Forestry University, 2019: 88-90]
[34] 孙军艳,刘禹,蔡秋芳,等. 额济纳233年来胡杨树轮年表的建立及其所记录的气象、水文变化[J].第四纪研究,2006,26(5):799-807. [SUN Junyan, LIU Yu, CAI Qiufang, et al. Climatic and hydrological changes of Ejin, Inner Mongolia, China during the past 233 years recorded in tree-rings of populus euphratica [J]. Quaternary Sciences, 2006,26(5): 799-807] DOI: 10.3321/j.issn:1001-7410.2006.05.015
[35] YANG B, QIN C, WANG J, et al. A 3500-year tree-ring record of annual precipitation on the northeastern Tibetan plateau [J]. Proceedings of the National Academy of Sciences of the United States of America, 2014, 111(8):2903-2908. DOI: 10.1073/pnas.1319238111
[36] 褚胜利,李登武,李景侠. 陕西府谷杜松自然保护区杜松种群结构与生命表分析[J]. 四川大学学报(自然科学版),2008,45(1): 176-180. [CHU Shengli, LI Dengwu, LI Jingxia. Study on the population structure and life table of the endangered population of juniperus rigida in Fugu Natural Reserve in Shaanxi province [J]. Journal of Sichuan University(Natural Science Edition), 2008,45(1):176-180] DOI: 10.3969/j.issn.0490-6756.2008.01.034
[37] SHIN W S, HA J. Analyses of lipid and volatile components in juniper seed(Juniperus rigida Sieb. et Zucc.)[J]. Journal of the Korean Society of Food Science & Nutrition, 2003, 32(6): 795.
[38] 刘静,温仲明,刚成诚. 黄土高原不同植被覆被类型NDVI对气候变化的响应[J]. 生态学报,2020,40(2):678-691. [LIU Jing, WEN Zhongming, GANG Chengcheng. Normalized difference vegetation index of different vegetation cover types and its responses to climate change in the Loess Plateau [J]. Acta Ecologica Sinica, 2020,40(2):678-691] DOI: 10.5846/stxb201901090082
[39] LIU Y, ZHANG X, SONG H, et al. Tree-ring-width-based PDSI reconstruction for central Inner Mongolia, China over the past 333 years [J]. Climate Dynamics, 2017, 48(3-4):867-879. DOI: 10.1007/s00382-016-3115-6
[40] 赵利清,杨劼. 准格尔黄土丘陵沟壑区杜松疏林特征分析[J]. 西北植物学报,2011,31(3):595-601. [ZHAO Liqing, YANG Jie. Characteristics of Juniperus rigida open forest in Junger Loess hill-gully region [J]. Acta Botanica Boreali-Occidentalia Sinica, 2011, 31(3): 595-601]
[41] 曹红芳,秦伟,胡永宁,等. 榆树年轮记录的浑善达克沙地春季平均最高气温[J]. 中国沙漠,2018,38(6):1313-1320. [CAO Hongfang, QIN Wei, HU Yongning. et al. Elm tree-ring records of Spring mean maximum temperature in the Otindag Sandy Land, China [J]. Journal of Desert Research, 2018, 38(6):1313-1320] DOI: 10.7522/j.issn.1000-694X.2018.00056
[42] 刘欣华,张春霞,万芳. 内蒙古西部地区生态环境建设的成就与问题[J]. 内蒙古林业调查设计,2002,25(3):19-20+45. [LIU Xinhua, ZHANG Chunxia, WAN Fang. Achievements and problems of ecological environment construction in western Inner Mongolia [J]. Inner Mongolia Forestry Investigation and Design, 2002,25(3): 19-20+45] DOI: 10.3969/j.issn.1006-6993.2002.03.008
[43] 郭金海. 乌拉山植被及植物区系组成特征[J]. 内蒙古林业调查设计,2006,29(3): 27-30. [GUO Jinhai. Vegetation and floristic composition characteristics of Wula Mountain [J]. Inner Mongolia Forestry Investigation and Design, 2006,29(3): 27-30] DOI: 10.3969/j.issn.1006-6993.2006.03.010
[44] 李荣. 有杜松(Juniperus rigida Sieb. et Zucc.)参加群落的群落特征、生长速率及其与生境关系的研究[D]. 呼和浩特: 内蒙古大学,2013:55-56. [LI Rong. Study of community characteristics, growth rate and relationship with different habitats of community participated with Juniperus [D]. Hohhot: Inner Mongolia University, 2013:55-56]
[45] 李宗善,刘国华,傅伯杰,等. 利用树木年轮宽度资料重建川西米亚罗地区过去200年夏季温度的变化[J]. 第四纪研究, 2011, 31(3):522-534. [LI Zongshan, LIU Guohua, FU Bojie, et al. Reconstruction of summer temperature changes in the past 200 years using tree-ring width data in the Miyaluo region, western Sichuan [J]. Quaternary Sciences, 2011, 31(3):522-534]
[46] 孙柏林,马龙,冯起,等. 内蒙古气温变暖停滞对其影响因子变化的响应[J]. 中国环境科学,2019,39(5): 2131-2142. [SUN Bolin, MA Long, FENG Qi, et al. Response of the warming hiatus to changing influences over the Inner Mongolia Autonomous Region [J]. China Environmental Science, 2019, 39(5):2131-2142] DOI: 10.19674/j.cnki.issn1000-6923.2019.0255
[47] FANG O, ZHANG Q B, VITASSE Y, et al. The frequency and severity of past droughts shape the drought sensitivity of juniper trees on the Tibetan plateau [J]. Forest Ecology and Management, 2021, 486:118968. DOI: 10.1016/j.foreco.2021.118968
[48] COOK E R, BRIFFA K R, JONES P D. et al. Spatial regression methods in dendroclimatology: A review and comparison of two techniques [J]. International Journal of Climatology, 1994, 14:379-402. DOI: 10.1002/joc.3370140404
[49] 何吉成,邵雪梅. 德令哈地区树轮宽度指数与草地植被指数的关系[J]. 科学通报,2006,51(9):1083-1090. [HE Jicheng, SHAO Xuemei. Relationship between tree-ring width index and grassland vegetation index in Delingha region [J]. Science Bulletin, 2006,51(9):1083-1090] DOI: 10.3321/j.issn:0023-074X.2006.09.014
[50] 李宗善,刘国华,张齐兵,等. 利用树木年轮宽度资料重建川西卧龙地区过去159年夏季温度的变化[J]. 植物生态学报,2010,34(6): 628-641. [LI Zongshan, LIU Guohua, ZHANG Qibing, et al. Tree ring reconstruction of summer temperature variations over the past 159 years in Wolong National Natural Reserve, western Sichuan, China [J]. Chinese Journal of Plant Ecology, 2010, 34(6): 628-641] DOI: 10.3773/j.issn.1005-264x.2010.06.002
[51] 杜恒文,叶茂. 塔里木河下游胡杨年轮径向生长对极端低温的响应研究[J]. 生物学杂志,2020,37(4):50-53+84. [DU Hengwen, YE Mao. Response of radial growth of Populus euphratica Oliv. to extreme low temperature in the lower reaches of Tarim River [J]. Journal of Biology, 2020, 37(4):50-53+84] DOI: 10.3969/j.issn.2095-1736.2020.04.050
[52] 尚华明,洪建昌,张瑞波,等. 树轮记录的西藏东北部过去552 a上年10月至当年5月降水量变化[J].山地学报,2018,36(6):821-832. [SHANG Huaming, HONG Jianchang, ZHANG Ruibo, et al. Tree-ring recorded 522-year precipitation from previous October to May in northeast Tibet, China [J]. Mountain Research, 2018,36(6):821-832] DOI: 10.16089/j.cnki.1008-2786.000378
[53] 陈峰,袁玉江,喻树龙. 闽中北柳杉树轮指示的气候信号与季风区不同地域干湿变化关系[J]. 山地学报,2015,33(6):690-695. [CHEN Feng, YUAN Yujiang, YU Shulong. Drought signals in the tree-ring width record of cedar(cryptomeria fortunei)trees from north central Fujian: Linkages to the monsoonal regions [J]. Mountain Research, 2015,33(6):690-695] DOI: 10.16089/j.cnki.1008-2786.000083
[54] 杨丽萍. 内蒙古多伦县近60年气候变化及基于榆树轮宽年表的气候相关[D]. 呼和浩特: 内蒙古农业大学, 2013:66-75. [YANG Liping. Correlation study on climate based on ring width chronology of Ulmus pumila and climate change in Inner Mongolia Duolun County in past 60 years [D]. Hohhot: Inner Mongolia Agricultural University, 2013: 66-75]
[55] 刘洪滨,邵雪梅. 采用秦岭冷杉年轮宽度重建陕西镇安1755年以来的初春温度[J]. 气象学报, 2000,58(2):223-233. [LIU Hongbin, SHAO Xuemei. Reconstruction of early-spring temperature at Zhen An from 1755 using tree ring chronology [J]. Acta Meteorologica Sinica, 2000,58(2):223-233]
[56] 沈建国. 中国气象灾害大典:内蒙古卷[M]. 北京: 气象出版社,2008:190-200. [SHEN Jianguo. China meteorological disaster canon: Inner Mongolia volume [M]. Beijing: Meteorological Press, 2008:190-200]
[57] 靳立亚,秦宁生,勾晓华,等. 青海南部高原近450年来春季最高气温序列及其时变特征[J]. 第四纪研究,2005,25(2): 193-201. [JIN Liya, QIN Ningsheng, GOU Xiaohua, et al. Series of Spring maximum temperature in southern Qinghai plateau and analysis of its variations during the last 450 years [J]. Quaternary Sciences, 2005, 25(2): 193-201]
[58] 张瑞波,袁玉江,魏文寿,等. 西藏东部过去400年秋、冬季平均最低气温的树木年轮分析[J]. 高原气象,2010,29(2): 359-365. [ZHANG Ruibo, YUAN Yujiang, WEI Wenshou, et al. Analysis on mean minimum temperature in the east Tibet from Autumn to Winter in tree ring of the past 400 years [J]. Plateau Meteorology, 2010, 29(2): 359-365]
[59] XU D, YAN H. A study of the impacts of climate change on the geographic distribution of Pinus koraiensis in China [J]. Environment International, 2001, 27(2-3):201-205. DOI: 10.1016/S0160-4120(01)00083-6
[60] 刘禹,蔡秋芳,马利民,等. 树轮降水记录及东亚夏季风强弱变化——以内蒙古包头地区为例[J]. 地学前缘(中国地质大学,北京),2001,8(1): 91-97. [LIU Yu, CAI Qiufang, MA Limin, et al. Tree ring precipitation records from Baotou and the east Summer monsoon variations for the last 254 years [J]. Earth Science Frontiers(China University of Geosciences, Beijing), 2001,8(1): 91-97] DOI: 10.3321/j.issn:1005-2321.2001.01.012
[61] SHAH S K, PANDEY U, MEHROTRA N, et al. A Winter temperature reconstruction for the Lidder Valley, Kashmir, Northwest Himalaya based on tree-rings of Pinus wallichiana [J]. Climate Dynamics, 2019(53):4059-4075. DOI: 10.1007/s00382-019-04773-6
[62] KAUFMANN R K, KAUPPI H, MANN M L, et al. Reconciling anthropogenic climate change with observed temperature since 1998 [J]. Proceedings of the National Academy of Sciences, 2011, 108(29):11790-11793.
[63] 段建平,王丽丽,李论,等. 树轮最大密度记录的贡嘎山区公元1837年以来的温度变化[J]. 科学通报,2010,55(11):1036-1042. [DUAN Jianping, WANG Lili, LI Lun, et al. Temperature variability since A.D. 1837 inferred from tree-ring maximum density of Abies fabric in Gongga Mountains, China [J]. Chinese Science Bulletin, 2010, 55(11):1036-1042] DOI: 10.3969/j.issn.1002-0799.2014.04.001

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备注/Memo

备注/Memo:
收稿日期(Received date):2019-06-11; 改回日期(Accepted date): 2021-04-23
基金项目(Foundation item):国家自然科学基金(51669016,51869016); 内蒙古自治区“草原英才”工程[National Natural Science Foundation of China(51669016,51869016); Inner Mongolia Autonomous Region "Grassland Talents" Project]
作者简介(Biography):周莹(1995-),女,内蒙古乌兰察布市人,硕士研究生,主要研究方向:水文学及水资源、气候变化、环境演变及三者间的响应关系。[ZHOU Ying(1995-), female, born in Wulanchabu, Inner Mongolia Autonomous Region, M.Sc. candidate, research on hydrology and water resources, climate change, environmental evolution and their response]E-mail:1352348024@qq.com
*通讯作者(Corresponding author):马龙(1978-),男,博士,教授,主要研究方向:水文学及水资源、气候变化、环境演变及三者间的响应关系。[MA Long(1978-), male, Ph.D.,professor, specialized in hydrology and water resources, climate change, environmental evolution and their response]E-mail: malong4444333@163.com
更新日期/Last Update: 2021-05-30