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【目的】随着能源需求增长及对气候变化的关注,合理利用边际土地种植生物质能源作物成为近年研究的热点。以往研究表明边际土地种植多年生作物对区域气候变化和粮食生产影响显著,但均未全面考虑植物生长与气候变化的“相互”反馈,使结果可靠性略显不足。为克服早期研究的不足,【方法】基于耦合模型CWRF-BioCro综合考虑以上两者之间的“相互”反馈,分析在美国边际土地种植多年生生物质作物和维持现有植被覆盖两种情景下区域内降水格局的变化及其物理机制。【结果】结果表明,在边际土地种植多年生生物质作物后:区域合计平均日降水量增加6.33 mm/day(0.01%),以上增加主要发生在中西部春、夏、秋季和东部秋冬季,区域内水汽输送和潜热通量的显著增强是其主要原因;区域最大日降水量减少2.1 mm(4.39%),该减少主要集中于中东部,源于中东部感热通量的显著减少;同时中东部地区平均日降水量大于50 mm/d的降水事件频率降低,其中达50.0~99.9 mm/day的减少更胜、为31 d(0.24%)。【结论】综上,边际土地种植多年生生物质作物能增加区域降水量,同时减少极端降水。强调了生物物理反馈机制在调节区域气候中的关键作用,并为制定适应气候变化的土地管理策略提供了科学依据。
Abstract:[Objective]With increasing energy demand and growing concerns about climate change, the rational utilization of marginal lands for cultivating biomass energy crops has emerged as a research focus in recent years. Previous studies have demonstrated that cultivating perennial biomass crops on marginal lands significantly impacts regional climate change and food production. However, these investigations did not fully consider the interactive feedback between plant growth and climate change, leading to slightly insufficient reliability of the result. [ Methods] To address the limitations of earlier studies, the coupled model CWRF-Bio Cro was employed to comprehensively consider the interactive feedback between plant growth and climate change, and to analyze changes in regional precipitation patterns and their physical mechanisms under two scenarios in the United States: cultivation of perennial biomass crops on marginal lands and maintenance of existing vegetation cover. [Results]The result showed that after cultivating perennial biomass crops on marginal lands, the regional total average daily precipitation increased by 6. 33 mm/day(0. 01%), with most of the increase occurring during spring, summer, and autumn in the central and western regions and during autumn and winter in the eastern region. This was primarily due to the significant enhancement of water vapor transport and latent heat flux in the region. The regional maximum daily precipitation decreased by 2. 1 mm(4. 39%), mainly in the central and eastern regions, Resulting from a significant decrease in sensible heat flux in these regions. Meanwhile, the frequency of precipitation events with an average daily precipitation greater than 50 mm/d decreased in the central and eastern regions, with the most pronounced reduction of 31 days(0. 24%) observed in events in the range of 50. 0 ~ 99. 9 mm/day.[Conclusion] In summary, planting perennial biomass crops on marginal lands can increase regional precipitation and reduce extreme precipitation. These findings highlight the critical role of biophysical feedback mechanisms in regulating regional climate and provide a scientific foundation for developing climate-adaptive land management strategies.
[1] ZHAI P M,ZHOU B Q,CHEN Y,et al.Several new understandings in the climate change science[J].Climate Change Research,2021,17(6):629-635.
[2] FOUNDATION T G.Agrofuels and the myth of the Marginal Lands[J].Science.2008,319:1235-1238.
[3] SEARCHINGER T,HEIMLICH R,HOUGHTON R A,et al.Use of U.S.croplands for biofuels increases greenhouse gases through emissions from land-use change[J].Staff General Research Papers Archive,2008,319(5867):1238-1240.
[4] TILMAN D,HILL J,LEHMAN C,et al.Carbon-negative biofuels from low-input high-diversity grassland biomass[J].Science,2006,314(5805):1598-1600.
[5] FARGIONE J,HILL J,TILMAN D,et al.Land clearing and the biofuel carbon debt[J].Science,2008,319(5867):1235-1238.
[6] HANSEN E M,CHRISTENSEN B T,JENSEN L S,et al.Carbon sequestration in soil beneath long-term Miscanthus plantations as determined by 13C abundance[J].Biomass & Bioenergy,2004,26(2):97-105.
[7] SCHULTE L A,NIEMI J,HELMERS M J,et al.Prairie strips improve biodiversity and the delivery of multiple ecosystem services from corn-soybean croplands [J].Proceedings of the National Academy of Sciences,2017,114 (42):11247-11252.
[8] LOBELL D B,ASNER G P.Climate and management contributions to recent trends in U.S.agricultural yields[J].Science,2003,299(5609):1032-1032.
[9] PORTER,JOHN R.Rising temperatures are likely to reduce crop yields[J].Nature,2005,436(7048):174.
[10] BRANDES E,MCNUNN G S,SCHULTE L A,et al.Targeted subfield switchgrass integration could improve the farm economy,water quality,and bioenergy feedstock production[J].GCB Bioenergy,2018,10(3):199-212.
[11] BRANDES E,PLASTINA A,HEATON E A.Where can switchgrass production be more profitable than corn and soybean An integrated subfield assessment in Iowa,USA[J].GCB Bioenergy,2018,10(7):473-488.
[12] JAISWAL D,SOUZA A P D,LARSEN S,et al.Reply to:Brazilian ethanol expansion subject to limitations[J].Nature Climate Change,2019,9:211-212.
[13] FIELD J L,RICHARD T L,SMITHWICK E A H,et al.Robust paths to net greenhouse gas mitigation and negative emissions via advanced biofuels[J].Proceedings of the National Academy of Sciences,2020,117(36):21968-21977.
[14] CAI X,ZHANG X,WANG D.Land availability for biofuel production[J].Environmental Science & Technology,2011,45(1):334-339.
[15] JIANG D B,ZHANG Y,LANG X M.Vegetation feedback under future global warming[J].Theoretical and Applied Climatology,2011,106:211-227.
[16] JIN V L,SCHMER M R,STEWART C E,et al.Management controls the net greenhouse gas outcomes of growing bioenergy feedstocks on marginally productive croplands[J].Science Advances,2019,5(12):eaav9318.
[17] GEORGESCU M,LOBELL D B,FIELD C B,et al.Direct climate effects of perennial bioenergy crops in the United States[J].Proceedings of the National Academy of Sciences,2011,108(11):4307-4312.
[18] LOARIE S R,LOBELL D B,ASNER G P,et al.Direct impacts on local climate of sugar-cane expansion in Brazil[J].Nature Climate Change,2011,1(2):105-109.
[19] DEANGELIS A,DOMINGUEZ F,FAN Y,et al.Evidence of enhanced precipitation due to irrigation over the Great Plains of the United States[J].Journal of Geophysical Research Atmospheres,2010,115(D15):D15115.
[20] LEVIS S,BONAN G B,KLUZEK E,et al.Interactive crop management in the community earth system model (CESM1):Seasonal influences on land-atmosphere fluxes[J].Journal of Climate,2012,25(14):4839-4859.
[21] PIELKE R A SR,PITMAN A,NIYOGI D,et al.Land use/land cover changes and climate:modeling analysis and observational evidence[J].WIREs Climate Change,2011,2(6):828-850.
[22] ZHU J,LIANG X Z.Impacts of the bermuda high on regional climate and ozone over the United States[J].Journal of Climate,2013,26(3):1018-1032.
[23] JAISWAL D,DE SOUZA A,LARSEN S,et al.Brazilian sugarcane ethanol as an expandable green alternative to crude oil use[J].Nature Climate Change,2017,7:788-792.
[24] LARSEN S,JAISWAL D,BENTSEN NS,et al.Comparing predicted yield and yield stability of willow and Miscanthus across Denmark[J].GCB Bioenergy,2016,8(6):1061-1070.
[25] ]MIGUEZ F E,MAUGHAN M,BOLLERO G A,et al.Modeling spatial and dynamic variation in growth,yield,and yield stability of the bioenergy crops Miscanthus× giganteus and Panicum virgatum across the conterminous United States[J].GCB Bioenergy,2012,4(5):509-520.
[26] WANG D,JAISWAL D,LEBAUER D S,et al.A physiological and biophysical model of coppice willow (Salix spp.) production yields for the contiguous USA in current and future climate scenarios[J].Plant Cell & Environment,2015,38(9):1850-1865.
[27] MENGIS N,MATTHEWS H D.Non-CO2 forcing changes will likely decrease the remaining carbon budget for 1.5℃[J].NPJ Climate and Atmospheric Science,2020,3(1):1-7.
[28] OTTERMAN J.Baring high-albedo soils by overgrazing:A hypothesized desertification mechanism[J].Science,1974,186(4163):531-533.
[29] CHARNEY J,STONE P H,QUIRK W J.Drought in the sahara:A biogeophysical feedback mechanism[J].Science,1975,187(4175):434-435.
[30] SAGAN C,TOON O B,POLLACK J B.Anthropogenic albedo changes and the earth’s climate[J].Science,1979,206(4425):1363-1368.
[31] WOODWELL G M,HOBBIE J E,HOUGHTON R A,et al.Global deforestation:Contribution to atmospheric carbon dioxidee[J].Science,1983,222(4628):1081-1086.
[32] HOUGHTON R A,BOONE R D,MELILLO J M,et al.Net flux of carbon dioxide from tropical forests in 1980e[J].Nature,1985,316(6029):617-620.
[33] FORZIERI G,FEYEN L,RUSSO S,et al.Multi-hazard assessment in Europe under climate change[J].Climatic Change,2016,137(1-2):105-119.
[34] WANG N,QUESADA B,XIA L,et al.Effects of climate warming on carbon fluxes in grasslands:A global meta-analysis[J].Global Change Biology,2019,25(5):1839-1851.
[35] HE Y,JAISWAL D,LIANG X Z,et al.Perennial biomass crops on marginal land improve both regional climate and agricultural productivity[J].GCB Bioenergy,2022,14(5):558-571.
[36] MORICE C P,KENNEDY J J,RAYNER N A,et al.An updated assessment of near-surface temperature change from 1850:The hadcrut5 data set[J].Journal of Geophysical Research Atmospheres,2021,126(3):e2019JD032361.
[37] MYHRE G,ALTERSKJÆR K,STJERN C W,et al.Frequency of extreme precipitation increases extensively with event rareness under global warming[J].Scientific Reports,2019,9(1):16063.
[38] CHEN Y,MOUFOUMA-OKIA W,MASSON-DELMOTTE V,et al.Recent progress and emerging topics on weather and climate extremes since the fifth assessment report of the intergovernmental panel on climate change[J].Annual Review of Environment and Resources,2018,43(1):35-59.
[39] KJELLSTROM T,MCMICHAEL A J.Climate change threats to population health and well-being:the imperative of protective solutions that will last[J].Global Health Action.2013,6(1):20816.
[40] MARENGO J A,BERNASCONI M.Regional differences in aridity/drought conditions over Northeast Brazil:present state and future projections[J].Climatic Change,2015,129:103-115.
[41] DAI A.Increasing drought under global warming in observations and models[J].Nature climate change,2013,3(1):52-58.
[42] LIANG X Z,XU M,YUAN X,et al.Regional climate-weather research and forecasting model [J].Bulletin of the American Meteorological Society,2012,93(9):1363-1387.
[43] HERSBACH H,BELL B,BERRISFORD P,et al.The ERA5 global reanalysis[J].Quarterly journal of the royal meteorological society,2020,146(730):1999-2049.
[44] SUN C,LIANG X Z.Improving US extreme precipitation simulation:Dependence on cumulus parameterization and underlying mechanism[J].Climate Dynamics,2020,55(5):1325-1352.
[45] SUN C,LIANG X Z.Improving US extreme precipitation simulation:Sensitivity to physics parameterizations[J].Climate Dynamics,2020,54(11):4891-4918.
[46] HERRERA-ESTRADA J E,MARTINEZ J A,DOMÍNGUEZ F,et al.Reduced moisture transport linked to drought propagation across North America[J].Geophysical Research Letters,2019,46(10):5243-5253.
[47] GNANN S,BALDWIN J W,CUTHBERT M O,et al.The influence of topography on the global terrestrial water cycle[J].Reviews of Geophysics,2025,63(1):e2023RG000810.
[48] ROBERT A.HOUZE J.Orographic effects on precipitating clouds[J].Reviews of Geophysics,2012,50(1):e2011RG000365.
[49] HU Y H,JIA G S,GUO H D.Linking primary production,climate and land use along an urban-wildland transect:A satellite view[J].Environmental Research Letters,2009,4(4):044009.
[50] MISHRA M,DESUL S,SANTOS C A G,et al.A bibliometric analysis of sustainable development goals (SDGs):A review of progress,challenges,and opportunities[J].Environment,development and sustainability,2024,26(5):11101-11143.
基本信息:
DOI:10.13928/j.cnki.wrahe.2026.04.005
中图分类号:P426.6;TK6
引用信息:
[1]卢春燕,何雨峰,王遂缠,等.边际土地生物质作物:增加降水量并缓解极端降水事件(英文)[J].水利水电技术(中英文),2026,57(04):58-80.DOI:10.13928/j.cnki.wrahe.2026.04.005.
基金信息:
National Natural Science Foundation of China(32101324); Joint Funds of the Provincial Research Foundation of Gansu(25JRRA1117)~~
2025-08-04
2025-08-04
2025-08-04