Interannual Variation of Summer Rainfall at the Tianchi Station in the Changbai Mountains and its Associated Circulation Anomalies
-
摘要: 长白山地处吉林省东南部，作为国家级重点生态功能区，其降水变化特征对该地森林生态系统和水资源结构变化有重要影响。本文基于1979～2016年吉林省47个台站逐月降水资料，探究了长白山天池站夏季降水的气候特征及其相关的环流异常，并与吉林省降水进行对比。分析结果表明天池夏季降水量以及年际变率高出吉林省其它站点一倍左右。此外，天池降水年际变化对应的环流异常与吉林省降水一致，即6月东北亚气旋式异常和东亚高空急流的增强，以及7、8月西太平洋副热带高压增强和东亚高空西风急流偏北，均可引起吉林省和天池降水偏多。另一方面，天池降水变异还表现出其独特的环流异常，与吉林省降水对应的环流异常显著不同或者甚至近乎相反，究其原因为长白山地形所致。本文的结果说明山地的气候和大气环流的关系复杂、多变。Abstract: The Changbai Mountains are located in the southeastern part of Jilin Province. Rainfall has a crucial effect on the forest ecosystem and water resource in the Changbai Mountains, which is a national key ecological function area. Based on the monthly precipitation data from 47 stations in Jilin Province and the ERA-Interim monthly reanalysis data from 1979 to 2016, we investigated the climate characteristics of summer precipitation at the Tianchi station in the Changbai Mountains and circulation anomalies associated with the interannual variation of rainfall at this station and compared the Tianchi station with the other stations in Jilin Province. Results show that summer precipitation at the Tianchi station and its interannual variation are approximately two times larger than that at other stations in Jilin Province. On one hand, the circulation anomalies associated with the interannual variation of precipitation at the Tianchi station are consistent with those for the entire Jilin Province. The circulation anomalies that favor more rainfall at the Tianchi station and the entire Jilin Province are characterized by a cyclonic anomaly over Northeast Asia and an enhanced East Asian jet stream in June and an enhanced western Pacific subtropical high and a northward-displaced East Asian jet stream in July and August. On the other hand, precipitation at the Tianchi station is associated with unique circulation anomalies, which are quite different or nearly opposite to precipitation in the entire Jilin Province, and can be attributed to the terrain of the Changbai Mountains. The results indicate that climate variability in the mountains can be related to the complicated and varying patterns of large-scale atmospheric circulation anomalies.
-
Key words:
- Tianchi in Changbai Mountains /
- Precipitation /
- Interannual variation /
- Circulation /
- Summer
-
图 1 吉林省地形（单位：m）及47个站点分布图。红色三角形代表天池站
Figure 1. Topography (units: m) and spatial distribution of 47 stations in Jilin Province. The red triangle denotes the Tianchi station
图 2 1979～2016年吉林省47个站降水量的（a–c）平均值及（d–f）年际标准差：（a，d）6月；（b，e）7月；（c，f）8月。黑色虚线为除天池站外吉林省46站平均值，红色柱代表天池站
Figure 2. (a–c) Average and (d–f) interannual standard deviations of precipitation of 47 stations in Jilin Province for the period 1979–2016: (a, d) June; (b, e) July; (c, f) August. The black dotted line denotes the average value of 46 stations in Jilin Province, except for Tianchi station. The red bar denotes the Tianchi station
图 3 与吉林省有关的降水量（红色）及天池特有的降水量（蓝色）标准化时间序列：（a）6月；（b）7月；（c）8月
Figure 3. Standardized time series of precipitation at the Tianchi station consistent (red) and inconsistent (blue) with that in the entire Jilin Province: (a) June; (b) July; (c) August
图 4 1979～2016年8月（a）TC_JL、（b）TC_R回归得到的吉林省降水异常（单位：mm）。蓝色（红色）代表降水量正（负）异常。实心圆代表天池站
Figure 4. Regression of precipitation anomalies in Jilin Province onto the (a) TC_JL index and (b) TC_R index in August from 1979 to 2016 (units: mm). Blue (red) denotes the positive (negative) anomaly. The solid circle denotes the Tianchi station
图 5 TC_JL回归得到的500 hPa位势高度异常（单位：m）：（a）6月；（b）7月；（c）8月。黑色实线代表达到90%信度水平
Figure 5. Regression of the 500 hPa geopotential height anomalies onto the TC_JL index (units: m): (a) June; (b) July; (c) August. Black solid lines denote the anomalies above the 90% confidence level
图 6 TC_JL回归得到的700 hPa水平风异常（单位：m s−1）：（a）6月；（b）7月；（c）8月。阴影区域代表纬向风或经向风异常达到90%信度水平，图仅显示大于0.2 m s−1的风
Figure 6. Regression of the 700 hPa horizontal wind anomalies onto the TC_JL index (units: m s−1): (a) June; (b) July; (c) August. The shaded areas denote either zonal or meridional wind anomalies above the 90% confidence level. Only vectors greater than 0.2 m s−1 are presented
图 7 指数TC_JL回归得到的200 hPa纬向风异常（单位：m s−1）：（a）6月；（b）7月；（c）8月。黑色实线代表达到90%信度水平
Figure 7. Regression of the 200 hPa zonal wind anomalies onto the TC_JL index (units: m s−1): (a) June; (b) July; (c) August. Black solid lines denote the anomalies above the 90% confidence level
图 8 指数TC_JL回归得到的200 hPa经向风异常（单位：m s−1）：（a）6月；（b）7月；（c）8月。黑色实线代表达到90%信度水平；网格区域为指数1的定义范围；粗实线为气候平均的西风急流轴
Figure 8. Regression of the 200 hPa meridional wind anomalies onto the TC_JL index (units: m s−1): (a) June; (b) July; (c) August. Black solid lines denote the anomalies above the 90% confidence level. The grid areas represent the defining areas for Index 1. The thick solid line denotes the axis of the climatological mean westerly jet
图 9 指数TC_R回归得到的700 hPa水平风异常（单位：m s−1）：（a）6月；（b）7月；（c）8月。阴影区域代表纬向风或经向风异常达到90%信度水平；图仅显示大于0.2 m s−1的风
Figure 9. Regression of the 700 hPa horizontal wind anomalies onto the TC_JL index (units: m s−1): (a) June; (b) July; (c) August. The shaded areas represent either zonal or meridional wind anomalies above the 90% confidence level. Only vectors greater than 0.2 m s−1 are presented
图 10 指数TC_R回归得到的200 hPa水平风异常（单位：m s−1）：（a）7月；（b）8月。阴影区域代表纬向风或经向风异常达到90%信度水平；图仅显示大于0.2 m s−1的风
Figure 10. Regression of the 200 hPa horizontal wind anomalies onto the TC_R index (units: m s−1): (a) July; (b) August. The shaded areas represent either zonal or meridional wind anomalies above the 90% confidence level. Only vectors greater than 0.2 m s−1 are presented
图 11 指数TC_R回归得到的200 hPa经向风异常（单位：m s−1）：（a）7月；（b）8月。黑色实线代表达到90%信度水平；网格区域为指数2的定义范围；粗实线为气候平均的西风急流轴
Figure 11. Regression of the 200 hPa meridional wind anomalies onto the TC_R index (units: m s−1): (a) July; (b) August. Black solid lines denote the anomalies above the 90% confidence level. The grid areas represent the defining areas for Index 2. The thick solid line denotes the axis of the climatological mean westerly jet
图 12 1979～2016年8月（a）指数1、（b）指数2回归得到的吉林省降水异常（单位：mm）。蓝色（红色）代表降水量正（负）异常；实心圆代表天池站
Figure 12. Regression of precipitation anomalies in Jilin Province onto (a) Index 1 and (b) Index 2 in August from 1979 to 2016 (units: mm). Blue (red) denotes the positive (negative) anomaly. The solid circle denotes the Tianchi station
图 13 1979～2016年8月（a）指数1、（b）指数2回归得到的700 hPa水平风异常（单位：m s−1）。阴影区域代表达到90%信度水平；图仅显示大于0.2 m s−1的风
Figure 13. Regression of the 700 hPa horizontal wind anomalies onto (a) Index 1 and (b) Index 2 in August from 1979 to 2016 (units: m s−1). The shaded areas represent either zonal or meridional wind anomalies above the 90% confidence level. Only vectors greater than 0.2 m s−1 are presented
图 14 1979～2016年8月指数2回归得到的（a）500 hPa、（b）850 hPa垂直速度异常（单位：hPa s−1）。黑色实线代表达到90%信度水平
Figure 14. Regression of the 500 hPa (a) and 850 hPa (b) vertical velocity anomalies onto Index 2 in August from 1979 to 2016 (units: hPa s−1). Black solid lines denote the anomalies above the 90% confidence level
-
[1] Amante C, Eakins B W. 2009. ETOPO1 1 Arc-Minute Global Relief Model: Procedures, data sources and analysis [R]. NOAA Tech. Memorandum NESDIS NGDC-24. [2] Berrisford P, Dee D, Fielding K, et al. 2009. The ERA-Interim archive [R]. ECMWF, ERA Rep. Series 1. [3] Chen W, Lu R Y. 2014. The interannual variation in monthly temperature over Northeast China during summer [J]. Adv. Atmos. Sci., 31(3): 515−524. doi: 10.1007/s00376-013-3102-3 [4] 陈海山, 陈健康. 2017. 东亚夏季风指数的分类及物理特征分析 [J]. 大气科学学报, 40(3): 299−309. doi: 10.13878/j.cnki.dqkxxb.20160323001Chen Haishan, Chen Jiankang. 2017. Classification of East Asian summer monsoon indicesand their basic physical features [J]. Trans. Atmos. Sci. (in Chinese), 40(3): 299−309. doi: 10.13878/j.cnki.dqkxxb.20160323001 [5] 陈列, 高露双, 张赟, 等. 2013. 长白山北坡不同林型内红松年表特征及其与气候因子的关系 [J]. 生态学报, 33(4): 1285−1291. doi: 10.5846/stxb201209181309Chen Lie, Gao Lushaung, Zhang Yun, et al. 2013. Characteristics of tree-ring chronology of Pinus koraiensis and its relationship with climate factors on the northern slope of Changbai Mountain [J]. Acta Ecologica Sinica (in Chinese), 33(4): 1285−1291. doi: 10.5846/stxb201209181309 [6] 陈力, 尹云鹤, 赵东升, 等. 2014. 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, 34(6): 1568−1574. doi: 10.5846/stxb201210121415Chen Li, Yin Yunhe, Zhao Dongsheng, et al. 2014. Climate response of tree growth along an altitudinal gradient in the Changbai Mountains, Northeast China [J]. Acta Ecologica Sinica (in Chinese), 34(6): 1568−1574. doi: 10.5846/stxb201210121415 [7] Chen W, Hong X W, Lu R Y, et al. 2016. Variation in summer surface air temperature over northeast Asia and its associated circulation anomalies [J]. Adv. Atmos. Sci., 33(1): 1−9. doi: 10.1007/s00376-015-5056-0 [8] Cheng Hongjun. 2012. Climate characteristics in the summer of 2012 in Jilin Province and its circulation characteristics [J]. Jilin Meteorology (in Chinese)(3): 34−37. [9] 崔玉琴. 1995. 东北地区上空水汽平衡状况及其源地 [J]. 地理科学, 15(1): 80−87.Cui Yuqin. 1995. Budget condition of water vapoue over Northeast China and its source [J]. Scientia Geographica Sinica (in Chinese), 15(1): 80−87. [10] Ding Q H, Wang B. 2005. Circumglobal teleconnection in the Northern Hemisphere summer [J]. J. Climate, 18(17): 3483−3505. doi: 10.1175/JCLI3473.1 [11] 董伟, 刘海峰, 朱玉祥. 2012. 吉林省夏季极端降水事件特征分析 [J]. 自然灾害学报, 21(4): 69−75. doi: 10.13577/j.jnd.2012.0411Dong Wei, Liu Haifeng, Zhu Yuxiang. 2012. Characteristic analysis of summer extreme precipitation events in Jilin Province [J]. Journal of Natural Disasters (in Chinese), 21(4): 69−75. doi: 10.13577/j.jnd.2012.0411 [12] 董伟, 刘玉芬, 朱丹, 等. 2013. 吉林省夏季降水时空变化特征研究 [J]. 气象科学, 33(2): 229−235. doi: 10.3969/2012jms.0078Dong Wei, Liu Yufen, Zhu Dan, et al. 2013. Analysis of spatial and temporal variation characteristics of summer precipitation in Jilin Province [J]. Journal of the Meteorological Sciences (in Chinese), 33(2): 229−235. doi: 10.3969/2012jms.0078 [13] Du M X, Lin Z D, Lu R Y. 2017. Combined impact of in-phase and out-of-phase variation between the northern East Asian low and western North Pacific subtropical high on East Asian summer rainfall [J]. Atmos. Oceanic Sci. Lett., 10(4): 284−290. doi: 10.1080/16742834.2017.1312262 [14] Fang Y H, Chen H S, Teng F D, et al. 2017. Changing contribution rate of heavy rainfall to the rainy season precipitation in Northeast China and its possible causes [J]. Atmos. Res., 197: 437−445. doi: 10.1016/j.atmosres.2017.07.030 [15] 韩艳刚, 周旺明, 齐麟, 等. 2019. 长白山树木径向生长对气候因子的响应 [J]. 应用生态学报, 30(5): 1513−1520. doi: 10.13287/j.1001-9332.201905.039Han Yangang, Zhou Wangming, Qi Lin, et al. 2019. Tree radial growth-climate relationship in Changbai Mountain, Northeast China [J]. Chinese Journal of Applied Ecology (in Chinese), 30(5): 1513−1520. doi: 10.13287/j.1001-9332.201905.039 [16] Hong X W, Lu R Y, Li S L. 2018. Differences in the Silk Road Pattern and its relationship to the North Atlantic Oscillation between early and late summers [J]. J. Climate, 31(22): 9283−9292. doi: 10.1175/JCLI-D-18-0283.1 [17] 胡开喜, 陆日宇, 王东海. 2011. 东北冷涡及其气候影响 [J]. 大气科学, 35(1): 179−191. doi: 10.3878/j.issn.1006-9895.2011.01.15Hu Kaixi, Lu Riyu, Wang Donghai. 2011. Cold vortex over Northeast China and its climate effect [J]. Chinese Journal of Atmospheric Sciences (in Chinese), 35(1): 179−191. doi: 10.3878/j.issn.1006-9895.2011.01.15 [18] Huang G, Liu Y, Huang R H. 2011. The interannual variability of summer rainfall in the arid and semiarid regions of northern China and its association with the Northern Hemisphere circumglobal teleconnection [J]. Adv. Atmos. Sci., 28(2): 257−268. doi: 10.1007/s00376-010-9225-x [19] 贾小龙, 王谦谦. 2006. 东北地区汛期降水异常的大气环流特征分析 [J]. 高原气象, 25(2): 309−318. doi: 10.3321/j.issn:1000-0534.2006.02.018Jia Xiaolong, Wang Qianqian. 2006. Analyses on general circulation character of precipitation anomaly in Northeast China flood season [J]. Plateau Meteorology (in Chinese), 25(2): 309−318. doi: 10.3321/j.issn:1000-0534.2006.02.018 [20] Krishnan R, Sugi M. 2001. Baiu rainfall variability and associated monsoon teleconnections [J]. J. Meteor. Soc. Japan, 79(3): 851−860. doi: 10.2151/jmsj.79.851 [21] 兰明才, 张耀存. 2011. 东亚副热带急流与东北夏季降水异常的关系 [J]. 气象科学, 31(3): 258−265. doi: 10.3969/j.issn.1009-0827.2011.03.003Lan Mingcai, Zhang Yaocun. 2011. Relationship between the East Asian subtropical westerly jet and summer rainfall anomaly in Northeast China [J]. Journal of the Meteorological Sciences (in Chinese), 31(3): 258−265. doi: 10.3969/j.issn.1009-0827.2011.03.003 [22] Li C F, Chen W, Hong X W, et al. 2017. Why was the strengthening of rainfall in summer over the Yangtze River valley in 2016 less pronounced than that in 1998 under similar preceding El Niño events? — Role of midlatitude circulation in August [J]. Adv. Atmos. Sci., 34(11): 1290−1300. doi: 10.1007/s00376-017-7003-8 [23] Liang L Q, Li L J, Liu Q. 2011. Precipitation variability in Northeast China from 1961 to 2008 [J]. Journal of Hydrology, 404(1–2): 67−76. doi: 10.1016/j.jhydrol.2011.04.020 [24] Lin Z D, Wang B. 2016. Northern East Asian low and its impact on the interannual variation of East Asian summer rainfall [J]. Climate Dyn., 46(1–2): 83−97. doi: 10.1007/s00382-015-2570-9 [25] Lu R Y, Oh J H, Kim B J. 2002. A teleconnection pattern in upper-level meridional wind over the North African and Eurasian continent in summer [J]. Tellus A: Dynamic Meteorology and Oceanography, 54(1): 44−55. doi: 10.3402/tellusa.v54i1.12122 [26] Shen B Z, Lin Z D, Lu R Y, et al. 2011. Circulation anomalies associated with interannual variation of early- and late-summer precipitation in Northeast China [J]. Science China Earth Sciences, 54(7): 1095−1104. doi: 10.1007/s11430-011-4173-6 [27] 孙妍, 杨紫超, 云天, 等. 2015. 吉林省短时强降雨天气特征及大尺度环境条件 [J]. 气象灾害防御, 22(2): 9−12, 33. doi: 10.3969/j.issn.1006-5229.2015.02.003Sun Yan, Yang Zichao, Yun Tian, et al. 2015. Synoptic characteristics of short-time strong precipitation and large scale meteorological conditions in Jilin Province [J]. Meteorological Disaster Prevention (in Chinese), 22(2): 9−12, 33. doi: 10.3969/j.issn.1006-5229.2015.02.003 [28] 孙照渤, 曹蓉, 倪东鸿. 2016. 东北夏季降水分型及其大气环流特征 [J]. 大气科学学报, 39(1): 18−27. doi: 10.13878/j.cnki.dqkxxb.20140415001Sun Zhaobo, Cao Rong, Ni Donghong. 2016. A classification of summer precipitation patterns over Northeast China and their atmospheric circulation characteristics [J]. Trans. Atmos. Sci. (in Chinese), 39(1): 18−27. doi: 10.13878/j.cnki.dqkxxb.20140415001 [29] Sun L, Shen B Z, Sui B, et al. 2017. The influences of East Asian monsoon on summer precipitation in Northeast China [J]. Climate Dyn., 48(5): 1647−1659. doi: 10.1007/s00382-016-3165-9 [30] 王晓明, 赵秀海, 高露双, 等. 2013. 长白山北坡沿海拔梯度岳桦径向生长对气候的响应 [J]. 应用与环境生物学报, 19(6): 929−934. doi: 10.3724/SP.J.1145.2013.00929Wang Xiaoming, Zhao Xiuhai, Gao Lushuang, et al. 2013. Climatic response of Betula ermanii tree-ring growth along an altitudinal gradient on the northern slope of the Changbai Mountains [J]. Chinese Journal of Applied and Environmental Biology (in Chinese), 19(6): 929−934. doi: 10.3724/SP.J.1145.2013.00929 [31] 王学忠, 孙照渤, 谭言科, 等. 2006. 东北雨季的划分及其特征 [J]. 南京气象学院学报, 29(2): 203−208. doi: 10.3969/j.issn.1674-7097.2006.02.009Wang Xuezhong, Sun Zhaobo, Tan Yanke, et al. 2006. Demarcation and features of Northeast China rainy season [J]. Journal of Nanjing Institute of Meteorology (in Chinese), 29(2): 203−208. doi: 10.3969/j.issn.1674-7097.2006.02.009 [32] 王丽伟, 黄晓龙, 冯晓莉, 等. 2019. 2006~2015年吉林省夏季降水日变化特征 [J]. 中国农学通报, 35(3): 122−130. doi: 10.11924/j.issn.1000-6850.casb18070102Wang Liwei, Huang Xiaolong, Feng Xiaoli, et al. 2019. Diurnal precipitation variation of summer: Jilin 2006–2015 [J]. Chinese Agricultural Science Bulletin (in Chinese), 35(3): 122−130. doi: 10.11924/j.issn.1000-6850.casb18070102 [33] Xie Z W, Bueh C. 2015. Different types of cold vortex circulations over Northeast China and their weather impacts [J]. Mon. Wea. Rev., 143(3): 845−863. doi: 10.1175/MWR-D-14-00192.1 [34] Yasui S, Watanabe M. 2010. Forcing processes of the summertime circumglobal teleconnection pattern in a dry AGCM [J]. J. Climate, 23(8): 2093−2114. doi: 10.1175/2009JCLI3323.1 [35] 于秀晶, 王凤刚. 2005. 吉林省极端降水的变化特征及其与环流异常的关系 [J]. 吉林气象(4): 6−8, 19.Yu Xiujing, Wang Fenggang. 2005. Variation characteristics of extreme precipitation and its relation to circulation anomaly [J]. Jilin Meteorology (in Chinese)(4): 6−8, 19. [36] 曾丽红, 宋开山, 张柏, 等. 2010. 1960~2008年吉林省降水量的时空演变特征 [J]. 中国农业气象, 31(3): 344−352. doi: 10.3969/j.issn.1000-6362.2010.03.004Zeng Lihong, Song Kaishan, Zhang Bai, et al. 2010. Spatial–temporal precipitation variation over Jilin Province during 1960–2008 [J]. Chinese Journal of Agrometeorology (in Chinese), 31(3): 344−352. doi: 10.3969/j.issn.1000-6362.2010.03.004 [37] 张丽. 2002. 吉林省2002年夏季天气气候特点及影响 [J]. 吉林气象(4): 26−28.Zhang Li. 2002. Weather/Climate features and influence in the summer of 2002 in Jilin Province [J]. Jilin Meteorology (in Chinese)(4): 26−28. [38] 张丽, 石大明, 刘实. 2007. 吉林省2005年夏季降水特点及多雨成因 [J]. 吉林气象(1): 12−15.Zhang Li, Shi Daming, Liu Shi. 2007. Characteristics of precipitation and causes for heavier precipitation in summer of 2005 in Jilin Province [J]. Jilin Meteorology (in Chinese)(1): 12−15. [39] 张伟, 闫敏华, 陈泮勤, 等. 2007. 吉林省农作物生长季降水资源的时空分布特征 [J]. 中国农业气象, 28(4): 359−363. doi: 10.3969/j.issn.1000-6362.2007.04.002Zhang Wei, Yan Minhua, Chen Panqin, et al. 2007. Characteristics of temporal and spatial distribution of precipitation during crop growing season in Jilin Province [J]. Chinese Journal of Agrometeorology (in Chinese), 28(4): 359−363. doi: 10.3969/j.issn.1000-6362.2007.04.002 [40] 张伶俐, 成坤, 刘娜. 2016. 长白山不同海拔景点气象要素预报方法研究 [J]. 气象灾害防御, 23(4): 25−28. doi: 10.3969/j.issn.1006-5229.2016.04.007Zhang Lingli, Cheng Kun, Liu Na. 2016. Analysis of meteorological elements prediction method along an altitudinal gradient in the Changbai Mountains [J]. Meteorological Disaster Prevention (in Chinese), 23(4): 25−28. doi: 10.3969/j.issn.1006-5229.2016.04.007 [41] Zhao S X, Sun J H. 2007. Study on cut-off low-pressure systems with floods over Northeast Asia [J]. Meteor. Atmos. Phys., 96(1): 159−180. doi: 10.1007/s00703-006-0226-3 [42] 赵俊虎, 封国林, 杨杰, 等. 2012. 夏季西太平洋副热带高压的不同类型与中国汛期大尺度旱涝的分布 [J]. 气象学报, 70(5): 1021−1031. doi: 10.11676/qxxb2012.085Zhao Junhu, Feng Guolin, Yang Jie, et al. 2012. Analysis of the distribution of the large-scale drought/flood of summer in China under different types of the western Pacific subtropical high [J]. Acta Meteor. Sinica (in Chinese), 70(5): 1021−1031. doi: 10.11676/qxxb2012.085 [43] Zhao J H, Zhou J, Yang L, et al. 2018. Inter-annual and inter-decadal variability of early- and late-summer precipitation over Northeast China and their background circulation [J]. Int. J. Climatol., 38(6): 2880−2888. doi: 10.1002/joc.5470 [44] 周子建, 江源, 董满宇, 等. 2018. 长白山北坡不同海拔红松径向生长-气候因子关系对气温突变的响应 [J]. 生态学报, 38(13): 4668−4676. doi: 10.5846/stxb201706171104Zhou Zijian, Jiang Yuan, Dong Manyu, et al. 2018. Response of the relationship between radial growth and climatic factors to abrupt change of temperature along an altitudinal gradient on the northern slope of Changbai Mountain, Northeast China [J]. Acta Ecologica Sinica (in Chinese), 38(13): 4668−4676. doi: 10.5846/stxb201706171104 -
下载:
点击查看大图
计量
- 文章访问数: 45
- HTML全文浏览量: 8
- PDF下载量: 26
- 被引次数: 0
