滇西不同海拔云南松径向生长对气候水文要素的响应

doi:10.13287/j.1001-9332.202110.016

应用生态学报 ›› 2021, Vol. 32 ›› Issue (10): 3557-3566.doi: 10.13287/j.1001-9332.202110.016

滇西不同海拔云南松径向生长对气候水文要素的响应

王世杰¹, 陈友平¹, 陈峰^1,2*, 张合理^1,2

¹云南大学, 国际河流与生态安全研究院国际河流与跨境生态安全重点实验室, 昆明 650504;
²中国气象局乌鲁木齐沙漠气象研究所, 树木年轮理化研究重点开放实验室/新疆树木年轮生态实验室, 乌鲁木齐 830002

收稿日期:2021-04-13 修回日期:2021-07-22 出版日期:2021-10-15 发布日期:2022-04-15
通讯作者: * E-mail: feng653@163.com
作者简介:王世杰, 男, 1998年生, 硕士研究生。主要从事树木年轮与气候变化研究。E-mail: wsj1569@163.com
基金资助:
国家自然科学基金项目(32061123008)资助

Responses of radial growth of Pinus yunnanensis to climatic and hydrological factors at different altitudes in Western Yunnan, China

WANG Shi-jie¹, CHEN You-ping¹, CHEN Feng^1,2*, ZHANG He-li^1,2

¹Yunnan Key Laboratory of International Rivers and Transboundary Eco-Security, Institute of International Rivers and Eco-security, Yunnan University, Kunming 650504, China;
²Key Laboratory of Tree-ring Physical and Chemic Research of China Meteorological Administration/Key Laboratory of Tree-ring Ecology of Uigur Autonomous Region, Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China

Received:2021-04-13 Revised:2021-07-22 Online:2021-10-15 Published:2022-04-15
Contact: * E-mail: feng653@163.com
Supported by:
National Natural Science Foundation of China (32061123008).

摘要/Abstract

摘要： 利用滇西地区两个不同海拔采样点的云南松树轮样本,建立树轮宽度标准化年表,研究其径向生长对气候和水文要素的响应。结果表明:滇西云南松径向生长主要受降水量、气温和径流量的影响,其中高海拔(2413.3 m)云南松径向生长受夏季高温的制约和季风季节径流量影响,而低海拔(1062.6 m)云南松径向生长受生长季的降水量和全年径流量影响。滇西高海拔云南松径向生长对气温变化的响应受温度阈值影响表现出不稳定性;低海拔云南松径向生长对降水量和径流量的响应,在20世纪80年代均受到东亚夏季风的减弱而出现波动。滇西不同海拔云南松径向生长与亚洲夏季风活动及厄尔尼诺存在联系。

关键词: 云南松, 海拔, 径向生长, 气候变化

Abstract: A tree-ring width chronology (STD) was established using tree-ring cores of Pinus yunnanensis from two sites with different altitudes in Western Yunnan, to study the responses of radial growth to climatic and hydrological factors. The results showed that the radial growth of P. yunnanensis in Western Yunnan was mainly affected by precipitation, temperature and runoff. The radial growth of P. yunnanensis at high altitude (2413.3 m) was controlled primarily by high temperature in summer and runoff in the monsoon season. In contrast, the radial growth of P. yunnanensis at low altitude (1062.6 m) was mainly controlled by precipitation in the growing season and annual runoff. The responses of radial growth of P. yunnanensis at high altitude to temperature change was unstable due to the existence of the temperature threshold. Due to the weakening of the East Asian summer monsoon in the 1980s, the temporal stability of tree growth response at low altitude to precipitation and runoff fluctuated. The radial growth of P. yunnanensis at different altitudes in Western Yunnan was related to the Asian summer monsoon and El Nio-Southern Oscillation.

Key words: Pinus yunnanensis, altitude, radial growth, climate change

王世杰, 陈友平, 陈峰, 张合理. 滇西不同海拔云南松径向生长对气候水文要素的响应[J]. 应用生态学报, 2021, 32(10): 3557-3566.

WANG Shi-jie, CHEN You-ping, CHEN Feng, ZHANG He-li. Responses of radial growth of Pinus yunnanensis to climatic and hydrological factors at different altitudes in Western Yunnan, China[J]. Chinese Journal of Applied Ecology, 2021, 32(10): 3557-3566.

参考文献

[1] 秦大河. 气候变化科学与人类可持续发展. 地理科学进展, 2014, 33(7): 874-883 [Qin D-H. Climate change science and sustainable development. Progress in Geography, 2014, 33(7): 874-883]
[2] Qian WH, Chen D, Zhu Y, et al. Temporal and spatial variability of dryness/wetness in China during the last 530 years. Theoretical and Applied Climatology, 2003, 76: 13-29
[3] 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. 应用生态学报, 2012, 23(3): 603-609 [Zhao Z-J, Tan L-Y, Kang D-W, et al. Responses of Picea likiangensis radial growth to climate change in the Small Zhongdian area of Yunnan Province, Southwest China. Chinese Journal of Applied Ecology, 2012, 23(3): 603-609]
[4] 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. 生态学杂志, 2021, 40(5): 1275-1284 [Xue R-H, Jiao L, Liu X-P, et al. Evaluation of the stability of the radial growth of Larix sibirica at different altitudes in response to climate change in Altai Mountains, Xinjiang. Chinese Journal of Ecology, 2021, 40(5): 1275-1284]
[5] 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. 应用生态学报, 2017, 28(9): 2805-2812 [Zhang Y, Yin D-C, Tian K, et al. Response of radial growth of Larix potaninii var. macrocarpa to climate change at upper distributional limits on Northwestern Yunnan Plateau, China. Chinese Journal of Applied Ecology, 2017, 28(9): 2805-2812]
[6] 梁亚群, 陈友平, 陈峰, 等. 滇西北干热河谷地区1850年以来的干湿变化. 干旱区资源与环境, 2020, 34(6): 81-86 [Liang Y-Q, Chen Y-P, Chen F, et al. Drought variation for the dry-hot valley area of Northwest Yunnan since 1850 CE. Journal of Arid Land Resources and Environment, 2020, 34(6): 81-86]
[7] Yang B, Chen XH, He YH, et al. Reconstruction of annual runoff since CE 1557 using tree-ring chronologies in the upper Lancang-Mekong River basin. Journal of Hydrology, 2019, 569: 771-781
[8] 何大明. 澜沧江──湄公河水文特征分析. 云南地理环境研究, 1995, 7(1): 58-74 [He D-M. Analysis of hydrological characteristics in Lancang-Mekong River. Yunnan Geographic Environment Research, 1995, 7(1): 58-74]
[9] 王泉泉, 王行, 张卫国, 等. 滇西北高原湿地景观变化与人为、自然因子的相关性. 生态学报, 2019, 39(2): 726-738 [Wang Q-Q, Wang X, Zhang W-G, et al. The correlations between wetland landscape and social-natural factors on Northwestern Yunnan Plateau. Acta Ecologica Sinica, 2019, 39(2): 726-738]
[10] 方克艳, 杨保, 郑怀舟, 等. 树轮学研究方法及其在全球变化中的应用. 第四纪研究, 2015, 35(5): 1283-1293 [Fang K-Y, Yang B, Zheng H-Z, et al. Applying tree-ring methods in the global changes stu-dies. Quaternary Sciences, 2015, 35(5): 1283-1293]
[11] 陈友平, 陈峰, 张合理, 等. 树轮记录的自公元1200年以来强火山喷发事件与高亚洲南部河流源区气候水文变化的关联. 第四纪研究, 2021, 41(2): 323-333 [Chen Y-P, Chen F, Zhang H-L, et al. Strong link of large volcanic eruptions and climatic and hydrological changes recorded by tree rings in the river source area of southern high Asia since 1200 A.D. Quaternary Sciences, 2021, 41(2): 323-333]
[12] 张东, 宋献方, 张应华, 等. 基于CRU格点数据集的近百年渭河流域降水变化. 干旱区资源与环境, 2018, 32(2): 142-148 [Zhang D, Song X-F, Zhang Y-H, et al. Variation characteristics of precipitation over Weihe River basin based on CRU grid dataset during last 100 years. Journal of Arid Land Resources and Environment, 2018, 32(2): 142-148]
[13] 杜灵通, 田庆久, 刘可, 等. 气候变化背景下区域干旱监测理论与实践. 北京: 科学出版社, 2017: 31-34 [Du L-T, Tian Q-J, Liu K, et al. Theory and Practice of Regional Drought Monitoring in the Context of Climate Change. Beijing: Science Press, 2017: 31-34]
[14] Rodwell MJ, Rowell DP, Folland CK. Oceanic forcing of the wintertime North Atlantic Oscillation and European climate. Nature, 1999, 398: 320-323
[15] Li JP, Zheng QC. A new monsoon index and the geographical distribution of the global monsoons. Advances in Atmospheric Sciences, 2003, 20: 299-302
[16] 乔晶晶, 王童, 潘磊, 等. 不同海拔和坡向马尾松树轮宽度对气候变化的响应. 应用生态学报, 2019, 30(7): 2231-2240 [Qiao J-J, Wang T, Pan L, et al. Responses of radial growth to climate change in Pinus massoniana at different altitudes and slopes. Chinese Journal of Applied Ecology, 2019, 30(7): 2231-2240]
[17] 韩艳刚, 周旺明, 齐麟, 等. 长白山树木径向生长对气候因子的响应. 应用生态学报, 2019, 30(5): 1513-1520 [Han Y-G, Zhou W-M, Qi L, et al. Tree radial growth-climate relationship in Changbai Mountain, Northeast China. Chinese Journal of Applied Ecology, 2019, 30(5): 1513-1520]
[18] 李大稳. 闽东南树轮宽度和稳定碳同位素研究. 硕士论文. 福州: 福建师范大学, 2017 [Li D-W. Investigations of Tree-ring Growths and Stable Isotopes in Southeast of Fujian Province. Master Thesis. Fuzhou: Fujian Normal University, 2017]
[19] 林学椿. 统计天气预报中相关系数的不稳定性问题. 大气科学, 1978, 2(1): 55-63 [Lin X-C. Instability of correlation coefficient in statistical weather forecast. Chinese Journal of Atmospheric Sciences, 1978, 2(1): 55-63]
[20] Wang HQ, Chen F. Increased stream flow in the Nu River (Salween) Basin of China, due to climatic warming and increased precipitation. Geografiska Annaler, 2017, 99: 1-11
[21] Wigley T, Briffa KR, Jones PD. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Climate and Applied Meteorology, 1984, 23: 201-213
[22] 刘磊, 李小雁, 蒋志云, 等. 青海湖流域不同海拔高度土壤水分时空变化特征. 资源科学, 2017, 39(2): 263-275 [Liu L, Li X-Y, Jiang Z-Y, et al. Variation in soil water content along different altitude gradients in the Qinghai Lake Watershed. Resources Science, 2017, 39(2): 263-275]
[23] Rossi S, Anfodillo T, čufar K, et al. Pattern of xylem phenology in conifers of cold ecosystems at the Northern Hemisphere. Global Change Biology, 2016, 22: 3804-3813
[24] 申佳艳, 李帅锋, 黄小波, 等. 金沙江流域不同海拔处云南松生态弹性及生长衰退过程. 林业科学, 2020, 56(6): 1-11 [Shen J-Y, Li S-F, Huang X-B, et al. Ecological resilience and growth degradation of Pinus yunnanensis at different altitudes in Jinsha River basin. Scientia Silvae Sinicae, 2020, 56(6): 1-11]
[25] 于健, 陈佳佳, 周光, 等. 横断山脉中部川滇冷杉和丽江云杉径向生长对气象因子的响应. 林业科学, 2020, 56(12): 28-38 [Yu J, Chen J-J, Zhou G, et al. Response of radial growth of Abies forrestii and Picea likiangensis to climate factors in the central Hengduan Mountains, southwest China. Scientia Silvae Sinicae, 2020, 56(12): 28-38]
[26] 于健, 刘琪璟, 周光, 等. 小兴安岭红松和鱼鳞云杉径向生长对气候变化的响应. 应用生态学报, 2017, 28(11): 3451-3460 [Yu J, Liu Q-J, Zhou G, et al. Response of radial growth of Pinus koraiensis and Picea jezoensis to climate change in Xiaoxing'anling Mountains, Northeast China. Chinese Journal of Applied Ecology, 2017, 28(11): 3451-3460]
[27] 韩金生, 赵慧颖, 朱良军, 等. 小兴安岭蒙古栎和黄菠萝径向生长对气候变化的响应比较. 应用生态学报, 2019, 30(7): 2218-2230 [Han J-S, Zhao H-Y, Zhu L-J, et al. Comparing the responses of radial growth between Quercus mongolica and Phellodendron amurense to climate change in Xiaoxing'an Mountains, China. Chinese Journal of Applied Ecology, 2019, 30(7): 2218-2230]
[28] 吕朝阳, 贠瑞鑫, 吴涛, 等. 寒温带森林白桦径向生长的海拔差异及其气候响应——以奥克里堆山为例. 应用生态学报, 2020, 31(6): 1889-1897 [Lyu Z-Y, Yun R-X, Wu T, et al. Altitudinal differentiation in the radial growth of Betula platyphylla and its response to climate in cold temperate forest: A case of Oakley Mountain, Northeast China. Chinese Journal of Applied Ecology, 2020, 31(6):1889-1897]
[29] Chang CP, Zhang Y, Li T. Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs. Part I: Roles of the subtropical ridge. Journal of Climate, 2000, 13: 4310-4325
[30] 樊毅, 李靖, 仲远见, 等. 基于R/S分析法的云南干热河谷降水变化趋势分析. 水电能源科学, 2008, 26(2): 24-27 [Fan Y, Li J, Zhong Y-J, et al. Regional water resources vantage evaluation model based on exergy analysis theory. Water Resources and Power, 2008, 26(2): 24-27]
[31] Panthi S, Braeuning A, Zhou ZK, et al. Tree rings reveal recent intensified spring drought in the central Himalaya, Nepal. Global & Planetary Change, 2017, 157: 26-34
[32] 桓玉, 李跃清. 夏季东亚季风和南亚季风协同作用与我国南方夏季降水异常的关系. 高原气象, 2018, 37(6): 1563-1577 [Huan Y, Li Y-Q. The synergy between the East Asian summer monsoon and the South Asian summer monsoon and its relations with anomalous rainfall in southern China. Plateau Meteorology, 2018, 37(6): 1563-1577]
[33] 范可, 琚建华, 周秀美. 东南亚夏季强降水的基本物理量场的诊断分析. 气象科学, 2004, 24(2): 212-219 [Fan K, Ju J-H, Zhou X-M. The diagnosis for heavy rain in summer in the south-east area. Scientia Meteologica Sinica, 2004, 24(2): 212-219]
[34] Wang B, Clemens SC, Liu P. Contrasting the Indian and East Asian monsoons: Implications on geologic timescales. Marine Geology, 2003, 201: 5-21

滇西不同海拔云南松径向生长对气候水文要素的响应

Responses of radial growth of Pinus yunnanensis to climatic and hydrological factors at different altitudes in Western Yunnan, China

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