利用树轮揭示人类活动对柴达木盆地巴音河径流量的影响

doi:10.13287/j.1001-9332.202110.040

应用生态学报 ›› 2021, Vol. 32 ›› Issue (10): 3653-3660.doi: 10.13287/j.1001-9332.202110.040

利用树轮揭示人类活动对柴达木盆地巴音河径流量的影响

朱晓龙^1,2, 陈庆美³, 吕爱锋³, 黄茹¹, 邵雪梅^2,3, 梁尔源¹, 朱海峰^1*

¹中国科学院青藏高原研究所, 北京 100101;
²中国科学院大学, 北京 100049;
³中国科学院地理科学与资源研究所, 北京 100101

收稿日期:2021-08-19 修回日期:2021-09-14 出版日期:2021-10-15 发布日期:2022-04-15
通讯作者: * E-mail: zhuhf@itpcas.ac.cn
作者简介:朱晓龙, 男, 1995年生, 硕士研究生。主要从事树轮气候学研究。E-mail: zhxl@itpcas.ac.cn
基金资助:
国家自然科学基金项目(41671026)和青海省重大科技专项(2019-SF-A4-1)资助

Impacts of human activity on Bayin River runoff as revealed by tree rings in Qaidam Basin, China

ZHU Xiao-long^1,², CHEN Qing-mei³, LYU Ai-feng³, HUANG Ru¹, SHAO Xue-mei^2,3, LIANG Er-yuan¹, ZHU Hai-feng^1*

¹Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;
²University of Chinese Academy of Sciences, Beijing 100049, China;
³Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China

Received:2021-08-19 Revised:2021-09-14 Online:2021-10-15 Published:2022-04-15
Contact: * E-mail: zhuhf@itpcas.ac.cn
Supported by:
National Natural Science Foundation of China (41671026) and the Important Science & Technology Specific Projects of Qinghai Province (2019-SF-A4-1).

摘要/Abstract

摘要： 评估人类活动对径流的影响,对区域水资源开发管理有借鉴和指导意义。利用柴达木盆地北部山区7个祁连圆柏树轮宽度数据,建立区域平均树轮宽度年表。通过对区域平均树轮宽度年表与巴音河水文站径流量进行相关、滑动相关和回归分析,模拟了巴音河1956—2002年6月天然径流量变化,进而分析出人类活动对径流量的影响。结果表明: 树轮平均年表与6月径流量的相关性最强(r=0.63,P<0.01),两者相关系数在1986年后下降;基于1956—1986年树轮平均年表与6月径流量建立的转换方程,方差解释量为50.8%;基于转换方程模拟的1987—2002年径流量均值与实际观测径流量存在显著差异,模拟均值比观测均值大3.01 m³·s^-1。上游人类活动已经对巴音河径流量的变化带来了明显的影响。因此,在巴音河流域未来水资源开发利用规划中,有必要将人类活动作为重要的影响因素加以考虑,以保障可持续的水资源利用。

关键词: 树木年轮, 径流, 人类活动, 柴达木盆地

Abstract: Evaluating the impacts of human activity on river runoff has important implications for regional water resource management. Here, we used seven tree-ring width chronologies to establish a regional mean tree-ring width chronology from the northern mountain of Delingha, Qaidam Basin. We conducted the correlation, moving correlation and regression analysis of regional mean tree-ring width chronology with runoff data from Bayin River gauge station. Then, we stimulated the June runoff of Bayin River from 1956 to 2002. The results showed that the highest correlation coefficient was found for June runoff (r=0.63, P<0.01), and their moving correlation coefficient decreased after 1986. Based on the stable relationship between tree-ring width chronology and the June runoff during 1956-1986, we built the reconstruction function, which was explained 50.8% of observed runoff. The stimulated runoff during 1987 to 2002 was significantly higher than the observed runoff (3.01 m³·s^-1, P<0.001). These results indicated that human activity from the upper river had significant impacts on Bayin River runoff. Human activity should be considered as an important factor to protect security of sustainable water resource utilization for future water resource development and utilization in Bayin River region.

Key words: tree ring, runoff, human activity, Qaidam Basin

朱晓龙, 陈庆美, 吕爱锋, 黄茹, 邵雪梅, 梁尔源, 朱海峰. 利用树轮揭示人类活动对柴达木盆地巴音河径流量的影响[J]. 应用生态学报, 2021, 32(10): 3653-3660.

ZHU Xiao-long, CHEN Qing-mei, LYU Ai-feng, HUANG Ru, SHAO Xue-mei, LIANG Er-yuan, ZHU Hai-feng. Impacts of human activity on Bayin River runoff as revealed by tree rings in Qaidam Basin, China[J]. Chinese Journal of Applied Ecology, 2021, 32(10): 3653-3660.

参考文献

[1] 德令哈市地方志编纂委员会. 德令哈市志. 北京: 方志出版社, 2004: 1-397 [Delingha Local Chronicles Compilation Committee. Delingha Chronicles. Beijing: China Local Records Press, 2004: 1-397]
[2] 李健, 王建军, 黄勇, 等. 青海德令哈市巴音河流域水资源开发利用. 干旱区研究, 2009, 26(4): 483-489 [Li J, Wang J-J, Huang Y, et al. Analysis on the exploitation and utilization of water resources in the Bayin River watershed, Delingha City, Qinghai Province. Arid Zone Research, 2009, 26(4): 483-489]
[3] 黄斌斌, 郝成元, 李若男, 等. 气候变化及人类活动对地表径流改变的贡献率及其量化方法研究进展. 自然资源学报, 2018, 33(5): 899-910 [Huang B-B, Hao C-Y, Li R-N, et al. Research progress on the quantitative methods of calculating contribution rates of climate change and human activities to surface runoff changes. Journal of Natural Resources, 2018, 33(5): 899-910]
[4] 文广超, 王文科, 段磊, 等. 青海柴达木盆地巴音河上游径流量对气候变化和人类活动的响应. 冰川冻土, 2018, 40(1): 136-144 [Wen G-C, Wang W-K, Duan L, et al. Response of runoff to climate change and human activity in the upper reaches of the Bayin River, Qaidam Basin, Qinghai Province. Journal of Glaciology and Geocryology, 2018, 40(1): 136-144]
[5] Stockton CW, Jacoby GC. Long-term surface-water supply and streamflow trends in the Upper Colorado River basin based on tree-ring analyses. Lake Powell Research Project Bulletin, 1976, 18: 1-70
[6] Rao MP, Cook ER, Cook BI, et al. Seven centuries of reconstructed Brahmaputra River discharge demonstrate underestimated high discharge and flood hazard frequency. Nature Communications, 2020, 11: 6017
[7] Cook ER, Palmer JG, Ahmed M, et al. Five centuries of Upper Indus River flow from tree rings. Journal of Hydrology, 2013, 486: 365-375
[8] Chen F, Opała-Owczarek M, Khan A, et al. Late twentieth century rapid increase in high Asian seasonal snow and glacier-derived streamflow tracked by tree rings of the upper Indus River basin. Environmental Research Letters, 2021, 16: 094055
[9] 李江风, 周文盛, 袁玉江, 等. 利用树木年轮重建额尔齐斯河年径流量. 新疆气象, 1988(9): 26-32 [Li J-F, Zhou W-S, Yuan Y-J, et al. Using tree ring reconstruct Irtysh River runoff. Desert and Oasis Meteorology, 1988(9): 26-32]
[10] Gou XH, Chen FH, Cook E, et al. Streamflow variations of the Yellow River over the past 593 years in wes-tern China reconstructed from tree rings. Water Resources Research, 2007, 43: doi: 10.1029/2006WR005705
[11] 勾晓华, 邓洋, 陈发虎, 等. 黄河上游过去1234年流量的树轮重建与变化特征分析. 科学通报, 2010, 55(33): 3236-3243 [Gou X-H, Deng Y, Chen F-H, et al. Tree ring based streamflow reconstruction for the upper Yellow River over the past 1234 years. Chinese Science Bulletin, 2010, 55(33): 3236-3243]
[12] 肖丁木, 黄小梅, 秦宁生. 树轮记录的黄河源区过去390 a流量变化. 自然资源学报, 2017, 32(9): 1568-1578 [Xiao D-M, Huang X-M, Qin N-S. Streamflow reconstruction based on tree ring in the source region of Yellow River region over the past 390 years. Journal of Natural Resources, 2017, 32(9): 1568-1578]
[13] Li JB, Xie SP, Cook ER, et al. Deciphering human contributions to Yellow River flow reductions and downstream drying using centuries-long tree ring records. Geophysical Research Letters, 2019, 46: 898-905
[14] Liu Y, Song HM, An ZS, et al. Recent anthropogenic curtailing of Yellow River runoff and sediment load is unprecedented over the past 500 y. Proceedings of the National Academy of Sciences of the United States of America, 2020, 117: 18251-18257
[15] 秦宁生, 靳立亚, 时兴合, 等. 利用树轮资料重建通天河流域518年径流量. 地理学报, 2004, 59(4): 550-556 [Qin N-S, Jin L-Y, Shi X-H, et al. A 518-year runoff reconstruction of Tongtian River basin using tree-ring width chronologies. Acta Geographica Sinica, 2004, 59(4): 550-556]
[16] 李媛媛, 秦宁生, 时兴合, 等. 近714年扎曲河流域径流量的重建和变化特征. 高原气象, 2015, 34(4): 1065-1073 [Li Y-Y, Qin N-S, Shi X-H, et al. Reconstruction and variation of Zhaqu River runoff in recent 714 years. Plateau Meteorology, 2015, 34(4): 1065-1073]
[17] Liu Y, Sun JY, Song HM, et al. Tree-ring hydrologic reconstructions for the Heihe River watershed, western China since AD 1430. Water Research, 2010, 44: 2781-2792
[18] 刘普幸, 陈发虎, 靳立亚, 等. 基于胡杨年轮重建黑河下游近100年春季径流量. 干旱区地理, 2007, 30(5): 696-700 [Liu P-X, Chen F-H, Jin L-Y, et al. About 100-year reconstruction of spring streamflow based on tree rings in the lower reaches of Heihe River. Arid Land Geography, 2007, 30(5): 696-700]
[19] 刘义花, 汪青春, 马占良, 等. 利用多条树轮重建黑河上游地区540年径流量. 干旱区资源与环境, 2009, 23(3): 93-97 [Liu Y-H, Wang Q-C, Ma Z-L, et al. 540-year runoff reconstruction of upper Heihe River using tree-ring chronology. Journal of Arid Land Resources and Environment, 2009, 23(3): 93-97]
[20] Chen F, Shang HM, Panyushkina IP, et al. Tree-ring reconstruction of Lhasa River streamflow reveals 472 years of hydrologic change on southern Tibetan Plateau. Journal of Hydrology, 2019, 572: 169-178
[21] Zhang QB, Cheng GD, Yao TD, et al. A 2326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophysical Research Letters, 2003, 30, doi: 10.1029/2003GL017425
[22] 邵雪梅, 黄磊, 刘洪滨, 等. 树轮记录的青海德令哈地区千年降水变化. 中国科学D辑: 地球科学, 2004, 34(2): 145-153 [Shao X-M, Huang L, Liu H-B, et al. Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai. Science in China Series D: Earth Sciences, 2004, 34(2): 145-153]
[23] 刘禹, 安芷生, 马海州, 等. 青海都兰地区公元850年以来树轮记录的降水变化及其与北半球气温的联系. 中国科学D辑: 地球科学, 2006, 36(5): 461-471 [Liu Y, An Z-S, Ma H-Z, et al. Tree-ring based precipitation change since AD 850 in Dulan area of Qinghai Province and its association with Northern Hemi-spheric temperature. Science in China Series D: Earth Sciences, 2006, 36(5): 461-471]
[24] Yang B, Qin C, Wang JL, et al. A 3500-year tree-ring record of annual precipitation on the northeastern Tibe-tan Plateau. Proceedings of the National Academy of Sciences of the United States of America, 2014, 111: 2903-2908
[25] Yang B, Qin C, Bräuning A, et al. Long-term decrease in Asian monsoon rainfall and abrupt climate change events over the past 6700 years. Proceedings of the National Academy of Sciences of the United States of America, 2021, 118: e2102007118
[26] Yin ZY, Shao XM, Qin NS, et al. Reconstruction of a 1436-year soil moisture and vegetation water use history based on tree-ring widths from Qilian junipers in northeastern Qaidam Basin, northwestern China. International Journal of Climatology, 2008, 28: 37-53
[27] Yin ZY, Zhu HF, Huang L, et al. Reconstruction of biological drought conditions during the past 2847years in an alpine environment of the northeastern Tibetan Plateau, China, and possible linkages to solar forcing. Global and Planetary Change, 2016, 143: 214-227
[28] Liu Y, An ZS, Linderholm HW, et al. Annual temperatures during the last 2485 years in the mid-eastern Tibe-tan Plateau inferred from tree rings. Science in China Series D: Earth Sciences, 2009, 52: 348-359
[29] 朱海峰, 郑永宏, 邵雪梅, 等. 树木年轮记录的青海乌兰地区近千年温度变化. 科学通报, 2008, 35(15): 1835-1841 [Zhu H-F, Zheng Y-H, Shao X-M, et al. Millennial temperature reconstruction based on tree-ring widths of Qilian juniper from Wulan, Qinghai Province, China. Chinese Science Bulletin, 2008, 35(15): 1835-1841]
[30] 甘小莉, 郝玉培, 翟永洪, 等. 巴音河流域植被与水文动态变化研究. 水土保持研究, 2014, 21(2): 323-326 [Gan X-L, Hao Y-P, Zhai Y-H, et al. Study on dynamic change of vegetation and hydrology in Bayin River basin. Research of Soil and Water Conservation, 2014, 21(2): 323-326]
[31] 梁晓燕, 莫淑红, 巩瑶, 等. 巴音河流域气象要素变化特性探析. 电网与清洁能源, 2019, 35(10): 82-89 [Liang X-Y, Mo S-H, Gong Y, et al. Analysis on the change characteristics of meteorological elements in the Bayin River Basin. Power System and Clean Energy, 2019, 35(10): 82-89]
[32] Shao XM, Xu Y, Yin ZY, et al. Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau. Quaternary Science Reviews, 2010, 29: 2111-2122
[33] Melvin TM, Briffa KR. CRUST: Software for the implementation of Regional Chronology Standardisation: Part 1. Signal-Free RCS. Dendrochronologia, 2014, 32: 7-20
[34] Melvin TM, Briffa KR. A ‘signal-free’ approach to dendroclimatic standardisation. Dendrochronologia, 2008, 26: 71-86
[35] 赵佳辉. 巴音河流域农田灌溉模式对地下水补给的影响研究. 硕士论文. 西安: 长安大学, 2018 [Zhao J-H. Effects of Farmland Irrigation Modes on Groundwater Recharge in Bayin River Basin. Master Thesis. Xi’an: Chang’an University, 2018]
[36] Zang C, Biondi F. treeclim: An R package for the numerical calibration of proxy-climate relationships. Ecography, 2015, 38: 431-436
[37] Michaelsen J. Cross-validation in statistical climate forecast models. Journal of Applied Meteorology and Climatology, 1987, 26: 1589-1600
[38] Fritts HC. Tree Rings and Climate. London: Academic Press, 1976: 1-567
[39] Durbin J, Watson GS. Testing for serial correlation in least squares regression. Ⅱ. Biometrika, 1951, 38: 159-177
[40] 郑永宏, 朱海峰, 张永香, 等. 柴达木盆地东缘山地祁连圆柏林上限树木径向生长与气候要素的关系. 应用生态学报, 2009, 20(3): 507-512 [Zheng Y-H, Zhu H-F, Zhang Y-X, et al. Relationships between Sabina przewalskii radial growth and climatic factors at upper timberlines in Eastern Mountainous region of Qaidam Basin. Chinese Journal of Applied Ecology, 2009, 20(3): 507-512]
[41] 付霞, 张家武, 王林, 等. 近期人类活动对湖泊沉积记录的影响——以托素湖为例. 第四纪研究, 2016, 36(6): 1456-1465 [Fu X, Zhang J-W, Wang L, et al. Recent human impacts on sedimentary record: A case from Lake Toson. Quaternary Sciences, 2016, 36(6): 1456-1465]

利用树轮揭示人类活动对柴达木盆地巴音河径流量的影响

Impacts of human activity on Bayin River runoff as revealed by tree rings in Qaidam Basin, China

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