基于EEMD的太阳活动对印度夏季风的多尺度胁迫分析

doi:10.13249/j.cnki.sgs.2018.04.017

地理科学 ›› 2018, Vol. 38 ›› Issue (4): 628-635.doi: 10.13249/j.cnki.sgs.2018.04.017

基于EEMD的太阳活动对印度夏季风的多尺度胁迫分析

李玉霞^1,^2,^3,⁴(), 陈玲玲⁵, 江亭桂^1,^2,^3,⁴, 罗文^1,^3,⁴, 林振山^1,^2,^3,⁴()

1.南京师范大学地理科学学院,江苏南京210023
2.江苏省环境演变与生态建设重点实验室（南京师范大学）,江苏南京 210023
3.江苏省地理环境演化国家重点实验室培育建设点,江苏南京 210023
4.江苏省地理信息资源开发与利用协同创新中心,江苏南京 210023
5.金陵科技学院人文学院,江苏南京 211169

收稿日期:2017-04-27 修回日期:2017-08-20 出版日期:2018-04-20 发布日期:2018-04-20
作者简介:
作者简介：李玉霞（1986-）,女,河北宣化人,博士后,主要从事自然地理专业研究。E-mail: liyuxia618@126.com
基金资助:
国家自然科学基金项目（41601417）,江苏省高校优势学科建设工程资助项目（164320H116）资助

Multi-scale Modulation Analysis of Solar Activity and Indian Summer Monsoon Based on EEMD Method

Yuxia Li^1,^2,^3,⁴(), Lingling Chen⁵, Tinggui Jiang^1,^2,^3,⁴, Wen Luo^1,^3,⁴, Zhenshan Lin^1,^2,^3,⁴()

1. School of Geography Science, Nanjing Normal University, Nanjing 210023, Jiangsu, China
2. Jiangsu Key Laboratory of Environmental Change and Ecological Construction, Nanjing 210023, Jiangsu, China
3. State Key Laboratory Cultivation Base of Geographical Environment Evolution (Jiangsu Province), Nanjing 210023, Jiangsu, China
4. Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, Jiangsu, China
5. Jinling Institute of Technology, Nanjing 211169, Jiangsu, China

Received:2017-04-27 Revised:2017-08-20 Online:2018-04-20 Published:2018-04-20
Supported by:
[National Natural Science Foundation of China (41601417), A Project Funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions(164320H116).]

摘要/Abstract

摘要：

选取10.55~2.7 kaBP Qunf洞的Q5石笋δ¹⁸O记录作为印度夏季风的代用指标,集合经验模态分解（EEMD）多尺度分析结果揭示了印度夏季风的强弱变化和与亚洲季风减弱事件的一致性,进一步讨论了11 kaBP以来印度夏季风的逐渐增强而后减弱的发展态势。选用同时期的古树年轮¹⁴C记录作为太阳活动代用指标,调频、调幅分析结果发现印度夏季风的31 a、70 a和7 860 a尺度分量受太阳活动相应分量的调频胁迫较为显著;同时又揭示出“太阳活动71 a周期-印度夏季风31 a周期”“太阳活动1 379 a周期-印度夏季风142 a周期”和“太阳活动2 376 a周期-印度夏季风733 a周期”三对调幅胁迫。

关键词: EEMD, 印度夏季风, 太阳活动, 调频胁迫, 调幅胁迫

Abstract:

Recent analysis of the multi-scale incidence relation between the Indian summer monsoon(ISM) and the solar activity is relatively poor, which makes the research on the driving mechanism of the ISM cannot go further. To solve this problem, the multi-scale fluctuation characteristics of the ISM was analyzed based on the Ensemble Empirical Mode Decomposition (EEMD) method. Furthermore, based on the amplitude modulation method, the frequency modulation and amplitude modulation forcing by solar activity on ISM is analyzed. Finally, the driving mechanism of ISM was discussed. We selected the δ¹⁸O record of Q5 stalagmite from Qunf cave which covers 10.55-2.7 kaBP period as proxy of ISM, the EEMD multi-scale analysis results reveals that the weakened event of ISM is correlated with the Asian monsoon, furthermore, the trend component shows that the development procedure of ISM increased first and then decreased gradually since 11 kaBP. The ¹⁴C records of ancient tree rings was selected as solar activity proxy, frequency modulation and amplitude modulation analysis results showed that the ISM components on the scale of 31 years, 70 years and 7 860 years were significantly forced by the frequency modulation of solar activity components on the corresponding scale. Meanwhile, it revealed that there were three pairs of amplitude modulations: the cycles between 71 years of solar activity and 31 years of ISM, the cycles between 1 379 years of solar activity and 142 years of ISM, and the cycles between 2 376 years of solar activity and 733 years of ISM.

Key words: EEMD, Indian summer monsoon, solar activity, frequency modulation, amplitude modulation

中图分类号:

P467

李玉霞, 陈玲玲, 江亭桂, 罗文, 林振山. 基于EEMD的太阳活动对印度夏季风的多尺度胁迫分析[J]. 地理科学, 2018, 38(4): 628-635.

Yuxia Li, Lingling Chen, Tinggui Jiang, Wen Luo, Zhenshan Lin. Multi-scale Modulation Analysis of Solar Activity and Indian Summer Monsoon Based on EEMD Method[J]. SCIENTIA GEOGRAPHICA SINICA, 2018, 38(4): 628-635.

图/表 10

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参考文献 26

[1]	Wang Y, Cheng H, Edwards R L et al. The Holocene Asian monsoon: links to solar changes and North Atlantic climate[J]. Science, 2005, 308(5723): 854-857. doi: 10.1126/science.1106296 pmid: 15879216
[2]	O'Brien S R, Mayewski P A, Meeker L D et al. Complexity of Holocene climate as reconstructed from a Greenland ice core[J]. Science, 1995, 270: 1962-1964. doi: 10.1126/science.270.5244.1962
[3]	Bond G, Showers W, Cheseby M et al. A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates[J]. Science, 1997, 278(5341): 1257-1266.
[4]	Zhou W, Lu X, Wu Z. Peat record reflecting Holocene climatic change in the Zoige Plateau and AMS radiocarbon dating[J]. Chinese Science Bulletin, 2002, 47(1): 66-70. doi: 10.1360/02tb9013
[5]	冯松, 张拥军, 朱德琴, 等. 近2000年古里雅冰芯净积累量与南疆盆地南沿的干湿变化[J]. 地理科学, 2005, 25(2): 221-225. doi: 10.3969/j.issn.1000-0690.2005.02.015
	[Feng Song, Zhang Yongjun, Zhu Deqin et al. Guliya ice core accumulation and dry and wet change in south part of south Xinjiang Basis in the past 2000 years. Scientia Geographica Sinica, 2005, 25(2):221-225.] doi: 10.3969/j.issn.1000-0690.2005.02.015
[6]	朱西德, 王振宇, 李林, 等. 树木年轮指示的柴达木东北缘近千年夏季气温变化[J]. 地理科学, 2007, 27(2): 256-260. doi: 10.3969/j.issn.1000-0690.2007.02.022
	[Zhu Xide, Wang Zhenyu, Li lin et al. Summer temperature in Northeast of Qaidam Basin retrieved from Tree-Ring Chronology. Scientia Geographica Sinica, 2007,27(2):256-260.] doi: 10.3969/j.issn.1000-0690.2007.02.022
[7]	郭其蕴. 东亚夏季风强度指数及其变化的分析[J].地理学报,1983,38(3):207-217.
	[Guo Qiyun. East Asian summer monsoon intensity index and its variation analysis. Acta Geographica Sinica, 1983, 38(3):207-217.]
[8]	王建明, 王建力, 李廷勇. 洞穴石笋δ18O与δ13C气候意义研究[J]. 热带地理, 2008, 28(5): 395-399.
	[Wang Jianming, Wang Jianli, Li Tingyong. The paleoclimatic significance of carbon and oxygen stable isotopes in Speleothems. Tropical Geography, 2008, 28(5): 395-399.]
[9]	Eddy J A. Climate and the changing sun[J]. Climatic Change, 1977, 1(2): 173-190. doi: 10.1007/BF01884410
[10]	Hodell D A, Brenner M, Curtis J H et al. Solar forcing of drought frequency in the Maya lowlands[J]. Science, 2001, 292(5520): 1367-1370. doi: 10.1126/science.1057759 pmid: 11359010
[11]	Neff U, Burns S J, Mangini A et al. Strong coherence between solar variability and the monsoon in Oman between 9 and 6 kyr ago[J]. Nature, 2001, 411: 290-293. doi: 10.1038/35077048 pmid: 11357127
[12]	Agnihotri R, Dutta K, Bhushan R et al. Evidence for solar forcing on the Indian monsoon during the last millennium[J]. Earth and Planetary Science Letters, 2002, 198(3): 521-527. doi: 10.1016/S0012-821X(02)00530-7
[13]	林振山, 汪曙光. 天文气候学10万年问题的研究[J]. 地球物理学报, 2004, 47(6): 971-975. doi: 10.3321/j.issn:0001-5733.2004.06.006
	[Lin Zhenshan, Wang Shuguang. A study on the problem of 100 ka cycles of astroclimatology. Chinese Journal of Geophysics,2004,47(6):971-975.] doi: 10.3321/j.issn:0001-5733.2004.06.006
[14]	Lin Z, Wang S. EMD analysis of solar insolation[J]. Meteorology and Atmospheric Physics, 2006, 93(1-2):123-128. doi: 10.1007/s00703-005-0138-7
[15]	Liu H, Lin Z, Qi X et al. Multiple analysis of variation of the East Asian Monsoon during the Holocene[J]. Quaternary International, 2010, 213(1-2): 74-78. doi: 10.1016/j.quaint.2009.02.017
[16]	罗虎明. 26万年以来东亚夏季风多尺度机制分析[D]. 南京: 南京师范大学. 2013, 1-94.
	[Luo Huming. Multi-scale mechanism analysis of the over 260,000 years east Asian summer monsoon. Nanjing: Nanjing Normal University, 2013, 1-94.]
[17]	Wu Z, Huang N E. Ensemble empirical mode decomposition: A noise-assisted data analysis method[J]. Advances in Adaptive Data Analysis, 2009, 1(1): 1-41.
[18]	Huang N E, Shen Z, Long S R. A new view of nonlinear water waves- The Hilbert spectrum[J]. Ann. Rev. Fluid. Mech., 1999, 31: 417-457. doi: 10.1146/annurev.fluid.31.1.417
[19]	Fleitmann D, Burns S J, Mudelsee M et al. Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman[J]. Science, 2003, 300(5626): 1737-1739. doi: 10.1126/science.1083130 pmid: 12805545
[20]	Suess H E. The radiocarbon record in tree rings of the last 8000 years[J]. Radiocarbon, 1980, 22(2): 200-209. doi: 10.1029/RS015i006p01195
[21]	Stuiver M, Braziunas T F. Sun, ocean, climate and atmospheric 14CO2: an evaluation of causal and spectral relationships[J]. The Holocene, 1993, 3(4): 289-305.
[22]	Stuiver M, Reimer P J, Bard E et al. Intcal98 radiocarbon age calibration, 24000-0 cal BP[J]. Radiocarbon, 1998, 40(3): 1041-1083. doi: 10.1029/97RS03183
[23]	Schulz M, Mudelsee M. REDFIT: estimating red-noise spectra directly from unevenly spaced paleoclimatic time series. Computers & Geosciences, 2002, 28(3):421-426. doi: 10.1016/S0098-3004(01)00044-9
[24]	Krishnamurthy V, Goswami B N. Indian monsoon-ENSO relationship on interdecadal timescale[J]. Journal of Climate, 2000, 13(3): 579-595.
[25]	Goswami B N, Madhusoodanan M S, Neema C P et al. A physical mechanism for North Atlantic SST influence on the Indian summer monsoon[J]. Geophysical Research Letters, 2006, 33(2): L02706. doi: 10.1029/2005GL024803
[26]	Solanki S K, Usoskin I G, Kromer B et al. Unusual activity of the Sun during recent decades compared to the previous 11,000 years[J]. Nature, 2004, 431(7012): 1084-1087. doi: 10.1038/nature02995 pmid: 15510145

	IMF1	IMF2	IMF3	IMF4	IMF5	IMF6	IMF7	IMF8	res
准周期（a）	31	70	142	279	733	1172	7280	7860	-
方差贡献率（%）	12.3	5.94	5.90	5.27	4.83	5.23	4.55	17.8	37.0
排序	3	4	5	6	8	7	9	2	1

分量	印度夏季风准周期（a）	太阳活动准周期（a）
IMF1	31	31
IMF2	70	71
IMF3	142	161
IMF4	279	341
IMF5	733	615
IMF6	1172	1397
IMF7	7280	2376
IMF8	7860	7860

分量	印度夏季风分量调频周期（a）	印度夏季风分量调幅周期（a）	太阳活动分量调频周期（a）
IM1	31	83	31
IM2	70	270	71
IM3	142	1299	161
IM4	279	1562	341
IM5	733	1960	615
IM6	1172	--	1397
IM7	7280	--	2376

基于EEMD的太阳活动对印度夏季风的多尺度胁迫分析

Multi-scale Modulation Analysis of Solar Activity and Indian Summer Monsoon Based on EEMD Method

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