Earth Science Frontiers ›› 2022, Vol. 29 ›› Issue (5): 355-371.DOI: 10.13745/j.esf.sf.2021.9.52
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TIAN Zhiping(), ZHANG Ran, JIANG Dabang
Received:
2021-06-02
Revised:
2021-07-02
Online:
2022-09-25
Published:
2022-08-24
CLC Number:
TIAN Zhiping, ZHANG Ran, JIANG Dabang. Mid-Holocene climate in China and the East Asian monsoon: Insights from PMIP4 simulations[J]. Earth Science Frontiers, 2022, 29(5): 355-371.
气候模式 | 所属国家 | 大气模式水平分辨率(经度×纬度) 和垂直分层 | 数值试验积分时间/ 模式年 | |
---|---|---|---|---|
1 | AWI-ESM-1-1-LR | 德国 | 1.875°×1.9°, L47 | 100 |
2 | CESM2 | 美国 | 1.25°×0.9°, L32 | 700 |
3 | EC-Earth3-LR | 欧盟 | 1.125°×1.1°, L62 | 203 |
4 | FGOALS-f3-L | 中国 | 1.25°×1°, L32 | 500 |
5 | FGOALS-g3 | 中国 | 2°×(2°~5°), L26 | 500 |
6 | GISS-E2-1-G | 法国 | 2.5°×2°, L40 | 100 |
7 | INM-CM4-8 | 俄罗斯 | 2°×1.5°, L21 | 200 |
8 | IPSL-CM6A-LR | 法国 | 2.5°×1.3°, L79 | 550 |
9 | MIROC-ES2L | 日本 | 2.8125°×2.8°, L40 | 100 |
10 | MPI-ESM1-2-LR | 德国 | 1.875°×2°, L47 | 500 |
11 | MRI-ESM2-0 | 日本 | 1.125°×1.1°, L80 | 200 |
12 | NESM3* | 中国 | 1.875°×1.9°, L47 | 100 |
13 | NorESM1-F | 挪威 | 2.5°×1.9°, L32 | 200 |
14 | NorESM2-LM | 挪威 | 2.5°×1.9°, L32 | 100 |
Table 1 Basic information of the 14 climate models within PMIP4 for the Mid-Holocene experiments in this study
气候模式 | 所属国家 | 大气模式水平分辨率(经度×纬度) 和垂直分层 | 数值试验积分时间/ 模式年 | |
---|---|---|---|---|
1 | AWI-ESM-1-1-LR | 德国 | 1.875°×1.9°, L47 | 100 |
2 | CESM2 | 美国 | 1.25°×0.9°, L32 | 700 |
3 | EC-Earth3-LR | 欧盟 | 1.125°×1.1°, L62 | 203 |
4 | FGOALS-f3-L | 中国 | 1.25°×1°, L32 | 500 |
5 | FGOALS-g3 | 中国 | 2°×(2°~5°), L26 | 500 |
6 | GISS-E2-1-G | 法国 | 2.5°×2°, L40 | 100 |
7 | INM-CM4-8 | 俄罗斯 | 2°×1.5°, L21 | 200 |
8 | IPSL-CM6A-LR | 法国 | 2.5°×1.3°, L79 | 550 |
9 | MIROC-ES2L | 日本 | 2.8125°×2.8°, L40 | 100 |
10 | MPI-ESM1-2-LR | 德国 | 1.875°×2°, L47 | 500 |
11 | MRI-ESM2-0 | 日本 | 1.125°×1.1°, L80 | 200 |
12 | NESM3* | 中国 | 1.875°×1.9°, L47 | 100 |
13 | NorESM1-F | 挪威 | 2.5°×1.9°, L32 | 200 |
14 | NorESM2-LM | 挪威 | 2.5°×1.9°, L32 | 100 |
边界条件 | PMIP3试验 | PMIP4试验 | |||||
---|---|---|---|---|---|---|---|
工业革命前期 | 全新世中期 | 工业革命前期 | 全新世中期 | ||||
地球轨道参数 | 偏心率 | 0.016724 | 0.018682 | 0.016764 | 0.018682 | ||
黄赤交角(°) | 23.446 | 24.105 | 23.459 | 24.105 | |||
岁差(°) | 102.04 | 0.87 | 100.33 | 0.87 | |||
大气温室气体 | 二氧化碳浓度/(μL·L-1) | 280 | 280 | 284.3 | 264.4 | ||
甲烷浓度/(nL·L-1) | 760 | 650 | 808.2 | 597 | |||
氧化亚氮浓度/(nL·L-1) | 270 | 270 | 273.0 | 262 | |||
太阳常数/(W·m-2) | 1365 | 同工业革命前期 | 1360.747 | 同工业革命前期 | |||
植被 | 固定或计算值 | 同工业革命前期 | 固定或计算值 | 同工业革命前期 | |||
气溶胶 | 固定或计算值 | 同工业革命前期 | 固定或计算值 | 同工业革命前期 |
Table 2 Boundary conditions for the experiment designs within the PMIP3 and PMIP4
边界条件 | PMIP3试验 | PMIP4试验 | |||||
---|---|---|---|---|---|---|---|
工业革命前期 | 全新世中期 | 工业革命前期 | 全新世中期 | ||||
地球轨道参数 | 偏心率 | 0.016724 | 0.018682 | 0.016764 | 0.018682 | ||
黄赤交角(°) | 23.446 | 24.105 | 23.459 | 24.105 | |||
岁差(°) | 102.04 | 0.87 | 100.33 | 0.87 | |||
大气温室气体 | 二氧化碳浓度/(μL·L-1) | 280 | 280 | 284.3 | 264.4 | ||
甲烷浓度/(nL·L-1) | 760 | 650 | 808.2 | 597 | |||
氧化亚氮浓度/(nL·L-1) | 270 | 270 | 273.0 | 262 | |||
太阳常数/(W·m-2) | 1365 | 同工业革命前期 | 1360.747 | 同工业革命前期 | |||
植被 | 固定或计算值 | 同工业革命前期 | 固定或计算值 | 同工业革命前期 | |||
气溶胶 | 固定或计算值 | 同工业革命前期 | 固定或计算值 | 同工业革命前期 |
Fig.1 Taylor diagram displaying the normalized pattern statistics of climatological variables between preindustrial simulations in PMIP4 models and observations
[1] | MASSON-DELMOTTE V, SCHULZ M, ABE-OUCHI A, et al. Information from Paleoclimate Archives[M]// STOCKER T F, QIND, PLATTNERG-K, et al. Climate change 2013:the physical science basis. Contribution of working group I to the fifth assessment report of the intergovernmental panel on climate change[M]. Cambridge: Cambridge University Press, 2013: 383-464. |
[2] |
BARTLEIN P J, HARRISON S P, BREWER S, et al. Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis[J]. Climate Dynamics, 2011, 37(3/4): 775-802.
DOI URL |
[3] | JOUSSAUME S, TAYLOR K. Status of the Paleoclimate Modeling Intercomparison Project (PMIP)[C]// GATES W L. Proceedings of the First International AMIP Scientific Conference. WCRP-92, WMO/TD-732, 1995: 425-430. |
[4] |
BRACONNOT P, OTTO-BLIESNER B, HARRISON S, et al. Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum-Part 1: experiments and large-scale features[J]. Climate of the Past, 2007, 3(2): 261-277.
DOI URL |
[5] |
TAYLOR K E, STOUFFER R J, MEEHL G A. An overview of CMIP5 and the experiment design[J]. Bulletin of the American Meteorological Society, 2012, 93(4): 485-498.
DOI URL |
[6] |
JOUSSAUME S, TAYLOR K E, BRACONNOT P, et al. Monsoon changes for 6000 years ago: results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)[J]. Geophysical Research Letters, 1999, 26(7): 859-862.
DOI URL |
[7] | 张肖剑, 靳立亚, 俞飞, 等. 基于PMIP2气候模式模拟的中全新世北大西洋涛动[J]. 海洋学报, 2010, 32(4): 41-50. |
[8] |
ZHOU B T, ZHAO P. Modeling variations of summer upper tropospheric temperature and associated climate over the Asian Pacific region during the Mid-Holocene[J]. Journal of Geophysical Research: Atmospheres, 2010, 115(D20): D20109.
DOI URL |
[9] | O'ISHI R, ABE-OUCHI A. Polar amplification in the Mid-Holocene derived from dynamical vegetation change with a GCM[J]. Geophysical Research Letters, 2011, 38(14): L14702. |
[10] |
ZHAO Y, HARRISON S P. Mid-Holocene monsoons: a multi-model analysis of the inter-hemispheric differences in the responses to orbital forcing and ocean feedbacks[J]. Climate Dynamics, 2012, 39(6): 1457-1487.
DOI URL |
[11] |
ZHOU B T, ZHAO P. Simulating changes of spring Asian-Pacific oscillation and associated atmospheric circulation in the Mid-Holocene[J]. International Journal of Climatology, 2013, 33(3): 529-538.
DOI URL |
[12] |
AN S I, CHOI J. Mid-Holocene tropical Pacific climate state, annual cycle, and ENSO in PMIP2 and PMIP3[J]. Climate Dynamics, 2014, 43(3/4): 957-970.
DOI URL |
[13] |
LIU Y Y, JIANG D B. Mid-Holocene permafrost: results from CMIP5 simulations[J]. Journal of Geophysical Research: Atmospheres, 2016, 121(1): 221-240.
DOI URL |
[14] |
BRIERLEY C, WAINER I. Inter-annual variability in the tropical Atlantic from the Last Glacial Maximum into future climate projections simulated by CMIP5/PMIP3[J]. Climate of the Past, 2018, 14(10): 1377-1390.
DOI URL |
[15] |
JIANG D B, SUI Y, LANG X M, et al. Last glacial maximum and Mid-Holocene thermal growing season simulations[J]. Journal of Geophysical Research: Atmospheres, 2018, 123(20): 11466-11478.
DOI URL |
[16] |
TIAN Z P, LI T, JIANG D B. Strengthening and westward shift of the tropical Pacific walker circulation during the Mid-Holocene: PMIP simulation results[J]. Journal of Climate, 2018, 31(6): 2283-2298.
DOI URL |
[17] | GĂINUŞĂ-BOGDAN A, SWINGEDOUW D, YIOU P, et al. AMOC and summer sea ice as key drivers of the spread in Mid-Holocene winter temperature patterns over Europe in PMIP3 models[J]. Global and Planetary Change, 2020, 184: 103055. |
[18] |
JIANG D B, LANG X M, TIAN Z P, et al. Considerable model-data mismatch in temperature over China during the Mid-Holocene: results of PMIP simulations[J]. Journal of Climate, 2012, 25(12): 4135-4153.
DOI URL |
[19] | TIAN Z P, JIANG D B. Revisiting Mid-Holocene temperature over China using PMIP3 simulations[J]. Atmospheric and Oceanic Science Letters, 2015, 8(6): 358-364. |
[20] |
JIANG D B, TIAN Z P, LANG X M. Mid-Holocene net precipitation changes over China: model-data comparison[J]. Quaternary Science Reviews, 2013, 82: 104-120.
DOI URL |
[21] | 周波涛, 赵平. 古东亚冬季风和夏季风反位相变化吗?[J]. 科学通报, 2009, 54(20): 3136-3143. |
[22] |
JIANG D B, LANG X M, TIAN Z P, et al. Mid-Holocene east Asian summer monsoon strengthening: insights from paleoclimate modeling intercomparison project (PMIP) simulations[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 369: 422-429.
DOI URL |
[23] |
TIAN Z P, JIANG D B. Strengthening of the East Asian winter monsoon during the Mid-Holocene[J]. The Holocene, 2018, 28(9): 1443-1451.
DOI URL |
[24] |
WANG N, JIANG D B, LANG X M. Mechanisms for spatially inhomogeneous changes in east Asian summer monsoon precipitation during the Mid-Holocene[J]. Journal of Climate, 2020, 33(8): 2945-2965.
DOI URL |
[25] | 陈星, 于革, 刘健. 东亚中全新世的气候模拟及其温度变化机制探讨[J]. 中国科学D辑: 地球科学, 2002, 32(4): 335-345. |
[26] | 王志远, 靳立亚, 俞飞, 等. 中东亚中全新世气候与植被反馈作用: PMIP2多模式结果分析[J]. 第四纪研究, 2011, 31(1): 36-47. |
[27] |
TIAN Z P, JIANG D B. Mid-Holocene ocean and vegetation feedbacks over East Asia[J]. Climate of the Past, 2013, 9(5): 2153-2171.
DOI URL |
[28] |
KAGEYAMA M, BRACONNOT P, HARRISON S P, et al. The PMIP4 contribution to CMIP6-Part 1: overview and over-arching analysis plan[J]. Geoscientific Model Development, 2018, 11(3): 1033-1057.
DOI URL |
[29] |
OTTO-BLIESNER B L, BRACONNOT P, HARRISON S P, et al. The PMIP4 contribution to CMIP6-Part 2: two interglacials, scientific objective and experimental design for Holocene and Last Interglacial simulations[J]. Geoscientific Model Development, 2017, 10(11): 3979-4003.
DOI URL |
[30] |
EYRING V, BONY S, MEEHL G A, et al. Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization[J]. Geoscientific Model Development, 2016, 9(5): 1937-1958.
DOI URL |
[31] | GROSE M R, NARSEY S, DELAGE F P, et al. Insights from CMIP6 for Australia's future climate[J]. Earth's Future, 2020, 8(5): e2019EF001469. |
[32] | TIAN B J, DONG X Y. The double-ITCZ bias in CMIP3, CMIP5 and CMIP6 models based on annual mean precipitation[J]. Geophysical Research Letters, 2020, 47(8): e2020GL087232. |
[33] |
JIANG D B, HU D, TIAN Z P, et al. Differences between CMIP6 and CMIP5 models in simulating climate over China and the East Asian monsoon[J]. Advances in Atmospheric Sciences, 2020, 37(10): 1102-1118.
DOI URL |
[34] |
BRIERLEY C M, ZHAO A N, HARRISON S P, et al. Large-scale features and evaluation of the PMIP4-CMIP6 midHolocene simulations[J]. Climate of the Past, 2020, 16(5): 1847-1872.
DOI URL |
[35] |
BROWN J R, BRIERLEY C M, AN S I, et al. Comparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models[J]. Climate of the Past, 2020, 16(5): 1777-1805.
DOI URL |
[36] | OTTO-BLIESNER B L, BRADY E C, TOMAS R A, et al. A comparison of the CMIP6 Mid-Holocene and lig127k simulations in CESM2[J]. Paleoceanography and Paleoclimatology, 2020, 35(11): e2020PA003957. |
[37] |
WILLIAMS C J R, GUARINO M V, CAPRON E, et al. CMIP6/PMIP4 simulations of the Mid-Holocene and Last Interglacial using HadGEM3: comparison to the pre-industrial era, previous model versions and proxy data[J]. Climate of the Past, 2020, 16(4): 1429-1450.
DOI URL |
[38] |
ZHANG Q, BERNTELL E, AXELSSON J, et al. Simulating the Mid-Holocene, last interglacial and Mid-Pliocene climate with EC-Earth3-LR[J]. Geoscientific Model Development, 2021, 14(2): 1147-1169.
DOI URL |
[39] |
BERGER A. Long-term variations of daily insolation and quaternary climatic changes[J]. Journal of the Atmospheric Sciences, 1978, 35(12): 2362-2367.
DOI URL |
[40] | 吴佳, 高学杰. 一套格点化的中国区域逐日观测资料及与其它资料的对比[J]. 地球物理学报, 2013, 56(4): 1102-1111. |
[41] |
KALNAY E, KANAMITSU M, KISTLER R, et al. The NCEP/NCAR 40-year reanalysis project[J]. Bulletin of the American Meteorological Society, 1996, 77(3): 437-471.
DOI URL |
[42] |
TAYLOR K E. Summarizing multiple aspects of model performance in a single diagram[J]. Journal of Geophysical Research: Atmospheres, 2001, 106(D7): 7183-7192.
DOI URL |
[43] |
LU H Y, WU N Q, LIU K B, et al. Modern pollen distributions in Qinghai-Tibetan Plateau and the development of transfer functions for reconstructing Holocene environmental changes[J]. Quaternary Science Reviews, 2011, 30(7/8): 947-966.
DOI URL |
[44] |
CAO X Y, HERZSCHUH U, TELFORD R J, et al. A modern pollen-climate dataset from China and Mongolia: assessing its potential for climate reconstruction[J]. Review of Palaeobotany and Palynology, 2014, 211: 87-96.
DOI URL |
[45] | 吴海斌, 李琴, 于严严, 等. 全新世中期中国气候格局定量重建[J]. 第四纪研究, 2017, 37(5): 982-998. |
[46] |
LI J Y, DODSON J, YAN H, et al. Quantitative Holocene climatic reconstructions for the Lower Yangtze region of China[J]. Climate Dynamics, 2018, 50(3/4): 1101-1113.
DOI URL |
[47] |
KAUFMAN D, MCKAY N, ROUTSON C, et al. A global database of Holocene paleotemperature records[J]. Scientific Data, 2020, 7(1): 115.
DOI URL |
[48] |
SHI Y F, KONG Z Z, WANG S M, et al. Mid-Holocene climates and environments in China[J]. Global and Planetary Change, 1993, 7(1/2/3): 219-233.
DOI URL |
[49] |
YU G, CHEN X, NI J, et al. Palaeovegetation of China: a pollen data-based synthesis for the Mid-Holocene and last glacial maximum[J]. Journal of Biogeography, 2000, 27(3): 635-664.
DOI URL |
[50] | 温锐林, 肖举乐, 常志刚, 等. 全新世呼伦湖区植被和气候变化的孢粉记录[J]. 第四纪研究, 2010, 30(6): 1105-1115. |
[51] |
JIANG W Y, GUIOT J, CHU G Q, et al. An improved methodology of the modern analogues technique for palaeoclimate reconstruction in arid and semi-arid regions[J]. Boreas, 2010, 39(1): 145-153.
DOI URL |
[52] |
NI J, YU G, HARRISON S P, et al. Palaeovegetation in China during the late Quaternary: biome reconstructions based on a global scheme of plant functional types[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 289(1/2/3/4): 44-61.
DOI URL |
[53] |
GUIOT J, WU H B, JIANG W Y, et al. East Asian Monsoon and paleoclimatic data analysis: a vegetation point of view[J]. Climate of the Past, 2008, 4(2): 137-145.
DOI URL |
[54] | 吴敬禄, 王苏民, 王洪道. 新疆艾比湖全新世以来的环境变迁与古气候[J]. 海洋与湖沼, 1996, 27(5): 524-530. |
[55] |
ROUTSON C C, MCKAY N P, KAUFMAN D S, et al. Mid-latitude net precipitation decreased with Arctic warming during the Holocene[J]. Nature, 2019, 568(7750): 83-87.
DOI URL |
[56] |
AN Z S. The history and variability of the East Asian paleomonsoon climate[J]. Quaternary Science Reviews, 2000, 19(1/2/3/4/5): 171-187.
DOI URL |
[57] | 肖尚斌, 李安春, 陈木宏, 等. 近8 ka东亚冬季风变化的东海内陆架泥质沉积记录[J]. 地球科学: 中国地质大学学报, 2005, 30(5): 573-581. |
[58] |
MORIMOTO M, KAYANNE H, ABE O, et al. Intensified Mid-Holocene Asian monsoon recorded in corals from Kikai Island, subtropical northwestern Pacific[J]. Quaternary Research, 2007, 67(2): 204-214.
DOI URL |
[59] |
WANG L, LI J J, LU H Y, et al. The East Asian winter monsoon over the last 15,000 years: its links to high-latitudes and tropical climate systems and complex correlation to the summer monsoon[J]. Quaternary Science Reviews, 2012, 32: 131-142.
DOI URL |
[60] |
LI Y, MORRILL C. A Holocene East Asian winter monsoon record at the southern edge of the Gobi Desert and its comparison with a transient simulation[J]. Climate Dynamics, 2015, 45(5/6): 1219-1234.
DOI URL |
[61] |
ZHAO S, XIA D S, JIN H L, et al. Long-term weakening of the East Asian summer and winter monsoons during the Mid- to Late Holocene recorded by aeolian deposits at the eastern edge of the Mu Us Desert[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 457: 258-268.
DOI URL |
[62] |
ZHANG E L, WANG Y B, SUN W W, et al. Holocene Asian monsoon evolution revealed by a pollen record from an alpine lake on the southeastern margin of the Qinghai-Tibetan Plateau, China[J]. Climate of the Past, 2016, 12(2): 415-427.
DOI URL |
[63] |
AI L N, HAN Z Z, WU X, et al. Geochemical and grain-sized implications for provenance variations of the central Yellow Sea muddy area since the middle Holocene[J]. Journal of Ocean University of China, 2020, 19(3): 577-588.
DOI URL |
[64] |
YANCHEVA G, NOWACZYK N R, MINGRAM J, et al. Influence of the intertropical convergence zone on the East Asian monsoon[J]. Nature, 2007, 445(7123): 74-77.
DOI URL |
[65] |
XIA D S, JIA J, LI G H, et al. Out-of-phase evolution between summer and winter East Asian monsoons during the Holocene as recorded by Chinese loess deposits[J]. Quaternary Research, 2014, 81(3): 500-507.
DOI URL |
[66] |
TU L Y, ZHOU X, CHENG W H, et al. Holocene East Asian winter monsoon changes reconstructed by sensitive grain size of sediments from Chinese coastal seas: a review[J]. Quaternary International, 2017, 440: 82-90.
DOI URL |
[67] | STEINKE S, MOHTADI M, GROENEVELD J, et al. Reconstructing the southern South China Sea upper water column structure since the Last Glacial Maximum: implications for the East Asian winter monsoon development[J]. Paleoceanography, 2010, 25(2): PA2219. |
[68] |
STEINKE S, GLATZ C, MOHTADI M, et al. Past dynamics of the East Asian monsoon: no inverse behaviour between the summer and winter monsoon during the Holocene[J]. Global and Planetary Change, 2011, 78(3/4): 170-177.
DOI URL |
[69] |
JIAN Z M, HUANG B Q, KUHNT W, et al. Late quaternary upwelling intensity and east Asian monsoon forcing in the South China Sea[J]. Quaternary Research, 2001, 55(3): 363-370.
DOI URL |
[70] |
WANG Y J, 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 URL |
[71] |
FENG Z D, TANG L Y, WANG H B, et al. Holocene vegetation variations and the associated environmental changes in the western part of the Chinese Loess Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 241(3/4): 440-456.
DOI URL |
[72] |
WANG Y J, CHENG H, EDWARDS R L, et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years[J]. Nature, 2008, 451(7182): 1090-1093.
DOI URL |
[73] |
SUN Q L, WANG S M, ZHOU J, et al. Lake surface fluctuations since the late glaciation at Lake Daihai, North central China: a direct indicator of hydrological process response to East Asian monsoon climate[J]. Quaternary International, 2009, 194(1/2): 45-54.
DOI URL |
[74] |
LI C H, WU Y H, HOU X H. Holocene vegetation and climate in Northeast China revealed from Jingbo Lake sediment[J]. Quaternary International, 2011, 229(1/2): 67-73.
DOI URL |
[75] |
ZHAI D Y, XIAO J L, ZHOU L, et al. Holocene East Asian monsoon variation inferred from species assemblage and shell chemistry of the ostracodes from Hulun Lake, Inner Mongolia[J]. Quaternary Research, 2011, 75(3): 512-522.
DOI URL |
[76] | WU X D, ZHANG Z H, XU X M, et al. Asian summer monsoonal variations during the Holocene revealed by Huguangyan maar lake sediment record[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 323/324/325: 13-21. |
[77] |
ZHANG Z Q, YAO Q, LIU K B, et al. Hydrological regime responses to Holocene East Asian summer monsoon circulation in marshes of the Sanjiang Plain, NE China[J]. Land Degradation and Development, 2020, 31(2): 240-250.
DOI URL |
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