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Advancing Our Understanding of Eddy-driven Jet Stream Responses to Climate Change – A Roadmap 推进我们对涡流驱动喷气流应对气候变化的认识--路线图
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-11-06 DOI: 10.1007/s40641-024-00199-3
Albert Ossó, Ileana Bladé, Alexey Karpechko, Camille Li, Douglas Maraun, Olivia Romppainen-Martius, Len Shaffrey, Aiko Voigt, Tim Woollings, Giuseppe Zappa

Purpose of Review

Extratropical jets and associated storm tracks significantly influence weather and regional climate across various timescales. Understanding jet responses to climate change is essential for reliable regional climate projections. This review serves two main purposes: (1) to provide an accessible overview of extratropical jet dynamics and a comprehensive examination of current challenges and uncertainties in predicting jet responses to greenhouse gas increases and (2) to suggest innovative experiments to advance our understanding of these responses.

Recent Findings

While successive generations of climate model ensembles consistently project a mean poleward shift of the midlatitude zonal-mean maximum winds, there remains considerable intermodel spread and large uncertainty across seasonal and regional jet responses. Of particular note is our limited understanding of how these jets respond to the intricate interplay of multiple concurrent drivers, such as the strong warming in polar and tropical regions, and the relative importance of each factor. Furthermore, the difficulty of simulating processes requiring high resolution, such as those linked to sharp sea surface temperature gradients or diabatic effects related to tropical convection and extratropical cyclones, has historically hindered progress.

Summary

We advocate for a collaborative effort to enhance our understanding of the jet stream response to climate change. We propose a series of new experiments that take advantage of recent advances in computing power and modelling capabilities to better resolve small-scale processes such as convective circulations, which we consider essential for a good representation of jet dynamics.

审查目的外热带喷流和相关风暴轨道在不同时间尺度上对天气和区域气候有重大影响。了解喷流对气候变化的响应对于可靠的区域气候预测至关重要。本综述有两个主要目的:(1)提供关于外热带喷流动力学的简明概述,并全面探讨目前在预测喷流对温室气体增加的响应方面所面临的挑战和不确定性;(2)提出创新性实验建议,以促进我们对这些响应的理解。最近的研究结果虽然连续几代气候模式集合一致预测中纬度地带性平均最大风向极地移动,但在季节性和区域性喷流响应方面仍存在相当大的模式间差异和不确定性。特别值得注意的是,我们对这些喷流如何应对多种并发驱动因素的复杂相互作用(如极地和热带地区的强烈变暖)以及每个因素的相对重要性了解有限。此外,由于难以模拟需要高分辨率的过程,例如与急剧的海面温度梯度或与热带对流和外热带气旋相关的二重效应有关的过程,这一直阻碍着研究的进展。我们提出了一系列新实验,利用最近计算能力和建模能力的进步,更好地解析对流环流等小尺度过程。
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引用次数: 0
Climate Change and Hydrological Extremes 气候变化与极端水文现象
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-10-02 DOI: 10.1007/s40641-024-00198-4
Jinghua Xiong, Yuting Yang

Purpose of Review

Climate change has profoundly impacted the Earth's atmospheric system and altered the terrestrial water cycle, reshaping the spatiotemporal patterns of hydrological extremes, including floods and droughts. This review aims to summarize recent advancements in understanding the response of hydrological extremes to climate change in both past and future.

Recent Findings

Historical floods driven by heavy rainfall are increasing, while those dominated by snow processes are decreasing, resulting in non-significant changes on a global average. Previously overestimated droughts, due to inaccuracies in hydrological modules within offline diagnostic metrics, have been corrected by advanced modeling results, also revealing minimal historical changes on a global scale. Earth system simulations project concurrent increases in both floods and droughts under future climate change scenarios.

Summary

Climate change influences hydrological extremes across various scales, with diverse spatial distributions and underlying mechanisms. Decision-makers should integrate multi-source information to enhance the monitoring and adaptation of hydrological extremes, particularly focusing on abrupt drought-flood alternations.

综述目的气候变化深刻影响了地球的大气系统,改变了陆地水循环,重塑了极端水文现象(包括洪水和干旱)的时空模式。本综述旨在总结最近在理解极端水文现象对过去和未来气候变化的响应方面取得的进展。最新发现历史上由强降雨驱动的洪水正在增加,而由降雪过程主导的洪水正在减少,导致全球平均洪水变化不大。以前由于离线诊断指标中的水文模块不准确而高估的干旱,已被先进的建模结果所纠正,同时也揭示了全球范围内的微小历史变化。地球系统模拟预测,在未来气候变化情景下,洪水和干旱会同时增加。决策者应整合多源信息,加强对极端水文现象的监测和适应,尤其要关注突发性旱涝交替现象。
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引用次数: 0
More Climate Finance from More Countries? 更多国家提供更多气候资金?
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-07-24 DOI: 10.1007/s40641-024-00197-5
W. Pieter Pauw, Michael König-Sykorova, María José Valverde, Luis H. Zamarioli

Purpose of Review

This paper analyses the options to broaden the base of climate finance provided by countries in a mixed-methods review. It (1) reviews Non-Annex II countries’ commitments in international agreements, declarations, and agendas; (2) provides and applies a literature-based review of criteria to identify countries’ responsibilities and capabilities to provide finance; (3) reviews institutional affiliation; and (4) reviews countries’ willingness to provide finance through their contributions to 27 relevant multilateral funds.

Recent Findings

Scaling up climate finance has been a political and operational priority for the UN climate negotiations. However, the Annex II list of countries that commit to support developing countries financially with mitigation and adaptation has hardly changed since 1992. Given countries’ diverse emission pathways and economic development as well as geopolitical dynamics, Annex II is turning into a weakness of the UNFCCC in times when developing countries’ climate finance needs are increasing.

Summary

Our largely qualitative analysis indicates that Eastern European countries, Russia, South Korea, Türkiye, Monaco, and Gulf States (including Saudi Arabia) meet many justifications for further negotiations about the expansion of the climate finance provider base. However, we argue against a continued rigid dichotomy of providers and recipients. We recommend four innovations going forward, including establishing ‘net recipients’ as a third category; this 1) broadens the base; 2) increases climate finance; and 3) could increase effectiveness and cooperation. More research is needed on the role of countries’ vulnerability and debt levels in discussions on climate finance provision.

综述目的 本文通过混合方法综述,分析了扩大各国气候融资基础的备选方案。本文 (1) 回顾了非附件二国家在国际协议、宣言和议程中的承诺;(2) 提供并应用了基于文献的标准回顾,以确定各国提供资金的责任和能力;(3) 回顾了机构隶属关系;以及 (4) 回顾了各国通过向 27 个相关多边基金捐款来提供资金的意愿。然而,自 1992 年以来,附件二中承诺在资金上支持发展中国家减缓和适应气候变化的国家名单几乎没有变化。鉴于各国不同的排放路径和经济发展状况以及地缘政治动态,在发展中国家的气候资金需求不断增加的情况下,附件二正在成为《联合国气候变化框架公约》的一个弱点。摘要我们的分析主要是定性分析,分析表明东欧国家、俄罗斯、韩国、土耳其、摩纳哥和海湾国家(包括沙特阿拉伯)符合进一步谈判扩大气候资金提供者基础的许多理由。然而,我们反对继续僵化地将提供方和接受方对立起来。我们建议今后采取四项创新措施,包括将 "净受援国 "作为第三类;这将:1)扩大基础;2)增加气候资金;3)提高效率,加强合作。需要对各国的脆弱性和债务水平在气候资金提供讨论中的作用进行更多研究。
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引用次数: 0
The Multi-Scalar Inequities of Climate Adaptation Finance: A Critical Review 气候适应融资的多尺度不平等:批判性评论
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-05-23 DOI: 10.1007/s40641-024-00195-7
Kayin Venner, Melissa García-Lamarca, Marta Olazabal

Purpose of Review

Following a multi-scalar analytical approach, this critical literature review explores the factors that determine adaptation finance accessibility and allocation with particular attention to how the needs of climate-vulnerable communities are considered.

Recent Findings

Our review reveals that climate vulnerability is not a primary determinant in the accessibility and allocation of climate adaptation finance at inter-state, sub-national and local scales. Instead, factors such as institutional capacities and financial and political interests exert significant influence. This leads to maladaptation and multi-scalar inequities where climate finance favours relatively resilient groups across scales with less support for more vulnerable populations.

Summary

We argue that finance does not trickle down, but “ripples” within a climate finance arena – where we define the latter as a messy space of competition, negotiation and collaboration. To unlock equitable adaptation finance patterns, future research should focus on the multi-scalar configurations of adaptation finance beyond the international level and consider local and regional territorial and scalar politics.

最近的研究结果我们的研究表明,在国家间、国家以下和地方范围内,气候脆弱性并不是气候适应资金获取和分配的主要决定因素。相反,机构能力、财政和政治利益等因素发挥着重要影响。我们认为,资金不会 "涓滴 "而下,而是在气候融资领域内 "荡漾"--我们将后者定义为竞争、谈判与合作的混乱空间。为了开启公平的适应性融资模式,未来的研究应关注国际层面以外的适应性融资的多尺度配置,并考虑地方和区域的地域和尺度政治。
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引用次数: 0
Equity and Justice in Loss and Damage Finance: A Narrative Review of Catalysts and Obstacles 损失和损害赔偿融资中的公平与公正:催化剂与障碍的叙述性回顾
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-05-20 DOI: 10.1007/s40641-024-00196-6
Ike Uri, Stacy-ann Robinson, J. Timmons Roberts, David Ciplet, Romain Weikmans, Mizan Khan

Purpose of Review

Recent focus on loss and damage within the United Nations Framework Convention on Climate Change (UNFCCC) follows decades of demands by vulnerable countries for compensation for losses due to climate change. Reviewing recent literature on loss and damage finance, we consider how the new UNFCCC Loss and Damage Fund could be transformative for climate finance.

Recent Findings

This article reviews developments within the UNFCCC, including the creation of the new Loss and Damage Fund and changes in the broader field of climate finance. Recent literature indicates that the factors necessary for just loss and damage finance include inclusive governance, new and additional funds, purpose-made instruments and channels, direct access to funds, and burden sharing aligned with the polluter pays principle.

Summary

We overview the history of loss and damage finance, suggest five criteria that could make the Loss and Damage Fund just, and discuss four potential catalysts for just loss and damage finance: ecological and climatic impacts, institutional developments outside the UNFCCC, Global South leadership on debt justice, and legal developments. As the Loss and Damage Fund is operationalized and the need for loss and damage finance grows, scholars must continue to ask whether loss and damage finance furthers core tenets of climate justice, including forms of restitution.

回顾的目的《联合国气候变化框架公约》(UNFCCC)最近对损失和损害问题的关注是在脆弱国家数十年来要求对气候变化造成的损失进行赔偿之后。本文回顾了《联合国气候变化框架公约》的发展,包括新的损失和损害基金的设立以及更广泛的气候融资领域的变化。摘要我们概述了损失和损害融资的历史,提出了可使损失和损害基金公正的五项标准,并讨论了公正损失和损害融资的四种潜在催化剂:生态和气候影响、《联合国气候变化框架公约》之外的制度发展、全球南方在债务公正方面的领导力以及法律发展。随着损失和损害赔偿基金的运作以及对损失和损害赔偿融资需求的增长,学者们必须继续追问损失和损害赔偿融资是否促进了气候正义的核心原则,包括恢复原状的形式。
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引用次数: 0
Solar-Induced Chlorophyll Fluorescence (SIF): Towards a Better Understanding of Vegetation Dynamics and Carbon Uptake in Arctic-Boreal Ecosystems 太阳诱导叶绿素荧光 (SIF):更好地了解北极-北方生态系统的植被动态和碳吸收情况
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-04-04 DOI: 10.1007/s40641-024-00194-8

Abstract

Purpose of Review

Terrestrial ecosystems in the Arctic-Boreal region play a crucial role in the global carbon cycle as a carbon sink. However, rapid warming in this region induces uncertainties regarding the future net carbon exchange between land and the atmosphere, highlighting the need for better monitoring of the carbon fluxes. Solar-Induced chlorophyll Fluorescence (SIF), a good proxy for vegetation CO (^{2}) uptake, has been broadly utilized to assess vegetation dynamics and carbon uptake at the global scale. However, the full potential and limitations of SIF in the Arctic-Boreal region have not been explored. Therefore, this review aims to provide a comprehensive summary of the latest insights into Arctic-Boreal carbon uptake through SIF analyses, underscoring the advances and challenges of SIF in solving emergent unknowns in this region. Additionally, this review proposes applications of SIF across scales in support of other observational and modeling platforms for better understanding Arctic-Boreal vegetation dynamics and carbon fluxes.

Recent Findings

Cross-scale SIF measurements complement each other, offering valuable perspectives on Arctic-Boreal ecosystems, such as vegetation phenology, carbon uptake, carbon-water coupling, and ecosystem responses to disturbances. By incorporating SIF into land surface modeling, the understanding of Arctic-Boreal changes and their climate drivers can be mechanistically enhanced, providing critical insights into the changes of Arctic-Boreal ecosystems under global warming.

Summary

While SIF measurements are more abundant and with finer spatiotemporal resolutions, it is important to note that the coverage of these measurements is still limited and uneven in the Arctic-Boreal region. To address this limitation and further advance our understanding of the Arctic-Boreal carbon cycle, this review advocates for fostering a SIF network providing long-term and continuous measurements across spatial scales. Simultaneously measuring SIF and other environmental variables in the context of a multi-modal sensing system can help us comprehensively characterize Arctic-Boreal ecosystems with spatial details in land surface models, ultimately contributing to more robust climate projections.

摘要 综述目的 北极-北方地区的陆地生态系统作为碳汇在全球碳循环中发挥着至关重要的作用。然而,该地区的快速变暖给未来陆地与大气之间的净碳交换带来了不确定性,因此需要更好地监测碳通量。太阳诱导叶绿素荧光(SIF)是植被吸收二氧化碳的良好替代物,已被广泛用于评估全球范围内的植被动态和碳吸收。然而,SIF 在北极-北方地区的全部潜力和局限性尚未得到探索。因此,本综述旨在全面总结通过 SIF 分析对北极-北方地区碳吸收的最新见解,强调 SIF 在解决该地区新出现的未知问题方面所取得的进展和面临的挑战。此外,本综述还提出了跨尺度 SIF 的应用,以支持其他观测和建模平台,从而更好地了解北极-北方植被动态和碳通量。 最新发现 跨尺度 SIF 测量结果相辅相成,为北极-北方生态系统提供了宝贵的视角,如植被物候、碳吸收、碳-水耦合以及生态系统对干扰的响应。通过将 SIF 纳入陆地表面建模,可以从机理上加强对北极-北方变化及其气候驱动因素的理解,从而为了解全球变暖下北极-北方生态系统的变化提供重要见解。 小结 虽然 SIF 测量数据更加丰富,时空分辨率也更精细,但必须指出的是,这些测量数据在北极-北方地区的覆盖范围仍然有限,而且不均衡。为解决这一局限性,进一步推动我们对北极-北冰洋碳循环的了解,本综述主张建立一个 SIF 网络,提供跨空间尺度的长期连续测量。在多模式传感系统的背景下同时测量 SIF 和其他环境变量,可帮助我们在地表模型中全面描述北极-北冰洋生态系统的空间细节,最终有助于更可靠的气候预测。
{"title":"Solar-Induced Chlorophyll Fluorescence (SIF): Towards a Better Understanding of Vegetation Dynamics and Carbon Uptake in Arctic-Boreal Ecosystems","authors":"","doi":"10.1007/s40641-024-00194-8","DOIUrl":"https://doi.org/10.1007/s40641-024-00194-8","url":null,"abstract":"<h3>Abstract</h3> <span> <h3>Purpose of Review</h3> <p>Terrestrial ecosystems in the Arctic-Boreal region play a crucial role in the global carbon cycle as a carbon sink. However, rapid warming in this region induces uncertainties regarding the future net carbon exchange between land and the atmosphere, highlighting the need for better monitoring of the carbon fluxes. Solar-Induced chlorophyll Fluorescence (SIF), a good proxy for vegetation CO<span> <span>(^{2})</span> </span> uptake, has been broadly utilized to assess vegetation dynamics and carbon uptake at the global scale. However, the full potential and limitations of SIF in the Arctic-Boreal region have not been explored. Therefore, this review aims to provide a comprehensive summary of the latest insights into Arctic-Boreal carbon uptake through SIF analyses, underscoring the advances and challenges of SIF in solving emergent unknowns in this region. Additionally, this review proposes applications of SIF across scales in support of other observational and modeling platforms for better understanding Arctic-Boreal vegetation dynamics and carbon fluxes.</p> </span> <span> <h3>Recent Findings</h3> <p>Cross-scale SIF measurements complement each other, offering valuable perspectives on Arctic-Boreal ecosystems, such as vegetation phenology, carbon uptake, carbon-water coupling, and ecosystem responses to disturbances. By incorporating SIF into land surface modeling, the understanding of Arctic-Boreal changes and their climate drivers can be mechanistically enhanced, providing critical insights into the changes of Arctic-Boreal ecosystems under global warming.</p> </span> <span> <h3>Summary</h3> <p>While SIF measurements are more abundant and with finer spatiotemporal resolutions, it is important to note that the coverage of these measurements is still limited and uneven in the Arctic-Boreal region. To address this limitation and further advance our understanding of the Arctic-Boreal carbon cycle, this review advocates for fostering a SIF network providing long-term and continuous measurements across spatial scales. Simultaneously measuring SIF and other environmental variables in the context of a multi-modal sensing system can help us comprehensively characterize Arctic-Boreal ecosystems with spatial details in land surface models, ultimately contributing to more robust climate projections.</p> </span>","PeriodicalId":54235,"journal":{"name":"Current climate change reports","volume":"54 1","pages":""},"PeriodicalIF":9.5,"publicationDate":"2024-04-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140343595","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Hydrologic Extremes in a Changing Climate: a Review of Extremes in East Africa 不断变化的气候中的极端水文现象:东非极端水文现象综述
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-01-18 DOI: 10.1007/s40641-024-00193-9
Meron Teferi Taye, Ellen Dyer

Abstract

Purpose

Eastern Africa has a complex hydroclimate and socio-economic context, making it vulnerable to climate change-induced hydrological extremes. This review presents recent research on drivers and typologies of extremes across different geographies and highlights challenges and improvements in forecasting hydrological extremes at various timescales.

Recent Findings

Droughts and floods remain the major challenges of the region. Recently, frequent alterations between droughts and floods have been a common occurrence and concern. Research underlines the heterogeneity of extremes and the impact of climate change as increased intensity and duration of extremes. Moreover, the importance of local and antecedent conditions in changing the characteristics of extremes is emphasized.

Summary

A better understanding of these drivers and how they interact is required. Observational and modeling tools must capture these relationships and extremes on short timescales. Although there are improvements in forecasting these extremes, providing relevant information beyond meteorological variables requires further research.

摘要 目的 东非具有复杂的水文气候和社会经济背景,因此很容易受到气候变化引起的极端水文现象的影响。本综述介绍了最近对不同地域极端现象的驱动因素和类型进行的研究,并强调了在不同时间尺度上预报极端水文现象所面临的挑战和改进之处。最近,干旱和洪水之间的频繁变化已成为一种普遍现象,并引起了人们的关注。研究强调了极端天气的异质性,以及气候变化对极端天气强度和持续时间增加的影响。此外,研究还强调了当地条件和先决条件在改变极端气候特征方面的重要性。观测和建模工具必须在短时尺度上捕捉这些关系和极端现象。尽管在预报这些极端天气方面有所改进,但要提供气象变量以外的相关信息,还需要进一步的研究。
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引用次数: 0
Global Review of Modification, Optimization, and Improvement Models for Aquifer Vulnerability Assessment in the Era of Climate Change 气候变化时代含水层脆弱性评估的修改、优化和改进模型全球回顾
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-01-06 DOI: 10.1007/s40641-023-00192-2

Abstract

Purpose of Review

This review aims to examine the methods used to date in assessing aquifer vulnerability over the last three decades (1993-2023). In addition to a comprehensive review of prior AVA research, the novelty of this study lies in its specific focus on these methods and their application to the widely used DRASTIC and GALDIT models. We particularly emphasize statistical analysis, multicriteria decision-making, optimization techniques, machine learning algorithms, and deep learning (DL) models.

Recent findings

The most widely used modification, optimization, and improvement-based methods for DRASTIC indices are the analytic hierarchy process, genetic algorithm, and fuzzy logic. In contrast, single-parameter sensitivity analysis, genetic algorithm, and support vector machine are commonly applied to modify, optimize, and improve GALDIT indices.

Summary

The results of this study are important especially in the era of global warming and climate change/variability when the need and demand for aquifers and groundwater resources is increasing.

摘要 综述目的 本综述旨在研究过去三十年(1993-2023 年)中迄今为止用于评估含水层脆弱性的 方法。除了对之前的含水层脆弱性评估研究进行全面回顾外,本研究的新颖之处还在于特别关注这些方法及其在广泛使用的 DRASTIC 和 GALDIT 模型中的应用。我们特别强调统计分析、多标准决策、优化技术、机器学习算法和深度学习 (DL) 模型。 最新发现 DRASTIC 指数最广泛使用的修改、优化和改进方法是层次分析法、遗传算法和模糊逻辑。相比之下,单参数灵敏度分析、遗传算法和支持向量机通常用于修改、优化和改进 GALDIT 指数。 小结 本研究的结果非常重要,尤其是在全球变暖和气候变化/多变的时代,对含水层和地下水资源的需求与日俱增。
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引用次数: 0
Recent Advances and Challenges in Monitoring and Modeling Non-Growing Season Carbon Dioxide Fluxes from the Arctic Boreal Zone 北极寒带非生长季二氧化碳通量监测与模拟的最新进展与挑战
1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2023-10-26 DOI: 10.1007/s40641-023-00190-4
Kyle A. Arndt, Josh Hashemi, Susan M. Natali, Luke D. Schiferl, Anna-Maria Virkkala
Abstract Purpose of Review While previously thought to be negligible, carbon emissions during the non-growing season (NGS) can be a substantial part of the annual carbon budget in the Arctic boreal zone (ABZ), which can shift the carbon balance of these ecosystems from a long-held annual carbon sink towards a net annual carbon source. The purpose of this review is to summarize NGS carbon dioxide (CO 2 ) flux research in the ABZ that has been published within the past 5 years. Recent Findings We explore the processes and magnitudes of CO 2 fluxes, and the status of modeling efforts, and evaluate future directions. With technological advances, direct measurements of NGS fluxes are increasing at sites across the ABZ over the past decade, showing ecosystems in the ABZ are a large source of CO 2 in the shoulder seasons, with low, consistent, winter emissions. Summary Ecosystem carbon cycling models are being improved with some challenges, such as modeling below ground and snow processes, which are critical to understanding NGS CO 2 fluxes. A lack of representative in situ carbon flux data and gridded environmental data are leading limiting factors preventing more accurate predictions of NGS carbon fluxes.
虽然以前认为碳排放可以忽略不计,但非生长季(NGS)的碳排放可能是北极寒带(ABZ)年度碳预算的重要组成部分,它可以将这些生态系统的碳平衡从长期存在的年度碳汇转变为年度净碳源。本文综述了近5年来在ABZ地区已发表的NGS二氧化碳(CO 2)通量研究。我们探讨了co2通量的过程和大小,以及模拟工作的现状,并评估了未来的方向。随着技术的进步,在过去十年中,在整个ABZ的站点对NGS通量的直接测量正在增加,这表明ABZ的生态系统是CO 2的一个主要来源,在肩部季节,排放量低,一致,冬季。生态系统碳循环模型正在不断改进,但也面临着一些挑战,例如模拟地下和积雪过程,这对了解NGS CO 2通量至关重要。缺乏具有代表性的原位碳通量数据和网格化环境数据是阻碍更准确地预测NGS碳通量的主要限制因素。
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引用次数: 0
Uncertainty and Climate Change Adaptation: a Systematic Review of Research Approaches and People’s Decision-Making 不确定性与气候变化适应:研究方法与人们决策的系统回顾
IF 9.5 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2023-02-17 DOI: 10.1007/s40641-023-00189-x
M. Moure, J. Jacobsen, C. Smith-Hall
{"title":"Uncertainty and Climate Change Adaptation: a Systematic Review of Research Approaches and People’s Decision-Making","authors":"M. Moure, J. Jacobsen, C. Smith-Hall","doi":"10.1007/s40641-023-00189-x","DOIUrl":"https://doi.org/10.1007/s40641-023-00189-x","url":null,"abstract":"","PeriodicalId":54235,"journal":{"name":"Current climate change reports","volume":"9 1","pages":"1-26"},"PeriodicalIF":9.5,"publicationDate":"2023-02-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48675244","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
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Current climate change reports
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