A Review on the Impact of Global Warming to Greenhouse Gas Flux in Frozen Ground Region

doi:10.11733/j.issn.1007-0435.2023.04.001

Acta Agrestia Sinica ›› 2023, Vol. 31 ›› Issue (4): 929-942.DOI: 10.11733/j.issn.1007-0435.2023.04.001

A Review on the Impact of Global Warming to Greenhouse Gas Flux in Frozen Ground Region

CHEN Zhe^1,5, JIN Yan-xia¹, SUN Jian³, SHAO Xin-qing⁴, WANG Ying-dian^1,5, ZHAO Xin-quan², WANG Wen-ying^1,5, XIE Hui-chun¹, ZHANG Zhen-hua², ZHANG Li¹, DU Yan-gong², ZHOU Hua-kun²

1. Qinghai Normal University/Academy of Plateau Science and Sustainability, Xining, Qinghai Province 810016, China;
2. Northwest Institute of Plateau Biology, Chinese Academy of Sciences/Qinghai Provincial Key Laboratory of Restoration Ecology for Cold Regions, Xining, Qinghai Province 810008, China;
3. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China;
4. China Agricultural University, Beijing 100083, China;
5. Qinghai Provincial Key Laboratory of Biodiversity Formation Mechanism and Comprehensive Utilization in Qinghai-Tibetan Plateau, Xining, Qinghai Province 810016, China

Received:2022-06-17 Revised:2022-12-04 Published:2023-04-28

全球变暖对高寒冻土区温室气体通量影响研究进展

陈哲^1,5, 金艳霞¹, 孙建³, 邵新庆⁴, 王英典^1,5, 赵新全², 王文颖^1,5, 谢惠春¹, 张振华², 张莉¹, 杜岩功², 周华坤²

1. 青海师范大学/高原科学与可持续发展研究院, 青海西宁 810016;
2. 中国科学院西北高原生物研究所, 青海西宁 810008;
3. 中国科学院青藏高原研究所, 北京 100085;
4. 中国农业大学, 北京 100083;
5. 青海省青藏高原生物多样性形成机制与综合利用重点实验室, 青海西宁 810016

通讯作者: 杜岩功,E-mail:ygdu@nwipb.cas.cn;周华坤,E-mail:hkzhou@nwipb.cas.cn
作者简介:陈哲(1986-),男,汉族,陕西眉县人,博士,副教授,主要从事高寒草地生态系统生态学研究,E-mail:chenzhe@qhnu.edu.cn
基金资助:
青海省自然科学基金(2018-ZJ-935Q)；青藏高原第二次综合科学考察(2019QZKK0302-02)；国家自然基金(32260288)；海南州科技支撑计划项目(2022-KZ01-A)资助

Abstract

Abstract: The Holarctic and Qinghai-Tibet Plateau are important organic carbon and nitrogen pool in terrestrial ecosystems. Global warming is changing the pattern of soil freeze-thaw in frozen ground in high latitude and/or high altitude regions. Such as accelerating permafrost degradation,promoting the organic matter decomposition in active layer of frozen soil,and causing a large amount of greenhouse gas emission. These positive feedbacks of climate change have been a main focus of global change ecology and biogeochemical cycle research. In this paper,we reviewed the characteristics and induced mechanisms of soil CO₂,CH₄ and N₂O fluxes under freeze-thaw ground in the Holarctic and Qinghai-Tibet Plateau. We also discussed the relationship between the effects of net greenhouse emissions and global warming in the cold ecosystems. Furthermore,some key processes about the soil carbon emission and nitrogen conversion in frozen region to be focused on in the ongoing research were proposed with an intention to provide some references for the researches on the carbon and nitrogen cycle in frozen ground under the background of climate warming.

Key words: Climate warming, Holarctic, Qinghai-Tibet Plateau, Freeze-thaw effect, Effects of net greenhouse emission

摘要： 泛北极地区和青藏高原是陆地生态系统重要的有机碳、氮库。在气候变暖驱动下，高纬度或高海拔冻土融化加速，冻土活动层冻融格局改变，土壤有机质分解增加，成为全球重要的温室气体排放源，其对气候变化的“正反馈”效应受到越来越多关注。本文重点综述了近年泛北极和青藏高原冻土区土壤CO₂，CH₄和N₂O三种主要温室气体通量对冻土退化及冻融作用的响应特征和影响机制，探讨了高寒地区生态系统净温室效应与气候变暖的相互关系，并简要提出了目前冻土区土壤碳排放和氮转化关键过程研究中需要加强的方面，旨在为继续深入开展气候变化背景下冻土碳氮循环研究提供参考。

关键词: 气候变暖, 泛北极, 青藏高原, 冻融作用, 净温室效应

CLC Number:

Q148

CHEN Zhe, JIN Yan-xia, SUN Jian, SHAO Xin-qing, WANG Ying-dian, ZHAO Xin-quan, WANG Wen-ying, XIE Hui-chun, ZHANG Zhen-hua, ZHANG Li, DU Yan-gong, ZHOU Hua-kun. A Review on the Impact of Global Warming to Greenhouse Gas Flux in Frozen Ground Region[J]. Acta Agrestia Sinica, 2023, 31(4): 929-942.

陈哲, 金艳霞, 孙建, 邵新庆, 王英典, 赵新全, 王文颖, 谢惠春, 张振华, 张莉, 杜岩功, 周华坤. 全球变暖对高寒冻土区温室气体通量影响研究进展[J]. 草地学报, 2023, 31(4): 929-942.

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References

[1] 赵林,盛煜.青藏高原多年冻土及变化[M]. 北京:科学出版社,2019:1-9
[2] OBU J,WESTERMANN S,BARTSCH A,et al. Northern Hemisphere Permafrost Map Based on TTOP Modelling for 2000-2016 at 1 km² Scale[J]. Earth-Science Reviews,2019,193:299-316
[3] ZOU D F,ZHAO L,SHENG Y,et al. A new map of permafrost distribution on the Tibetan Plateau[J]. The Cryosphere,2017,11(6):2527-2542
[4] SCHUUR E,MCGUIRE A D,SCHADEL C,et al. Climate change and the permafrost carbon feedback[J]. Nature,2015,520(7546):171-179
[5] DING J Z,LI F,YANG G B,et al. The Permafrost Carbon Inventory on the Tibetan Plateau:a New Evaluation Using Deep Sediment Cores[J]. Global Change Biology,2016,22(8):2688-2701
[6] 王蓝翔,董慧科,龚平,等. 多年冻土退化下碳、氮和污染物循环研究进展[J]. 冰川冻土,2021,43(5):1365-1382
[7] BROWN J,FERRIANS O,HEGINBOTTOM J A,et al. Circum-Arctic Map of Permafrost and Ground-Ice Conditions,Version 2[EB/OL]. https://nsidc.org/data/ggd318/versions/2,2022-06-17
[8] KATEY,WALTER,ANTHONY,et al. 21 st-century modeled permafrost carbon emissions accelerated by abrupt thaw beneath lakes[J]. Nature Communications,2018,9(1):3262
[9] WANG T,YANG D,YANG Y,et al. Permafrost thawing puts the frozen carbon at risk over the Tibetan Plateau[J]. Science Advances,2020,6(19):eaaz3513
[10] FRIEDLINGSTEIN P COX P,BETTS R,et al. Climate-Carbon Cycle Feedback Analysis:Results from the C4MIP Model Intercomparison[J]. Journal of Climate,2006,19(14):3337-3353
[11] QIAN H,JOSEPH R,ZENG N. Enhanced terrestrial carbon uptake in the Northern High Latitudes in the 21st century from the Coupled Carbon Cycle Climate Model Intercomparison Project model projections[J]. Global Change Biology,2010,16(2):641-656
[12] SCHAEFER K,ZHANG T,BRUHWILER L,et al. Amount and timing of permafrost carbon release in response to climate warming[J]. Tellus,2011,63(2):165-180
[13] KOVEN C D,LAWRENCE D M,RILEY W J. Permafrost carbon climate feedback is sensitive to deep soil carbon decomposability but not deep soil nitrogen dynamics[J]. Proceedings of the National Academy of Sciences of the United States of America,2015,112(12):3752-3757
[14] MCGUIRE A D,LAWRENCE D M,KOVEN C,et al. Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change[J]. Proceedings of the National Academy of Sciences of the United States of America,20181,15(15):3882-3887
[15] SCHUUR E,ABBOTT B W,BOWDEN W B,et al. Expert assessment of vulnerability of permafrost carbon to climate change[J]. Climatic Change,2013,119(2):359-374
[16] SCHUUR E,ABBOTT B. High risk of permafrost thaw:Northern soils will release huge amounts of carbon in a warmer world [J]. Nature,2011,480(7375):32-33
[17] HARDEN J W,KOVEN C D,PING C L,et al. Field information links permafrost carbon to physical vulnerabilities of thawing[J]. Geophysical Research Letters,2012,39(15):L15704
[18] GROGAN P,MICHELSEN A,AMBUSP,et al. Freeze-thaw regime effects on carbon and nitrogen dynamics in sub-arctic heath tundra mesocosms[J].Soil Biology and Biochemistry,2004,36(4):641-654
[19] 孙辉,秦纪洪,吴杨. 土壤冻融交替生态效应研究进展[J]. 土壤,2008,40(4):505-509
[20] CHAI Y J,ZENG X B,E S Z,et al. Effects of freeze-thaw on aggregate stability and the organic carbon and nitrogen enrichment ratios in aggregate fractions[J]. Soil Use Management,2014,30:507-516
[21] KREYLING J,PERSOH D,WERNER S,et al. Short-term impacts of soil freeze-thaw cycles on roots and root-associated fungi of holcus lanatus and calluna vulgaris[J]. Plant Soil,2012,353:19-31
[22] PEREZ-MON C,FROSSARD A,FREY B. Functional and structural responses of arctic and alpine soil prokaryotic and fungal communities under freeze-thaw cycles of different frequencies[J]. Frontiers in Microbiology,2020,11:982
[23] WU M H,CHEN S Y,CHEN J W,et al. Reduced microbial stability in the active layer is associated with carbon loss under alpine permafrost degradation[J]. Proceedings of the National Academy of Sciences of the United States of America,2021,118(25):e2025321118
[24] 陈哲,杨世琦,张晴雯,等. 冻融作用对土壤氮素损失及有效性的影响[J]. 生态学报,2016,36(4):1083-1094
[25] 胡仲豪,常顺利,张毓涛,等. 天山林区不同类型群落土壤氮素对冻融过程的动态响应[J]. 生态学报,2019,39(2):571-579
[26] PU J H,JIANG N,JUAN Y H,et al. Effects of freeze-thaw on dissolved nitrogen pool,nitrogen transformation processes and diversity of bacterial community in temperate soils[J]. The journal of applied ecology,2020,31(9):2893-2902
[27] JIANG N,JUANY,TIAN L,et al. Soil water contents control the responses of dissolved nitrogen pools and bacterial communities to freeze-thaw in temperate soils[J]. BioMed Research International,2020:6867081
[28] MAO C,KOU D,CHEN L Y,et al. Permafrost nitrogen status and its determinants on the Tibetan Plateau[J]. Global Change Biology,2020，26(9):5290-5302
[29] CHEN L,LIU L,QIN S,et al. Regulation of priming effect by soil organic matter stability over a broad geographic scale[J]. Nature Communications,2019,10:5112
[30] RISK N,SNIDER D,WAGNER-RIDDLE C. Mechanisms leading to enhanced soil nitrous oxide fluxes induced by freeze-thaw cycles[J]. Canadian Journal of Soil Science,2013,93:401-414
[31] BISKABORN B K,SMITH S L,NOETZLI J,et al. Permafrost is warming at a global scale[J]. Nature Communications,2019,10(1):264
[32] SMITH S L,O'NEILL H B,ISAKSEN K,et al. The changing thermal state of permafrost[J]. Nature Reviews Earth & Environment,2022,3(1):10-23
[33] STRANEO F,SUTHERLANG D A,HOLLAND D,et al. Characteristics of ocean waters reaching Greenland’s glaciers[J]. Annals of Glaciology,2012,53(60):202-210
[34] MUDRYK L R,KUSHNER P J,DERKSEN C,et al. Snow cover response to temperature in observational and climate model ensembles[J]. Geophysical Research Letters,2017,44(2):919-926
[35] BISKABORN B K,LANCKMAN J P,LANTUIT H,et al. The new database of the Global Terrestrial Network for Permafrost (GTN-P)[J]. Earth System Science Data,2015,7(2):245-259
[36] 蔡红艳,韩冬锐,杨林生,等. 泛北极地区多年冻土活动层厚度演变[J]. 遥感学报,2020,24(8):1045-1057
[37] AALTO J,KARJALAINEN O,HJORT J et al. Statistical forecasting of current and future circum-Arctic ground temperatures and active layer thickness[J]. Geophysical Research Letters,2018,45(10):4889-4898
[38] KUANG X X,JIU J J. Review on climate change on the Tibetan Plateau during the last half century[J]. Journal of Geophysical Research Atmospheres,2016,121(8):3979-4007
[39] 秦大河. 气候变化科学与人类可持续发展[J]. 地理科学进展,2014,33(7):874-883
[40] GUO D,WANG H. Simulated change in the near-surface soil freeze/thaw cycle on the Tibetan Plateau from 1981 to 2010[J]. Chinese Science Bulletin,2014,59(20):2439-2448
[41] DING J Z,CHEN L Y,JI C J,et al. Decadal soil carbon accumulation across Tibetan permafrost regions[J]. Nature Geoscience,2017,10:420-424
[42] 林笠,王其兵,张振华,等. 温暖化加剧青藏高原高寒草甸土非生长季冻融循环[J]. 北京大学学报:自然科学版,2017,53(1):171-178
[43] LIU F T,KOU D,CHEN Y L,et al. Altered microbial structure and function after thermokarst formation[J]. Global Change Biology,2021,27:823-835
[44] PENG X,ZHANG T,FRAUENFELD O,et al. Spatiotemporal Changes in Active Layer Thickness under Contemporary and Projected Climate in the Northern Hemisphere[J]. Journal of climate,2018,31(7):251-266
[45] WAN G N,YANG M X,LIU Z C,et al. The precipitation variations in the Qinghai-Xizang (Tibetan) Plateau during 1961-2015[J]. Atmosphere,2017,8:80
[46] LI W B,Wu J B,BAI E,et al. Response of terrestrial nitrogen dynamics to snow cover change:A meta-analysis of experimental manipulation[J]. Soil Biology & Biochemistry,2016,100:51-58
[47] 冉洪伍,范继辉,黄菁. 藏北高寒草地土壤冻融过程水热变化特征[J]. 草业科学,2019,36(4):980-990
[48] 马俊杰,李韧,刘宏超,等. 青藏高原多年冻土区活动层水热特性研究进展[J]. 冰川冻土,2020,42(1):195-204
[49] LIBBY M D,VANDERZAAG A C,GREGORICH E G,et al. An improved laboratory method shows that freezing intensity increases N₂O emissions[J]. Canadian Journal of Soil Science,2020,100(2):136-149
[50] HUGELIUS G,BOCKHEIM J G,CAMILL P,et al. A new data set for estimating organic carbon storage to 3 m depth in soils of the northern circumpolar permafrost region[J]. Earth System Science Data,2013,5(2),393-402
[51] HUGELIUS G,STRAUSS J,ZUBRZYCKI S,et al. Estimated stocks of circumpolar permafrost carbon with quantified uncertainty ranges and identified data gaps[J]. Biogeosciences,2014,11(23):6573-6593
[52] 王根绪,程国栋,沈永平. 青藏高原草地土壤有机碳库及其全球意义[J]. 冰川冻土,2002(6):693-700
[53] LOISEL J,YU Z,BEILMAN D W,et al. A Database and synthesis of northern peatland soil properties and holocene carbon and nitrogen accumulation[J]. The Holocene,2014,24(9):1028-1042
[54] KOU D,DING J,LI F,et al. Spatially-explicit estimate of soil nitrogen stock and its implication for land model across Tibetan alpine permafrost region[J]. Science of the Total Environment,2019,650:1795-1804
[55] 张亚亚,郭颖,刘海红,等. 青藏高原表土有机碳、全氮含量分布及其影响因素[J]. 生态环境学报,2018,27(5):866-872
[56] WANG Y,SONG C,YU L,et al. Convergence in temperature sensitivity of soil respiration:Evidence from the Tibetan alpine grasslands[J]. Soil Biology and Biochemistry,2018,122:50-59
[57] DAVIDSON E A,JANSSENS I A. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change[J]. Nature,2006,440(7081):165-173
[58] WANG Y,LIU H,CHUNG H,et al. Non-growing-season soil respiration is controlled by freezing and thawing processes in the summer monsoon-dominated Tibetan alpine grassland[J]. Global Biogeochemical Cycles, 2014,28(10):9-20
[59] SCHÄDEL C,BADER K F,SCHUUR E,et al. Potential carbon emissions dominated by carbon dioxide from thawed permafrost soils[J]. Nature Climate Change,2016,6(10):950-953
[60] LI J Q,YAN D,PENDALL E,et al. Depth dependence of soil carbon temperature sensitivity across Tibetan permafrost regions[J]. Soil Biology and Biochemistry,2018,126:82-90
[61] SCHÄDEL C,SCHUUR E,BRACHO R,et al. Circumpolar assessment of permafrost C quality and its vulnerability over time using long-term incubation data[J]. Global Change Biology,2014,20(2):641-652
[62] CHEN L,LIANG J,QIN S,et al. Determinants of carbon release from the active layer and permafrost deposits on the Tibetan Plateau[J]. Nature Communications,2016,7:13046
[63] CHEN Y,HAN M,YUAN X,et al. Warming has a minor effect on surface soil organic carbon in alpine meadow ecosystems on the Qinghai-Tibetan Plateau[J]. Global Change Biology,2022,28(10):1618-1629
[64] SCHUUR E,VOGEL J G,CRUMMER K G,et al. The effect of permafrost thaw on old carbon release and net carbon exchange from tundra[J]. Nature,2009,459(7246):556-559
[65] STEVEN B,POLLARD W H,GREER C W,et al. Microbial diversity and activity through a permafrost/ground ice core profile from the Canadian high Arctic[J]. Environmental Microbiology,2010,10(12):3388-3403
[66] HENRY H A L. Climate change and soil freezing dynamics:historical trends and projected changes[J]. Climatic Change,2008,87:421-434
[67] NATALI S M,WATTS J D,ROGERS B M,et al. Large loss of CO₂ in winter observed across the northern permafrost region[J]. Nature Climate Change,2019,9(12):852-857
[68] 王广帅,杨晓霞,任飞,等. 青藏高原高寒草甸非生长季温室气体排放特征及其年度贡献[J]. 生态学杂志,2013,32(8):1994-2001
[69] STIEGLITZ M,DÉRY S J,ROMANOVSKY V E,et al. The role of snow cover in the warming of arctic permafrost[J]. Geophysical Research Letters,2003,30(13):54-51
[70] GROFFMAN P M,DRISCOLL C T,FAHEY T J,et al. Colder soils in a warmer world:A snow manipulation study in a northern hardwood forest ecosystem[J]. Biogeochemistry,2001,56(2):135-150
[71] WANG Q,LV W,LI B,et al. Annual ecosystem respiration is resistant to changes in freeze-thaw periods in semi-arid permafrost[J]. Global Change Biology,2020,26(4):2630-2641
[72] OLEFELDT D,GOSWAMI S,GROSSE G,et al. Circumpolar distribution and carbon storage of thermokarst landscapes[J]. Nature Communications,2016,7,13043
[73] DAI L C,GUO X W,ZHANG F W,et al. Seasonal dynamics and controls of deep soil water infiltration in the seasonally-frozen region of the Qinghai-Tibet plateau[J]. Journal of Hydrology,2019,571:740-748
[74] 张贤,朱求安,杨斌,等. 基于过程模型的青藏高原湿地甲烷排放格局评估[J]. 生态学报,2020,40(9):3060-3071
[75] IPCC:MASSON-DELMOTTE V,ZHAI P,PIRANI A,et al. Climate Change:The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change[R]. Cambridge:Cambridge University Press,2021:1
[76] TREAT C C,NATALI S M,ERNAKOVICH J,et al. A pan-Arctic synthesis of CH₄and CO₂ production from anoxic soil incubations[J]. Global Change Biology,2015,21(7):2787-2803
[77] OLEFELDT D,TURETSKY M R,CRILL P M,et al. Environmental and physical controls on northern terrestrial methane emissions across permafrost zones[J]. Global Change Biology,2013,19(2):589-603
[78] PAUDEL R,MAHOWALD N M,HESS P G M,et al. Attribution of changes in global wetland methane emissions from pre-industrial to present using CLM4.5-BGC[J]. Environmental Research Letters,2016,11(3):034020
[79] KAPLAN,JED O. Wetlands at the Last Glacial Maximum:Distribution and methane emissions[J]. Geophysical Research Letters,2002,29(6):1079
[80] LI F,Yang G B,Peng Y F,et al. Warming Effects on Methane Fluxes Differ Between Two Alpine Grasslands with Contrasting Soil Water Status[J]. Agricultural and forest meteorology,2020,290:107988
[81] ZHANG Z H,WANG G S,WANG H,et al. Warming and drought increase but wetness reduces the net sink of CH₄ in alpine meadow on the Tibetan Plateau[J]. Applied Soil Ecology,2021,167:104061
[82] SONG W,WANG H,WANG G,et al. Methane emissions from an alpine wetland on the Tibetan Plateau:Neglected but vital contribution of the nongrowing season[J]. Journal of Geophysical Research Biogeosciences,2015,120(8):1475-1490
[83] SONG C,WANG Y,WANG Y,et al. Emission of CO₂,CH₄ and N₂O from freshwater marsh during freeze-thaw period in Northeast of China[J]. Atmospheric Environment,2006,40(35):6879-6885
[84] 陈哲,韩瑞芸,杨世琦,等. 东北季节性冻融农田土壤CO₂、CH₄、N₂O通量特征研究[J]. 农业环境科学学报,2016,35(2):387-395
[85] JEAN L M,PIERRE R. Production,oxidation,emission and consumption of methane by soils:A Review[J]. European journal of soil biology,2001,37(1):25-50
[86] DÖRSCH P,PALOJARVI A,MOMMERTZ S. Overwinter greenhouse gas fluxes in two contrasting agricultural habitats[J]. Nutrient Cycling in Agroecosystems,2004,70(2):117-133
[87] LI F,PENG Y,NATALI S M,et al. Warming effects on permafrost ecosystem carbon fluxes associated with plant nutrients[J]. Ecology,2017,98(11):2851-2859
[88] ZHANG X Z,YANG Y P,PIAO S L,et al. Ecological change on the Tibetan Plateau[J]. Chinese Science Bulletin,2015,60,(32):3048-3056
[89] WEI D,QI Y,MA Y,et al. Plant uptake of CO₂ outpaces losses from permafrost and plant respiration on the Tibetan Plateau[J]. Proceedings of the National Academy of Sciences of the United States of America,2021,118(33):2015283118
[90] LIU H Y,MI Z R,LIN L,et al. Shifting plant species composition in response to climate change stabilizes grassland primary production[J]. Proceedings of the National Academy of Science of the United States of America,2018,115(16):4051-4056
[91] PEDERSEN E P,ELBERLING B,MICHELSEN A. Foraging deeply:Depth-specific plant nitrogen uptake in response to climate-induced N-release and permafrost thaw in the High Arctic[J]. Global Change Biology,2020,26(11):6523-6536
[92] PU Y,WANG D,LI M,et al. Effects of alpine marsh degradation on soil phytoliths and phytolith-occluded carbon on the Zoige Plateau,China[J]. Journal of Soils and Sediments,2021,21:1730-1742
[93] GAO W,SUN W,XU X. Permafrost response to temperature rise in carbon and nutrient cycling:Effects from habitat-specific conditions and factors of warming[J]. Ecology and Evolution,2021,11(22):16021-16033
[94] GAO W,YAN D. Warming suppresses microbial biomass but enhances N recycling[J]. Soil Biology and Biochemistry,2019,131:111-118
[95] CRAINE J M,ELMORE A J,WANG L,et al. Isotopic evidence for oligotrophication of terrestrial ecosystems[J]. Nature Ecology & Evolution,2018,2(11):1735-1744
[96] WANG J,WU Q,YUAN Z,et al. Soil respiration of alpine meadow is controlled by freeze-thaw processes of active layer in the permafrost region of the Qinghai-Tibet Plateau[J]. The Cryosphere,2020,14(9):2835-2848
[97] VOIGT C,MARUSHCHAK M E,ABBOT B W,et al. Nitrous oxide emissions from permafrost-affected soils[J]. Nature Reviews Earth & Environment,2020,1:420-434
[98] MARUSHCHAK M E,KERTTULA J,DIÁKOVÁ，et al. Thawing Yedoma permafrost is a neglected nitrous oxide source[J]. Nature Communications,2021,12(1):7107
[99] ZHANG L W,ZHANG S,XIA X H,et al. Unexpectedly Minor Nitrous Oxide Emissions from Fluvial Networks Draining Permafrost Catchments of the East Qinghai-Tibet Plateau[J]. Nature Communications,2022,13(1):950-950
[100] WU H H,XU X K,CHENG W G,et al. Dissolved organic matter and inorganic N jointly regulate greenhouse gases fluxes from forest soils with different moistures during a freeze-thaw period[J]. Soil Science and Plant Nutrition,2020,66:163-176
[101] WOLF B,KIESE R,CHEN W,et al. Modeling N₂O emissions from steppe in Inner Mongolia,China,with consideration of spring thaw and grazing intensity[J]. Plant & Soil,2012,350(1-2):297-310
[102] CHEN Z,YANG S Q,ZHANG A P,et al. Nitrous oxide emissions following seasonal freeze-thaw events from arable soils in northeast China[J]. Journal of Integrative Agriculture,2018,17(1):231-246
[103] 周旺明,秦胜金,刘景双,等. 沼泽湿地土壤氮矿化对温度变化及冻融的响应[J]. 农业环境科学学报,2011,30(4):806-811
[104] TEEPE R,BERNARD L. Variability of CO₂ and N₂O Emissions During Freeze-Thaw Cycles:Results of Model Experiments on Undisturbed Forest-Soil Cores[J]. Journal of plant nutrition and soil science,2004,167(2):153-159
[105] SORENSEN P O,FINZI AC,MARC-ANDRE G,et al. Winter soil freeze-thaw cycles lead to reductions in soil microbial biomass and activity not compensated for by soil warming[J]. Soil Biology and Biochemistry,2018,116:39-47
[106] CHEN Z,GE S D,ZHANG Z H,et al. Soil moisture but not warming dominates nitrous oxide emissions during freeze-thaw cycles in a Qinghai-Tibetan Plateau alpine meadow with discontinuous permafrost[J]. Frontiers in Ecology and Evolution,2021,9:676027
[107] 徐欢,王芳芳,李婷,等. 冻融交替对土壤氮素循环关键过程的影响与机制研究进展[J]. 生态学报,2020,40(10):3168-3182
[108] MAO C,KOU D,WANG G,et al. Trajectory of topsoil nitrogen transformations along a thermo erosion gully on the Tibetan Plateau[J]. Journal of Geophysical Research Biogeosciences,2019,124(5):1342-1354
[109] BRUIJN A M G D,BUTTERBACH-BAHL K,BLAGODATSKY S,et al. Model evaluation of different mechanisms driving freeze-thaw N₂O emissions[J]. Agriculture Ecosystems & Environment,2009,133(3-4):196-207
[110] LUDWIG B,W0LF I,TEEPE R. Contribution of nitrification and denitrification to the emission of N₂O in a freeze-thaw event in an agricultural soil[J]. Journal of Plant Nutrition and Soil Science,2004,167(6):678-684
[111] ÖQUIST M G,NILSSON M,S RENSSON F,et al. Nitrous oxide production in a forest soil at low temperatures-processes and environmental controls[J].FEMS Microbiology Ecology,2004,49(3):371-378
[112] YANAI Y,TOYOTA K,OKAZAKI M. Response of denitrifying communities to successive soil freeze-thaw cycles[J]. Biology and Fertility of Soils,2007,44(1):113-119
[113] CHERKAUER K A,BOWLING L C,NAZ B. Treatise on Geomorphology[M]. New York:Academic Press,2013:151-172
[114] 蔡延江,丁维新,项剑. 农田土壤N₂O和NO排放的影响因素及其作用机制[J]. 土壤,2012,44(6):881-887
[115] YANG G,PENG Y,MARUSHCHAK M E,et al. Magnitude and pathways of increased nitrous oxide emissions from uplands following permafrost thaw[J]. Environmental Science & Technology,2018,52(16):9162-9169
[116] SANDERS-DEMOTT R,SORENSEN P O,REINMANN A B,et al. Growing season warming and winter freeze-thaw cycles reduce root nitrogen uptake capacity and increase soil solution nitrogen in a northern forest ecosystem[J]. Biogeochemistry,2018,137(3):337-349
[117] KOU D,YANG G,LI F,et al. Progressive nitrogen limitation across the Tibetan alpine permafrost region[J]. Nature Communications,2020,11:3331
[118] KLEIN J A,HARTE J,ZHAO X Q,et al. Decline in medicinal and forage species with warming is mediated by plant traits on the Tibetan Plateau[J]. Ecosystems,2007,11(5):775-789
[119] LV W,LUO C,ZHANG L,et al. Net neutral carbon responses to warming and grazing in alpine grassland ecosystems[J]. Agricultural and Forest Meteorology,2020,280:107792
[120] 陈哲,徐巍,门双,等. 祁连山岛状冻土活动层土壤氮库对模拟冻融响应[J]. 草地学报,2023,31(1):19-28
[121] 方精云. 碳中和的生态学透视[J]. 植物生态学报,2021,45(11):1173-1176
[122] 王云英,裴薇薇,郭小伟,等. 青藏高原高寒湿地生态系统碳水通量与水分利用效率研究[J].草地学报,2022,30(5):1037-1042
[123] 刘长雨,谢保鹏,杨洁,等. 青藏高原不同退化梯度下植被蒸散发的时空格局研究[J]. 草地学报,2023,31(1):252-262

A Review on the Impact of Global Warming to Greenhouse Gas Flux in Frozen Ground Region

全球变暖对高寒冻土区温室气体通量影响研究进展

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