[1]Liu B,Liang E,Liu K,et al.Species-and elevation-dependent
growth responses to climate warming of mountain forests in the Qin-
ling Mountains,central China [J].Forests,2018,9 (5):248.
[2]Gao S,Liang E,Liu R,et al.An earlier start of the thermal
growing season enhances tree growth in cold humid areas but not in
dry areas [J].Nature ecology evolution,2022,6 (4):397-404.
[3]岳伟鹏,陈峰,袁玉江,等。气侯变暖背景下云南西北部大果
红杉径向生长衰退及其气侯驱动因子分析[J].生态学报,022,
42(06):2331-2341.
[4]Babst F,Bouriaud O,Poulter B,et al.Twentieth century redistri-
bution in climatic drivers of global tree growth [J].Science Ad-
vances,2019,5(1):4313.
[5]黄敬文,张冬有,王兆鹏,等。气侯变化对大兴安岭地区不同
海拔落叶松径向生长的影响[J].东北林业大学学报,2023,
51(11):10-20.
[6]史丰鸣,杨睿,石松林,等.川西南高山松径向生长对气侯响
应的时空分异特征[J].山地学报,2023,41(04):478-492.
[7]Douglass A E.Solar records in tree growth J].Science,1927,
65(1679):220-221.
[8]Fritts H C.Tree Rings and Climate M].London:Academic
Press,1976.
[9]Quinn F H,Sellinger C E.A Reconstruction of Lake Michigan-
Huron Water Levels Derived fromTree Ring Chronologies for the Peri-
od 1600-1961 [J].Joumal of Great Lakes Research,2006,32
(1):29-39.
[10]Aryal S,Gaire N P,Pokhrel N R,et al.Spring season in west-
em Nepal Himalaya is not yet warming:a 400-year temperature
reconstruction based on tree-ring widths of Himalayan Hemlock
(Tsuga dumosa)[J].Atmosphere,2020,11 (2)132.
[11]Panthi S,Briiuning A,Zhou Z K,et al.Tree rings reveal recent
intensified spring drought in the central Himalaya,Nepal [J].
Global and Planetary Change,2017,157:26-34.
[12]Zheng L,Gaire N P,Shi P.High-altitude tree growth responses
to climate change across the Hindu Kush Himalaya [J ]Journal of
Plant Ecolog,2021,14(5):829-842.
[3]吴祥定,孙力,程志刚.若干西藏高原上树木年轮年表的建
立[J].科学通报,1988(08):616-619.
[14]于德水,卢杰,张萌,等。西藏色季拉山西藏红杉径向生长
对气温和降水波动的响应[J].林业科学研究,2023,36(01):
91-99.[15]D'Arrigo R,Wilson R,Liepert B,et al.On the 'divergence
problem'in northem forests:a review of the tree-ring evidence
and possible causes [J].Global and planetary change,2008,60
(3-4):289-305.
[16]Keyimu M,Li Z,Jiao L,et al.Radial growth response of Quer-
cus liaotungensis to climate change-a case study on the central Lo-
ess Plateau,China [J].Trees,2022,36 (6):1811-1822.
[17]薛盼盼,缪宁,岳喜明,等。青藏高原东缘岷江冷杉径向生
长对升温响应分异的坡向和海拔差异[J].林业科学,2023,
59(07):65-77.
[18]盖学瑞,于大炮,王守乐,等。树轮一气候“分异问题”形
成机制的研究进展[J].生态学杂志,2017,36(11):3273
-3280.
[19]周子建,江源,董满字,等.长白山北坡不同海拔红松径向
生长-气侯因子关系对气温突变的响应[J].生态学报,2018,38
(13):4668-4676
[20]薛儒鸿,焦亮,刘小萍,等.新疆阿尔泰山不同海拔西伯利
亚落叶松径向生长对气候变化的响应稳定性评价[J].生态
学杂志,2021,40(05):1275-1284.
[21]曾令兵,王襄平,常锦峰,等。祁连山中段青海云杉高山林
线交错区树轮宽度与气侯变化的关系[J].北京林业大学学
报,2012,34(05):50-56.
[22]Yang B,He M,Shishov V,et al.New perspective on spring
vegetation phenology and global climate change based on Tibetan
Plateau tree-ring data [J].Proceedings of the National Academy
of Sciences,2017,114(27):6966-6971.
[23]陶琴,陈星.青藏高原树轮点气侯要素确定及气侯响应分析
[C].中国气象学会.第35届中国气象学会年会S3高原天气
气侯研究进展.2018:13.[24]Song L,Li M,Zhu J,et al.Comparisons of radial growth and
tree-ring cellulose813C for Pinus sylvestris var.mongolica in natu-
ral and plantation forests on sandy lands J].Joumal of Forest
Research,2017,22(3):160-168.
[25]Qi Z,Liu H,Wu X,et al.Climate-driven speedup of alpine
treeline forest growth in the Tianshan Mountains,Northwestern
China [J].Global Change Biology,2015,21 (2):816-826.
[26]D'orangeville L,Duchesne L,Houle D,et al.Northeastem
North America as a potential refugium for boreal forests in a war-
ming climate [J].Science,2016,352 (6292)1452-1455.
[27]张梵,尹定财,田昆,等。玉龙雪山不同海拔丽江云杉径向
生长对气侯变异的响应[J].植物生态学报,2018,42(06):
629-639.
[28]韩艳刚,盖学瑞,邱思玉,等。大兴安岭兴安落叶松径向生
长对气侯响应的时空变化[J].应用生态学报,2021,32
(10):3397-3404.
[29]夏敬清,勾晓华,王玲玲,等。祁连山西部青海云杉径向生
长对气侯因子的响应[J].应用生态学报,2021,32(10):
3585-3593. |