哈巴雪山高山松径向生长对气候变化的响应
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摘要
基于树木年轮学方法,在哈巴雪山海拔上、下限采集高山松年轮样本,建立差值年表并分析其与气候因子关系,以揭示影响该区域高山松(Pinus densata)径向生长的主要气候因子。结果表明:海拔上限高山松径向生长主要受上年8月水热状况影响,还与当年3月平均最高温呈显著正相关、与5月平均温和6月降水均呈显著负相关;海拔下限高山松径向生长主要受当年5月水热状况影响,还与上年12月降水呈显著正相关;哈巴雪山高山松径向生长与气候因子关系较为稳定。通过对横断山区树轮研究的补充,可为未来气候变化下森林保护提供理论依据。
Based on the dendrochonological method,we collected tree ring samples at upper and lower distributional limits of Pinus densata in Haba Snow Mountain to reveal the key climatic factors affecting tree radial growth by studying the relationship between residual chronologies and climatic factors.The results showed that radial growth of P.densata at the upper distributional limits was mainly affected by the hydrothermal condition in previous August,its growth was also significantly correlated with monthly maximum temperature in current March(positive),monthly mean temperature in current May(negative),and precipitation in current June(negative). At lower distributional limits,hydrothermal condition in current May was the main factor affecting its radial growth,while precipitation in December of previous year also promoted its growth.The relationship between the radial growth of P.densata and climate factors was stable.This study is a favorable supplement to the tree ring research in Hengduan Mountains,and it can also provide a theoretical basis for forest protection under future climate change.
Based on the dendrochonological method,we collected tree ring samples at upper and lower distributional limits of Pinus densata in Haba Snow Mountain to reveal the key climatic factors affecting tree radial growth by studying the relationship between residual chronologies and climatic factors.The results showed that radial growth of P.densata at the upper distributional limits was mainly affected by the hydrothermal condition in previous August,its growth was also significantly correlated with monthly maximum temperature in current March(positive),monthly mean temperature in current May(negative),and precipitation in current June(negative). At lower distributional limits,hydrothermal condition in current May was the main factor affecting its radial growth,while precipitation in December of previous year also promoted its growth.The relationship between the radial growth of P.densata and climate factors was stable.This study is a favorable supplement to the tree ring research in Hengduan Mountains,and it can also provide a theoretical basis for forest protection under future climate change.
引文
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[12] 张贇,尹定财,田昆,等.滇西北海拔上限大果红杉径向生长对气候变化的响应[J].应用生态学报,2017,28(9):2805-2812.
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[24] 彭剑锋,勾晓华,陈发虎,等.阿尼玛卿山地不同海拔青海云杉(Picea crassifolia)树轮生长特征及其对气候的响应[J].生态学报,2007,27(8):3268-3276.
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[27] M?kinen H,N?jd P,Kahle H P,et al.Radial growth variation of Norway spruce (Picea abies,(L.)Karst.) across latitudinal and altitudinal gradients in central and northern Europe[J].Forest Ecology & Management,2002,171(3):243-259.
[28] Rolland C.Tree-ring and climate relationships for Abies alba in the internal Alps[J].Tree-ring Bulletin 1993,53:1-11.
[29] 林康.冬夏树木涂白的作用[J].云南林业,1984(6):23.
[30] Fan Zexin,Br?uning A,Cao Kunfang,et al.Growth-climate responses of high-elevation conifers in the central Hengduan Mountains,southwestern China[J].Forest Ecology & Management,2009,258(3):306-313.
[31] 张卫国,肖德荣,田昆,等.玉龙雪山3个针叶树种在海拔上限的径向生长及气候响应[J].生态学报,2017,37(11):3796-3804.
[32] Panthi S,Br?uning A,Zhou Zhekun,et al.Growth response of Abies georgei,to climate increases with elevation in the central Hengduan Mountains,southwestern China[J].Dendrochronologia,2018,47(2-3):1-9.
[33] Vaganov E A,Hughes M K,Kirdyanov A V,et al.Influence of snowfall and melt timing on tree growth in subarctic Eurasia[J].Nature,1999,400(6740):149-151.
[34] Zhang Yun,Bergeron Y,Zhao Xiuhai,et al.Stand history is more important than climate in controlling red maple (Acer rubrum L.) growth at its northern distribution limit in western Quebec,Canada[J].Journal of Plant Ecology,2015,8(4):368.
[2] 郑淑霞,上官周平.树木年轮与气候变化关系研究[J].林业科学,2006,42(6):100-107.
[3] 李腾,何兴元,陈振举.东北南部蒙古栎径向生长对气候变化的响应——以千山为例[J].应用生态学报,2014,25(7):1841-1848.
[4] Liang Eryuan,Liu Bo,Zhu Liping,et al.A short note on linkage of climatic records between a river valley and the upper timberline in the Sygera Mountains,Southeastern Tibetan Plateau[J].Global and Planetary Change,2011,77(1):97-102.
[5] Yu Dapao,Wang G G,Dai Limin,et al.Dendroclimatic analysis of Betula ermanii forests at their upper limit of distribution in Changbai Mountain[J],Northeast China.Forest Ecology and Management,2007,240(1/3):105-113.
[6] 张贇,尹定财,张卫国,等.普达措国家公园2个针叶树种径向生长对温度和降水的响应[J].生态学报,2018,38(15):5373-5382.
[7] 段建平,王丽丽,徐岩,等.贡嘎山东坡不同海拔高度树轮宽度对气候变化的响应[J].地理研究,2010,29(11):1940-1949.
[8] 陈力,尹云鹤,赵东升,等.长白山不同海拔树木生长对气候变化的响应差异[J].生态学报,2014,34(6):1568-1574.
[9] Zhang Yun,Yin Dingcai,Sun Mei,et al.Variations of Climate-Growth Response of Major Conifers at Upper Distributional Limits in Shika Snow Mountain,Northwestern Yunnan Plateau,China[J].Forests,2017,8(10):377.
[10] Fan Zexin,Br?uning A,Cao Kun Fang.Annual temperature reconstruction in the central Hengduan Mountains,China,as deduced from tree rings[J].Dendrochronologia,2008,26(2):97-107.
[11] Li Zongshan,Shi Chunming,Liu Yongbo,et al.Summer mean temperature variation from 1710-2005 inferred from tree-ring data of the Baimang Snow Mountains,northwestern Yunnan,China[J].Climate Research,2011,47(3):207-218.
[12] 张贇,尹定财,田昆,等.滇西北海拔上限大果红杉径向生长对气候变化的响应[J].应用生态学报,2017,28(9):2805-2812.
[13] 张贇,尹定财,田昆,等.玉龙雪山不同海拔丽江云杉径向生长对气候变异的响应[J].植物生态学报,2018,42(6):629-639.
[14] 陶晶,臧润国,余昌元.云南哈巴雪山植物群落和植物多样性海拔梯度分布格局[J].林业科学,2011,47(7):1-6.
[15] 吴征镒,朱彦丞.云南植被[M].科学出版社,1987.
[16] Larsson L A.CDendro V.7.3.Cybis Elektronik & Data AB[M].Sweden:Saltsj?baden,2010.
[17] Holmes R L.Computer-assisted quality control in tree-ring dating and measurement[J].Tree-Ring Bulletin,1983,43:69-75.
[18] Cook E R,Holmes R L.Users Manual for Program ARSTAN.Tucson:Laboratory of Tree-ring Research[M].University of Arizona,1996:81.
[19] 邵雪梅,吴祥定.华山树木年轮年表的建立[J].地理学报,1994(2):174-181.
[20] Biondi F,Waikul K.DENDROCLIM2002:a C++ program for statistical calibration of climate signals in tree-ring chronologies[J].Computers & Geosciences,2004,30(3):303-311.
[21] Blasing T J,Solomon A M,Ducick D N.Response function revisited[J].Tree-ring bulletin,1984,44(19):1-15.
[22] Qin Li,Yuan Yujiang,Zhang Ruibo,et al.Tree-ring response to snow cover and reconstruction of century annual maximum snow depth for northern Tianshan Mountains,China[J].Geochronometria,2016,43(1):9-17.
[23] Liang Eryuan,Shao Xuemei,Hu Yuxi,et al.Dendroclimatic evaluation of climate-growth relationships of meyer spruce (Picea meyeri) on a sandy substrate in semi-arid grassland,north China[J].Trees,2001,15(4):230-235.
[24] 彭剑锋,勾晓华,陈发虎,等.阿尼玛卿山地不同海拔青海云杉(Picea crassifolia)树轮生长特征及其对气候的响应[J].生态学报,2007,27(8):3268-3276.
[25] 李江风.树木年轮水文学研究与应用[M].科学出版社,2000.
[26] 赵志江,谭留夷,康东伟,等.云南小中甸地区丽江云杉径向生长对气候变化的响应[J].应用生态学报,2012,23(3):603-609.
[27] M?kinen H,N?jd P,Kahle H P,et al.Radial growth variation of Norway spruce (Picea abies,(L.)Karst.) across latitudinal and altitudinal gradients in central and northern Europe[J].Forest Ecology & Management,2002,171(3):243-259.
[28] Rolland C.Tree-ring and climate relationships for Abies alba in the internal Alps[J].Tree-ring Bulletin 1993,53:1-11.
[29] 林康.冬夏树木涂白的作用[J].云南林业,1984(6):23.
[30] Fan Zexin,Br?uning A,Cao Kunfang,et al.Growth-climate responses of high-elevation conifers in the central Hengduan Mountains,southwestern China[J].Forest Ecology & Management,2009,258(3):306-313.
[31] 张卫国,肖德荣,田昆,等.玉龙雪山3个针叶树种在海拔上限的径向生长及气候响应[J].生态学报,2017,37(11):3796-3804.
[32] Panthi S,Br?uning A,Zhou Zhekun,et al.Growth response of Abies georgei,to climate increases with elevation in the central Hengduan Mountains,southwestern China[J].Dendrochronologia,2018,47(2-3):1-9.
[33] Vaganov E A,Hughes M K,Kirdyanov A V,et al.Influence of snowfall and melt timing on tree growth in subarctic Eurasia[J].Nature,1999,400(6740):149-151.
[34] Zhang Yun,Bergeron Y,Zhao Xiuhai,et al.Stand history is more important than climate in controlling red maple (Acer rubrum L.) growth at its northern distribution limit in western Quebec,Canada[J].Journal of Plant Ecology,2015,8(4):368.
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