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Coastal protection via sediment accretion in mangrove ecosystems 红树林生态系统中沉积物的增加对海岸的保护
Pub Date : 2026-01-15 DOI: 10.1038/s43017-026-00758-2
Alice J. Twomey, Hannah Hatcher
Nature Reviews Earth & Environment interviewed Alice Twomey about their project investigating how mangroves recover after tropical storms.
《自然评论:地球与环境》采访了Alice Twomey关于他们调查热带风暴后红树林如何恢复的项目。
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引用次数: 0
Drone docks for automated forest phenology monitoring 无人机码头用于自动森林物候监测
Pub Date : 2026-01-13 DOI: 10.1038/s43017-026-00759-1
Yanwei Cong
Yangwei Cong describes how drone docking stations can improve the coverage and efficacy of phenological monitoring in forests.
丛阳伟介绍了无人机对接站如何提高森林物候监测的覆盖率和效率。
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引用次数: 0
Changing the heatwave visual discourse in the news media 改变新闻媒体的热浪视觉话语
Pub Date : 2026-01-06 DOI: 10.1038/s43017-025-00754-y
Saffron O’Neill, Clare Davis
Nature Reviews Earth & Environment interviewed Professor Saffron O’Neill about their project investigating the visual communication of heatwaves in the news media.
《自然评论:地球与环境》采访了Saffron O’neill教授,内容涉及他们的研究热浪在新闻媒体中的视觉传播的项目。
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引用次数: 0
ENSO impacts on marine ecosystems and fisheries in the tropical and South Atlantic ENSO对热带和南大西洋海洋生态系统和渔业的影响
Pub Date : 2025-12-18 DOI: 10.1038/s43017-025-00742-2
Belén Rodríguez-Fonseca, Elena Calvo-Miguélez, Lucia Montoya-Carramolino, Regina R. Rodrigues, Irene Polo, Marta Martín-Rey, Teresa Losada, Jorge López-Parages, Iñigo Gómara, David Rivas, Filippa Fransner, Eleftheria Exarchou, Noel Keenlyside, Arnaud Bertrand, Lynne Shannon, Louise Gammage, Francisco Ramírez, Camila Artana, Jose Carlos Sánchez-Garrido, Emilia Sánchez-Gómez, Marie Pierre Moine, Raffaele Bernardello, Jeroen Steenbeek, Marta Coll, Verónica Martín-Gómez, Joke Lübbecke, Moacyr Araujo, Peter Brandt, Jörn O. Schmidt, Hans Sloterdijk, Ronaldo Angelini, Rodrigue Anicet Imbol Koungue, Khady Diouf, Shunya Koseki, Elaine McDonagh, Elsa Mohino, Jose Muelbert, Siny Ndoye, Hyacinth Nnamchi, Juliano Ramanantsoa, Mathieu Rouault, Ralf Schwamborn, Heino Fock, Marek Ostrowski, Amadou Thierno Gaye, Carlos R. Mechoso, Michael J. McPhaden, Wenju Cai
Tropical and South Atlantic marine ecosystems support fisheries that have vital environmental and socioeconomic importance. In this Review, we outline how the El Niño–Southern Oscillation — a Pacific mode of sea surface temperature variability — influences Atlantic fisheries via teleconnections and cascading linkages between physical, biogeochemical and ecological systems. Connections are driven by tropical pathways (involving changes in atmospheric stability associated with the Walker circulation and tropospheric warming) and extratropical pathways (involving the Pacific–South American and Pacific–North American teleconnection patterns). Depending on the location, these pathways modify rainfall and river discharge, winds and upwelling, or a combination of both, impacting salinity, nutrient availability, primary production and, thus, fish recruitment, biomass and catch. Fishery responses are strongly species dependent, reflecting variations in behaviour between species to environmental factors (such as temperature, oxygen, salinity, habitat and food availability). This regional variability and species dependency, coupled with strong non-stationarity, highlights the complexity of El Niño–Southern Oscillation impacts on Atlantic marine ecosystems. This historical signal is projected to weaken in the future. Enhanced observational systems and refined ecosystem models are urgently needed to enhance predictive capabilities, reduce societal impacts and improve sustainable management in these regions. The influence of the El Niño–Southern Oscillation on Atlantic marine systems and fisheries is complex. This Review outlines the mechanisms by which El Niño–Southern Oscillation impacts the tropical and South Atlantic, connecting physical climate perturbations to biogeochemical and ecological responses.
热带和南大西洋海洋生态系统支持具有重要环境和社会经济意义的渔业。在这篇综述中,我们概述了El Niño-Southern涛动-一种太平洋海面温度变化模式-如何通过物理、生物地球化学和生态系统之间的遥相关和级联联系影响大西洋渔业。连接由热带路径(涉及与Walker环流和对流层变暖相关的大气稳定性变化)和温带路径(涉及太平洋-南美和太平洋-北美遥相关模式)驱动。根据地点的不同,这些途径会改变降雨和河流流量、风和上升流,或两者兼而有之,从而影响盐度、养分供应、初级生产,从而影响鱼类补充、生物量和渔获量。渔业反应强烈依赖于物种,反映了物种之间的行为随环境因素(如温度、氧气、盐度、生境和食物供应)的变化。这种区域变异性和物种依赖性,加上强烈的非平稳性,突出了El Niño-Southern振荡对大西洋海洋生态系统影响的复杂性。这一历史信号预计将在未来减弱。这些地区迫切需要加强观测系统和改进生态系统模型,以增强预测能力、减少社会影响和改善可持续管理。El Niño-Southern涛动对大西洋海洋系统和渔业的影响是复杂的。本文概述了El Niño-Southern振荡影响热带和南大西洋的机制,将物理气候扰动与生物地球化学和生态响应联系起来。
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引用次数: 0
Beyond the Global Plastics Treaty 超越全球塑料条约
Pub Date : 2025-12-17 DOI: 10.1038/s43017-025-00752-0
Samuel Winton, Antaya March
Although the latest round of Global Plastics Treaty negotiations ended without agreement, the process has mobilized research, funding, and public engagement. Rather than waiting for an agreement, governments and communities should sustain momentum and build readiness for a future treaty through coordinated national planning, ambitious policies, and local initiatives.
尽管最新一轮的《全球塑料条约》谈判没有达成协议,但这一进程调动了研究、资金和公众参与。各国政府和社区不应等待达成协议,而应通过协调一致的国家规划、雄心勃勃的政策和地方举措,保持势头,为未来的条约做好准备。
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引用次数: 0
Past and future change in global river flows 全球河流流量的过去和未来变化
Pub Date : 2025-12-16 DOI: 10.1038/s43017-025-00745-z
Lukas Gudmundsson, Manuela I. Brunner, Petra Döll, Etienne Fluet-Chouinard, Natalia Frolova, Simon N. Gosling, Yukiko Hirabayashi, Maria B. Kireeva, Xiaomang Liu, Hannes Müller Schmied, Dmitriy Magritskiy, Louise J. Slater, Lina Stein, Yves Tramblay, Kaiwen Wang, Conrad Wasko, Dai Yamazaki, Xudong Zhou
Rivers are a vital component of the global water cycle. However, human influence on climate and terrestrial systems is increasingly shaping river flow regimes. In this Review, we summarize the current understanding of past and projected changes in global river flow, focusing on annual volumes, seasonal dynamics and sudden changes. River flow observations reveal distinct regional trends, including increased flows in high-latitude regions and decreased flows in parts of the mid-latitudes and subtropics. Snow-dominated regions in particular show shifts in their seasonal cycle towards earlier flows. These patterns align broadly with historical climate model simulations, suggesting an anthropogenic climate change signal. However, attribution is complicated by the interplay of greenhouse gas emissions, CO2-driven vegetation response, land-use change and water management. Future projections indicate continued change, with certain regions experiencing wetter conditions and others intensified drying. Seasonal changes, particularly those due to altered snow dynamics, are also expected to intensify. Despite modelling and observational advances, uncertainties remain regarding the combined effects of anthropogenic climate change and direct human interventions in terrestrial systems. Closing these gaps requires improved monitoring, advances in modelling and robust attribution frameworks, in support of efficiently managing water resources, sustaining ecosystems and adapting to a changing climate. Human influence on the climate and terrestrial systems is increasingly altering global river flow. This Review discusses past and projected changes in global river flow, with an emphasis on annual volumes, seasonal dynamics and sudden changes in flow dynamics.
河流是全球水循环的重要组成部分。然而,人类对气候和陆地系统的影响正日益影响着河流的流向。在这篇综述中,我们总结了目前对过去和预测的全球河流流量变化的理解,重点是年流量、季节动态和突然变化。河流流量观测显示了明显的区域趋势,包括高纬度地区流量增加,中纬度和亚热带部分地区流量减少。积雪占主导地位的地区尤其表现出季节周期向早期流动的转变。这些模式与历史气候模式模拟大体一致,表明存在人为气候变化信号。然而,由于温室气体排放、二氧化碳驱动的植被响应、土地利用变化和水资源管理的相互作用,归因变得复杂。未来的预测表明,变化将继续,某些地区将经历更湿润的条件,而其他地区将更加干燥。季节变化,特别是由于雪的动态变化,预计也会加剧。尽管在模拟和观测方面取得了进展,但在人为气候变化和人类对陆地系统的直接干预的综合影响方面仍然存在不确定性。缩小这些差距需要改进监测、改进建模和健全的归因框架,以支持有效管理水资源、维持生态系统和适应不断变化的气候。人类对气候和陆地系统的影响正日益改变着全球河流流量。这篇综述讨论了过去和预测的全球河流流量的变化,重点是年流量、季节动态和流量动态的突然变化。
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引用次数: 0
Advancing an adaptable and practical framework to address water quality challenges in a changing world 在不断变化的世界中,推进一个适应性强、实用的框架,以应对水质挑战
Pub Date : 2025-12-15 DOI: 10.1038/s43017-025-00753-z
Qian Zhang, Robert M. Hirsch, Laura A. DeCicco, Jennifer C. Murphy
As water-quality challenges intensify, the widely used Weighted Regressions on Time, Discharge, and Season (WRTDS) method offers an adaptable and practical framework for global water-quality science and management.
随着水质挑战的加剧,广泛使用的时间、流量和季节加权回归(WRTDS)方法为全球水质科学和管理提供了一个适应性强、实用的框架。
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引用次数: 0
Glacier biogeochemical cycling and downstream impacts 冰川生物地球化学循环及其下游影响
Pub Date : 2025-12-11 DOI: 10.1038/s43017-025-00751-1
Jon. R. Hawkings, James A. Bradley, Eva L. Doting, Noor Hassan, Katharine R. Hendry, Amy D. Holt, Eran Hood, Robert G. M. Spencer, Marek Stibal, Martyn Tranter, Ryan A. Venturelli, Jemma L. Wadham, Maya P. Bhatia
Far from being frozen and sterile environments, glaciers are biogeochemical reactors and regulators. In this Review, we discuss the hydrology and biogeochemistry of glacierized environments and their impact on downstream ecosystems. Supraglacial meltwaters export labile organic carbon associated with active supraglacial microbial communities, as well as carbon and nutrients delivered via atmospheric deposition. Meltwaters funnelled to the glacier bed and exiting at the glacier snout transport large quantities of rock flour as well as supraglacial and subglacial-derived organic carbon and nutrients to downstream ecosystems. Subglacial water flow paths influence rock–water contact times and vary greatly, affecting weathering reactions. For instance, the hydrology of mountain glaciers and the Greenland Ice Sheet is typically dominated by seasonal melt with short (hours) to medium (weeks) water residence times, although extended biogeochemical isolation can exist in more isolated parts of the Greenland Ice Sheet. Conversely, the Antarctic Ice Sheet is dominated by basal ice melt and residence times that can exceed years and decades. As a result, the latter supports extended biogeochemical isolation and more advanced chemical weathering. Microbial processes and physical-chemical weathering can both sequester or emit greenhouse gases, but the net effect remains unknown. Meltwaters can potentially fuel biological processes in downstream ecosystems by priming glacier-fed streams, fjords, and oceans with rock flour and nutrients. The rapid reduction in glacier area projected for the next century mandates that future research provides a critical assessment of the effects of deglaciation on watershed biogeochemistry, ecology and global biogeochemical cycles. Far from frozen and sterile environments, glaciers are biogeochemical reactors and regulators. This Review outlines key biogeochemical and associated physical processes occurring in glacierized environments and the known impacts of glaciers on elemental cycling and the Earth system.
冰川远非冰冻和贫瘠的环境,而是生物地球化学的反应器和调节器。本文综述了冰川环境的水文和生物地球化学特征及其对下游生态系统的影响。冰上融水输出与活跃的冰上微生物群落相关的不稳定有机碳,以及通过大气沉降输送的碳和营养物质。融水以漏斗状流入冰川床,从冰川口流出,将大量的石粉以及冰川上和冰川下产生的有机碳和营养物质输送到下游生态系统。冰下水流路径影响岩石-水接触时间,且变化很大,影响风化反应。例如,山地冰川和格陵兰冰盖的水文通常以季节性融化为主,水停留时间较短(数小时)至中等(数周),尽管在格陵兰冰盖较孤立的部分可能存在较长的生物地球化学隔离。相反,南极冰盖主要是基底冰融化和停留时间可能超过几年和几十年。因此,后者支持扩展的生物地球化学隔离和更高级的化学风化。微生物过程和物理-化学风化作用都可以隔离或排放温室气体,但净效应尚不清楚。融水可以潜在地为下游生态系统的生物过程提供燃料,因为它为冰川补给的溪流、峡湾和海洋注入了岩粉和营养物质。预计下个世纪冰川面积将迅速减少,这要求未来的研究对冰川消融对流域生物地球化学、生态学和全球生物地球化学循环的影响进行关键评估。远离冰冻和贫瘠的环境,冰川是生物地球化学的反应器和调节器。本文概述了冰川环境中发生的主要生物地球化学和相关物理过程,以及冰川对元素循环和地球系统的已知影响。
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引用次数: 0
Antarctic Bottom Water in a changing climate 气候变化中的南极底水
Pub Date : 2025-12-09 DOI: 10.1038/s43017-025-00750-2
Stephen R. Rintoul, Andrew L. Stewart, Gregory C. Johnson, Shenjie Zhou, Annie Foppert, Qian Li, Adele K. Morrison, Alessandro Silvano, Kathryn L. Gunn, Matthew H. England, Sohey Nihashi, Shigeru Aoki
Antarctic Bottom Water (AABW) is derived from dense water that sinks from the Antarctic continental shelf to the deep ocean. The sinking of AABW is balanced by a return flow of lighter water, and the resulting overturning circulation determines the density stratification of the deep ocean, regulates ocean storage of heat and carbon, and supplies oxygen to the deep sea. In this Review, we highlight progress in understanding how and why AABW is changing and the consequences for the deep overturning circulation. Since the mid-1980s, ocean heat content below 4,000 dbar has increased at a rate of 12.9 (±1.8) trillion watts, and the AABW has thinned by more than 50 dbar decade−1, with more rapid thinning observed closer to the sources of AABW. The abyssal overturning circulation has slowed in response to freshening of shelf waters by glacial melt and changes in sea ice formation. Numerical model simulations indicate that these trends will accelerate under projected increases in meltwater input. Future research priorities include sustained observations in the deep ocean and on the Antarctic continental shelf; exploration of feedbacks between ocean circulation, sea ice, dense water formation and ice shelf melt; and improved representation of AABW in ocean and climate models. Antarctic Bottom Water (AABW) sinks near Antarctica and fills the deep ocean. This Review discusses how AABW is formed, past changes to its properties and transport, and projects future changes in AABW and the deep overturning circulation.
南极底水(AABW)是由从南极大陆架下沉到深海的稠密水形成的。AABW的下沉由较轻的水回流来平衡,由此产生的翻转环流决定了深海的密度分层,调节了海洋的热量和碳储存,并为深海提供氧气。在这篇综述中,我们强调了在理解AABW如何和为什么发生变化以及深层翻转环流的后果方面取得的进展。自20世纪80年代中期以来,低于4,000 dbar的海洋热含量以12.9(±1.8)万亿瓦特的速度增加,而AABW已变薄超过50 dbar(10−1),在靠近AABW源的地方观测到更快速的变薄。由于冰川融化和海冰形成的变化,陆架水域变新鲜,深海翻转环流已经减缓。数值模式模拟表明,在预计融水输入增加的情况下,这些趋势将加速。未来的研究重点包括对深海和南极大陆架的持续观测;海洋环流、海冰、稠密水形成与冰架融化之间的反馈探讨改善了AABW在海洋和气候模式中的代表性。南极底水(AABW)在南极洲附近下沉,填满了深海。本文讨论了低空环流的形成过程、过去低空环流性质和运移的变化,并预测了低空环流和深翻转环流的未来变化。
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引用次数: 0
Climate impacts of the El Niño–Southern Oscillation on Australia 厄尔尼诺Niño-Southern涛动对澳大利亚的气候影响
Pub Date : 2025-12-04 DOI: 10.1038/s43017-025-00747-x
Andréa S. Taschetto, Shayne McGregor, Dietmar Dommenget, Zoe E. Gillett, Neville Nicholls, Sur Sharmila, Peter van Rensch, Danielle Verdon-Kidd, Ghyslaine Boschat, Christine Chung, Ruby Lieber, Nerilie Abram, Rob Allan, Kathryn Allen, Linden Ashcroft, Josephine R. Brown, Wenju Cai, Savin Chand, Tim Cowan, Thi Lan Dao, Catherine de Burgh-Day, Mandy B. Freund, Ailie Gallant, Joelle Gergis, Neil J. Holbrook, Hanna Heidemann, Chiara Holgate, Pandora Hope, Andrew King, Eun-Pa Lim, John L. McBride, Roseanna C. McKay, Hanh Nguyen, Acacia Pepler, Sarah Perkins-Kirkpatrick, Scott Power, James S. Risbey, Agus Santoso, Caroline C. Ummenhofer, Guojian Wang, Xuebin Zhang
El Niño–Southern Oscillation (ENSO) profoundly affects Australian weather, climate, ecosystems and socio-economic sectors. In this Review, we summarize the advances in understanding the ENSO–Australian climate relationship, detailing the complexity beyond the traditional assumptions of El Niño-dry and La Niña-wet patterns, including mechanisms and impacts. The influence of ENSO is most coherent during austral spring, explaining about a quarter of rainfall variability over large parts of eastern Australia. La Niña typically exerts more robust rainfall changes than El Niño, and the Central Pacific El Niño has greater impacts than Eastern Pacific events. These effects are amplified by prolonged ENSO episodes and modulated by land–atmosphere feedback, surrounding sea surface temperatures, local processes and interactions with other climate modes, including multidecadal variability. El Niño-related drying generally worsens when co-occurring with positive Indian Ocean Dipole (IOD) and/or negative Southern Annular Mode (SAM), whereas La Niña rainfall intensifies with negative IOD and/or positive SAM. Although ENSO predictability has improved with advanced understanding of ocean processes and dynamical forecasting, predicting its impacts is challenging because of large internal atmospheric variability. Ongoing changes in ENSO underscore the need for strategic research, continuous in situ monitoring, reduced model biases and deeper understanding of the anthropogenically induced changes in Pacific temperatures to guide adaptation strategies. El Niño–Southern Oscillation (ENSO) profoundly affects Australian weather, climate, ecosystems and socio-economic sectors. This Review presents the progress made in understanding ENSO teleconnections to Australian weather over the past 40 years, describing the atmospheric dynamics, complexities and impacts of this climate phenomenon.
厄尔尼诺Niño-Southern涛动(ENSO)深刻地影响着澳大利亚的天气、气候、生态系统和社会经济部门。在这篇综述中,我们总结了在理解ENSO-Australian气候关系方面的进展,详细介绍了El Niño-dry和La Niña-wet模式的传统假设之外的复杂性,包括机制和影响。ENSO的影响在南部春季最为一致,可以解释澳大利亚东部大部分地区约四分之一的降雨变化。La Niña通常比El Niño产生更强劲的降雨变化,中太平洋El Niño比东太平洋事件产生更大的影响。这些影响被延长的ENSO事件放大,并受到陆地-大气反馈、周围海面温度、当地过程以及与其他气候模式(包括多年代际变率)的相互作用的调节。当El Niño-related与印度洋偶极子(IOD)正态和/或南环模(SAM)负态同时发生时,干燥通常会恶化,而La Niña与印度洋偶极子负态和/或南环模正态同时发生时,降雨会加剧。尽管随着对海洋过程和动力预报的深入了解,ENSO的可预测性有所提高,但由于大气内部变化很大,预测其影响仍具有挑战性。ENSO的持续变化强调需要进行战略研究、持续的原位监测、减少模式偏差和更深入地了解人为引起的太平洋温度变化,以指导适应战略。厄尔尼诺Niño-Southern涛动(ENSO)深刻地影响着澳大利亚的天气、气候、生态系统和社会经济部门。本综述介绍了过去40年来在理解ENSO与澳大利亚天气的遥相关方面取得的进展,描述了这种气候现象的大气动力学、复杂性和影响。
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引用次数: 0
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