首页 > 最新文献

Reviews of Geophysics最新文献

英文 中文
Advances in Mapping Lowermost Mantle Convective Flow With Seismic Anisotropy Observations 利用地震各向异性观测绘制最下部地幔对流图的进展
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-05-17 DOI: 10.1029/2023RG000833
Jonathan Wolf, Mingming Li, Maureen D. Long, Edward Garnero

Convective flow in the deep mantle controls Earth's dynamic evolution, influences plate tectonics, and has shaped Earth's current surface features. Present and past convection-induced deformation manifests itself in seismic anisotropy, which is particularly strong in the mantle's uppermost and lowermost portions. While the general patterns of seismic anisotropy have been mapped for the upper mantle, anisotropy in the lowermost mantle (called D′′) is at an earlier stage of exploration. Here we review recent progress in methods to measure and interpret D′′ anisotropy. Our understanding of the limitations of existing methods and the development of new measurement strategies have been aided enormously by the availability of high-performance computing resources. We give an overview of how measurements of seismic anisotropy can help constrain the mineralogy and fabric of the deep mantle. Specifically, new and creative strategies that combine multiple types of observations provide much tighter constraints on the geometry of anisotropy than have previously been possible. We also discuss how deep mantle seismic anisotropy provides insights into lowermost mantle dynamics. We summarize what we have learned so far from measurements of D′′ anisotropy, how inferences of lowermost mantle flow from measurements of seismic anisotropy relate to geodynamic models of mantle flow, and what challenges we face going forward. Finally, we discuss some of the important unsolved problems related to the dynamics of the lowermost mantle that can be elucidated in the future by combining observations of seismic anisotropy with geodynamic predictions of lowermost mantle flow.

地幔深处的对流控制着地球的动态演化,影响着板块构造,并塑造了地球目前的地表特征。目前和过去对流引起的形变表现为地震各向异性,在地幔的最上层和最下层尤为明显。虽然已经绘制了上地幔地震各向异性的一般模式图,但最下层地幔的各向异性(称为 D′′)还处于探索的早期阶段。在此,我们回顾了在测量和解释 D′′各向异性方法方面的最新进展。我们对现有方法局限性的理解和新测量策略的开发都得益于高性能计算资源的可用性。我们将概述地震各向异性测量如何帮助约束深地幔的矿物学和结构。具体来说,结合多种类型观测的新颖策略对各向异性的几何形状提供了比以往更为严格的约束。我们还讨论了深地幔地震各向异性如何深入了解最底层地幔动力学。我们总结了迄今为止我们从 D′′ 各向异性测量中了解到的情况,从地震各向异性测量中推断最底层地幔流动与地幔流动地球动力学模型之间的关系,以及我们未来面临的挑战。最后,我们讨论了与最下地幔动力学有关的一些尚未解决的重要问题,这些问题可以在未来通过将地震各向异性观测与最下地幔流动的地球动力学预测结合起来加以阐明。
{"title":"Advances in Mapping Lowermost Mantle Convective Flow With Seismic Anisotropy Observations","authors":"Jonathan Wolf,&nbsp;Mingming Li,&nbsp;Maureen D. Long,&nbsp;Edward Garnero","doi":"10.1029/2023RG000833","DOIUrl":"10.1029/2023RG000833","url":null,"abstract":"<p>Convective flow in the deep mantle controls Earth's dynamic evolution, influences plate tectonics, and has shaped Earth's current surface features. Present and past convection-induced deformation manifests itself in seismic anisotropy, which is particularly strong in the mantle's uppermost and lowermost portions. While the general patterns of seismic anisotropy have been mapped for the upper mantle, anisotropy in the lowermost mantle (called D′′) is at an earlier stage of exploration. Here we review recent progress in methods to measure and interpret D′′ anisotropy. Our understanding of the limitations of existing methods and the development of new measurement strategies have been aided enormously by the availability of high-performance computing resources. We give an overview of how measurements of seismic anisotropy can help constrain the mineralogy and fabric of the deep mantle. Specifically, new and creative strategies that combine multiple types of observations provide much tighter constraints on the geometry of anisotropy than have previously been possible. We also discuss how deep mantle seismic anisotropy provides insights into lowermost mantle dynamics. We summarize what we have learned so far from measurements of D′′ anisotropy, how inferences of lowermost mantle flow from measurements of seismic anisotropy relate to geodynamic models of mantle flow, and what challenges we face going forward. Finally, we discuss some of the important unsolved problems related to the dynamics of the lowermost mantle that can be elucidated in the future by combining observations of seismic anisotropy with geodynamic predictions of lowermost mantle flow.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"62 2","pages":""},"PeriodicalIF":25.2,"publicationDate":"2024-05-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140954555","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
Expressing Gratitude to Reviewers: A Message From the Editors of Reviews of Geophysics for 2023 向审稿人表示感谢:地球物理学评论》编辑 2023 年致辞
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-04-24 DOI: 10.1029/2024RG000844
Qingyun Duan, Valerio Acocella, Ann Marie Carlton, Paolo D’Odorico, Fabio Florindo, Andrew Gettelman, Jasper Halakas, Ruth Harris, Gesine Mollenhauer, Alan Robock, Claudine Stirling, Yusuke Yokoyama

On behalf of the authors and readers of Reviews of Geophysics (RoG), the American Geophysical Union, and the broader scientific community, the editors wish to wholeheartedly thank those who reviewed manuscripts for RoG in 2023.

编者谨代表《地球物理学评论》(Reviews of Geophysics,RoG)的作者和读者、美国地球物理学联合会以及更广泛的科学界,衷心感谢 2023 年为《地球物理学评论》审稿的人员。
{"title":"Expressing Gratitude to Reviewers: A Message From the Editors of Reviews of Geophysics for 2023","authors":"Qingyun Duan,&nbsp;Valerio Acocella,&nbsp;Ann Marie Carlton,&nbsp;Paolo D’Odorico,&nbsp;Fabio Florindo,&nbsp;Andrew Gettelman,&nbsp;Jasper Halakas,&nbsp;Ruth Harris,&nbsp;Gesine Mollenhauer,&nbsp;Alan Robock,&nbsp;Claudine Stirling,&nbsp;Yusuke Yokoyama","doi":"10.1029/2024RG000844","DOIUrl":"https://doi.org/10.1029/2024RG000844","url":null,"abstract":"<p>On behalf of the authors and readers of Reviews of Geophysics (RoG), the American Geophysical Union, and the broader scientific community, the editors wish to wholeheartedly thank those who reviewed manuscripts for RoG in 2023.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"62 2","pages":""},"PeriodicalIF":25.2,"publicationDate":"2024-04-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024RG000844","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140639547","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Land Data Assimilation: Harmonizing Theory and Data in Land Surface Process Studies 陆地数据同化:陆地表面过程研究中的理论与数据协调
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-03-19 DOI: 10.1029/2022RG000801
Xin Li, Feng Liu, Chunfeng Ma, Jinliang Hou, Donghai Zheng, Hanqing Ma, Yulong Bai, Xujun Han, Harry Vereecken, Kun Yang, Qingyun Duan, Chunlin Huang

Data assimilation plays a dual role in advancing the “scientific” understanding and serving as an “engineering tool” for the Earth system sciences. Land data assimilation (LDA) has evolved into a distinct discipline within geophysics, facilitating the harmonization of theory and data and allowing land models and observations to complement and constrain each other. Over recent decades, substantial progress has been made in the theory, methodology, and application of LDA, necessitating a holistic and in-depth exploration of its full spectrum. Here, we present a thorough review elucidating the theoretical and methodological developments in LDA and its distinctive features. This encompasses breakthroughs in addressing strong nonlinearities in land surface processes, exploring the potential of machine learning approaches in data assimilation, quantifying uncertainties arising from multiscale spatial correlation, and simultaneously estimating model states and parameters. LDA has proven successful in enhancing the understanding and prediction of various land surface processes (including soil moisture, snow, evapotranspiration, streamflow, groundwater, irrigation and land surface temperature), particularly within the realms of water and energy cycles. This review outlines the development of global, regional, and catchment-scale LDA systems and software platforms, proposing grand challenges of generating land reanalysis and advancing coupled land‒atmosphere DA. We lastly highlight the opportunities to expand the applications of LDA from pure geophysical systems to coupled natural and human systems by ingesting a deluge of Earth observation and social sensing data. The paper synthesizes current LDA knowledge and provides a steppingstone for its future development, particularly in promoting dual driven theory-data land processes studies.

数据同化在促进 "科学 "理解和充当地球系统科学的 "工程工具 "方面发挥着双重作用。陆地数据同化(LDA)已发展成为地球物理学中一门独特的学科,促进了理论和数据的协调统一,使陆地模型和观测数据能够相互补充和制约。近几十年来,LDA 在理论、方法和应用方面都取得了长足的进步,因此有必要对其进行全面深入的探讨。在此,我们将对 LDA 的理论和方法论发展及其显著特点进行全面综述。其中包括在解决地表过程中的强非线性、探索机器学习方法在数据同化中的潜力、量化多尺度空间相关性引起的不确定性以及同时估计模型状态和参数等方面的突破。事实证明,LDA 成功地增强了对各种地表过程(包括土壤水分、积雪、蒸散、溪流、地下水、灌溉和地表温度)的理解和预测,特别是在水循环和能量循环领域。本综述概述了全球、区域和流域尺度 LDA 系统和软件平台的发展情况,提出了生成陆地再分析和推进陆地-大气耦合 DA 的重大挑战。最后,我们强调了通过接收大量地球观测和社会感知数据,将 LDA 的应用从纯地球物理系统扩展到自然和人类耦合系统的机会。本文综述了当前的 LDA 知识,并为其未来发展,特别是在促进理论-数据双驱动的陆地过程研究方面,提供了一个基石。
{"title":"Land Data Assimilation: Harmonizing Theory and Data in Land Surface Process Studies","authors":"Xin Li,&nbsp;Feng Liu,&nbsp;Chunfeng Ma,&nbsp;Jinliang Hou,&nbsp;Donghai Zheng,&nbsp;Hanqing Ma,&nbsp;Yulong Bai,&nbsp;Xujun Han,&nbsp;Harry Vereecken,&nbsp;Kun Yang,&nbsp;Qingyun Duan,&nbsp;Chunlin Huang","doi":"10.1029/2022RG000801","DOIUrl":"https://doi.org/10.1029/2022RG000801","url":null,"abstract":"<p>Data assimilation plays a dual role in advancing the “scientific” understanding and serving as an “engineering tool” for the Earth system sciences. Land data assimilation (LDA) has evolved into a distinct discipline within geophysics, facilitating the harmonization of theory and data and allowing land models and observations to complement and constrain each other. Over recent decades, substantial progress has been made in the theory, methodology, and application of LDA, necessitating a holistic and in-depth exploration of its full spectrum. Here, we present a thorough review elucidating the theoretical and methodological developments in LDA and its distinctive features. This encompasses breakthroughs in addressing strong nonlinearities in land surface processes, exploring the potential of machine learning approaches in data assimilation, quantifying uncertainties arising from multiscale spatial correlation, and simultaneously estimating model states and parameters. LDA has proven successful in enhancing the understanding and prediction of various land surface processes (including soil moisture, snow, evapotranspiration, streamflow, groundwater, irrigation and land surface temperature), particularly within the realms of water and energy cycles. This review outlines the development of global, regional, and catchment-scale LDA systems and software platforms, proposing grand challenges of generating land reanalysis and advancing coupled land‒atmosphere DA. We lastly highlight the opportunities to expand the applications of LDA from pure geophysical systems to coupled natural and human systems by ingesting a deluge of Earth observation and social sensing data. The paper synthesizes current LDA knowledge and provides a steppingstone for its future development, particularly in promoting dual driven theory-data land processes studies.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"62 1","pages":""},"PeriodicalIF":25.2,"publicationDate":"2024-03-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2022RG000801","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140161345","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Lake Water Temperature Modeling in an Era of Climate Change: Data Sources, Models, and Future Prospects 气候变化时代的湖水温度建模:数据来源、模型和未来展望
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-02-11 DOI: 10.1029/2023RG000816
S. Piccolroaz, S. Zhu, R. Ladwig, L. Carrea, S. Oliver, A. P. Piotrowski, M. Ptak, R. Shinohara, M. Sojka, R. I. Woolway, D. Z. Zhu

Lake thermal dynamics have been considerably impacted by climate change, with potential adverse effects on aquatic ecosystems. To better understand the potential impacts of future climate change on lake thermal dynamics and related processes, the use of mathematical models is essential. In this study, we provide a comprehensive review of lake water temperature modeling. We begin by discussing the physical concepts that regulate thermal dynamics in lakes, which serve as a primer for the description of process-based models. We then provide an overview of different sources of observational water temperature data, including in situ monitoring and satellite Earth observations, used in the field of lake water temperature modeling. We classify and review the various lake water temperature models available, and then discuss model performance, including commonly used performance metrics and optimization methods. Finally, we analyze emerging modeling approaches, including forecasting, digital twins, combining process-based modeling with deep learning, evaluating structural model differences through ensemble modeling, adapted water management, and coupling of climate and lake models. This review is aimed at a diverse group of professionals working in the fields of limnology and hydrology, including ecologists, biologists, physicists, engineers, and remote sensing researchers from the private and public sectors who are interested in understanding lake water temperature modeling and its potential applications.

气候变化对湖泊热动力学产生了巨大影响,并可能对水生生态系统造成不利影响。为了更好地了解未来气候变化对湖泊热动态及相关过程的潜在影响,使用数学模型至关重要。在本研究中,我们对湖泊水温建模进行了全面回顾。我们首先讨论了调节湖泊热动力学的物理概念,作为描述基于过程的模型的入门读物。然后,我们概述了湖泊水温建模领域使用的不同水温观测数据来源,包括现场监测和卫星地球观测。我们对现有的各种湖泊水温模型进行了分类和评述,然后讨论了模型性能,包括常用的性能指标和优化方法。最后,我们分析了新出现的建模方法,包括预测、数字双胞胎、将基于过程的建模与深度学习相结合、通过集合建模评估结构模型差异、适应性水管理以及气候模型与湖泊模型的耦合。本综述面向湖泊学和水文学领域的各类专业人士,包括生态学家、生物学家、物理学家、工程师以及对了解湖泊水温建模及其潜在应用感兴趣的私营和公共部门的遥感研究人员。
{"title":"Lake Water Temperature Modeling in an Era of Climate Change: Data Sources, Models, and Future Prospects","authors":"S. Piccolroaz,&nbsp;S. Zhu,&nbsp;R. Ladwig,&nbsp;L. Carrea,&nbsp;S. Oliver,&nbsp;A. P. Piotrowski,&nbsp;M. Ptak,&nbsp;R. Shinohara,&nbsp;M. Sojka,&nbsp;R. I. Woolway,&nbsp;D. Z. Zhu","doi":"10.1029/2023RG000816","DOIUrl":"https://doi.org/10.1029/2023RG000816","url":null,"abstract":"<p>Lake thermal dynamics have been considerably impacted by climate change, with potential adverse effects on aquatic ecosystems. To better understand the potential impacts of future climate change on lake thermal dynamics and related processes, the use of mathematical models is essential. In this study, we provide a comprehensive review of lake water temperature modeling. We begin by discussing the physical concepts that regulate thermal dynamics in lakes, which serve as a primer for the description of process-based models. We then provide an overview of different sources of observational water temperature data, including in situ monitoring and satellite Earth observations, used in the field of lake water temperature modeling. We classify and review the various lake water temperature models available, and then discuss model performance, including commonly used performance metrics and optimization methods. Finally, we analyze emerging modeling approaches, including forecasting, digital twins, combining process-based modeling with deep learning, evaluating structural model differences through ensemble modeling, adapted water management, and coupling of climate and lake models. This review is aimed at a diverse group of professionals working in the fields of limnology and hydrology, including ecologists, biologists, physicists, engineers, and remote sensing researchers from the private and public sectors who are interested in understanding lake water temperature modeling and its potential applications.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"62 1","pages":""},"PeriodicalIF":25.2,"publicationDate":"2024-02-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2023RG000816","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139719928","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
River Damming Impacts on Fish Habitat and Associated Conservation Measures 河流大坝对鱼类栖息地的影响及相关保护措施
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-12-19 DOI: 10.1029/2023RG000819
Qiuwen Chen, Qinyuan Li, Yuqing Lin, Jianyun Zhang, Jun Xia, Jinren Ni, Steven J. Cooke, Jim Best, Shufeng He, Tao Feng, Yuchen Chen, Daniele Tonina, Rohan Benjankar, Sebastian Birk, Ayan Santos Fleischmann, Hanlu Yan, Lei Tang

River damming has brought great benefits to flood mitigation, energy and food production, and will continue to play a significant role in global energy supply, particularly in Asia, Africa, and South America. However, dams have extensively altered global river dynamics, including riverine connectivity, hydrological, thermal, sediment and solute regimes, and the channel morphology. These alterations have detrimental effects on the quality and quantity of fish habitat and associated impacts on aquatic life. Indeed, dams have been implicated in the decline of numerous fishes, emphasizing the need for effective conservation measures. Here, we present a global synthesis of critical issues concerning the impacts of river damming on physical fish habitats, with a particular focus on key fish species across continents. We also consider current fish conservation measures and their applicability in different contexts. Finally, we identify future research needs. The information presented herein will help support sustainable dam operation under the constraints of future climate change and human needs.

拦河筑坝为减轻洪灾、能源和粮食生产带来了巨大好处,并将继续在全球能源供应中发挥重要作用,尤其是在亚洲、非洲和南美洲。然而,大坝广泛地改变了全球河流的动态,包括河流的连通性、水文、热、沉积物和溶质系统以及河道形态。这些改变对鱼类栖息地的质量和数量产生了有害影响,并对水生生物产生了相关影响。事实上,水坝与许多鱼类的减少有牵连,因此需要采取有效的保护措施。在此,我们对河流筑坝对鱼类自然栖息地影响的关键问题进行了全球综述,并特别关注各大洲的主要鱼类物种。我们还考虑了当前的鱼类保护措施及其在不同情况下的适用性。最后,我们确定了未来的研究需求。本文介绍的信息将有助于在未来气候变化和人类需求的限制下支持大坝的可持续运行。
{"title":"River Damming Impacts on Fish Habitat and Associated Conservation Measures","authors":"Qiuwen Chen,&nbsp;Qinyuan Li,&nbsp;Yuqing Lin,&nbsp;Jianyun Zhang,&nbsp;Jun Xia,&nbsp;Jinren Ni,&nbsp;Steven J. Cooke,&nbsp;Jim Best,&nbsp;Shufeng He,&nbsp;Tao Feng,&nbsp;Yuchen Chen,&nbsp;Daniele Tonina,&nbsp;Rohan Benjankar,&nbsp;Sebastian Birk,&nbsp;Ayan Santos Fleischmann,&nbsp;Hanlu Yan,&nbsp;Lei Tang","doi":"10.1029/2023RG000819","DOIUrl":"https://doi.org/10.1029/2023RG000819","url":null,"abstract":"<p>River damming has brought great benefits to flood mitigation, energy and food production, and will continue to play a significant role in global energy supply, particularly in Asia, Africa, and South America. However, dams have extensively altered global river dynamics, including riverine connectivity, hydrological, thermal, sediment and solute regimes, and the channel morphology. These alterations have detrimental effects on the quality and quantity of fish habitat and associated impacts on aquatic life. Indeed, dams have been implicated in the decline of numerous fishes, emphasizing the need for effective conservation measures. Here, we present a global synthesis of critical issues concerning the impacts of river damming on physical fish habitats, with a particular focus on key fish species across continents. We also consider current fish conservation measures and their applicability in different contexts. Finally, we identify future research needs. The information presented herein will help support sustainable dam operation under the constraints of future climate change and human needs.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"61 4","pages":""},"PeriodicalIF":25.2,"publicationDate":"2023-12-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2023RG000819","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138739870","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Frontiers in Satellite-Based Estimates of Cloud-Mediated Aerosol Forcing 基于云介导的气溶胶强迫卫星估计的前沿
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-10-18 DOI: 10.1029/2022RG000799
Daniel Rosenfeld, Alexander Kokhanovsky, Tom Goren, Edward Gryspeerdt, Otto Hasekamp, Hailing Jia, Anton Lopatin, Johannes Quaas, Zengxin Pan, Odran Sourdeval

Atmospheric aerosols affect the Earth's climate in many ways, including acting as the seeds on which cloud droplets form. Since a large fraction of these particles is anthropogenic, the clouds' microphysical and radiative characteristics are influenced by human activity on a global scale leading to important climatic effects. The respective change in the energy budget at the top of the atmosphere is defined as the effective radiative forcing due to aerosol-cloud interaction (ERFaci). It is estimated that the ERFaci offsets presently nearly 1/4 of the greenhouse-induced warming, but the uncertainty is within a factor of two. A common method to calculate the ERFaci is by the multiplication of the susceptibility of the cloud radiative effect to changes in aerosols by the anthropogenic change of the aerosol concentration. This has to be done by integrating it over all cloud regimes. Here we review the various methods of the ERFaci estimation. Global measurements require satellites' global coverage. The challenge of quantifying aerosol amounts in cloudy atmospheres are met with the rapid development of novel methodologies reviewed here. The aerosol characteristics can be retrieved from space based on their optical properties, including polarization. The concentrations of the aerosols that serve as cloud drop condensation nuclei can be also estimated from their impact on the satellite-retrieved cloud drop number concentrations. These observations are critical for reducing the uncertainty in the ERFaci calculated from global climate models (GCMs), but further development is required to allow GCMs to properly simulate and benefit these novel observables.

大气气溶胶以多种方式影响地球气候,包括作为云滴形成的种子。由于这些粒子的很大一部分是人为的,云的微物理和辐射特征在全球范围内受到人类活动的影响,导致重要的气候效应。大气顶部能量收支的相应变化被定义为气溶胶-云相互作用(ERFaci)引起的有效辐射强迫。据估计,ERFaci目前抵消了近四分之一的温室气体引起的变暖,但不确定性在两个因素之内。计算ERFaci的一种常用方法是将云辐射效应对气溶胶变化的敏感性乘以气溶胶浓度的人为变化。这必须通过在所有云系统中集成它来完成。在这里,我们回顾了ERFaci估计的各种方法。全球测量需要卫星的全球覆盖。在多云大气中定量气溶胶量的挑战遇到了新方法的快速发展。基于气溶胶的光学特性,包括偏振,可以从太空中获取气溶胶的特征。作为云滴凝结核的气溶胶的浓度也可以通过它们对卫星检索的云滴数浓度的影响来估计。这些观测值对于减少由全球气候模式(gcm)计算的ERFaci的不确定性至关重要,但需要进一步发展,使gcm能够正确模拟并受益于这些新的观测值。
{"title":"Frontiers in Satellite-Based Estimates of Cloud-Mediated Aerosol Forcing","authors":"Daniel Rosenfeld,&nbsp;Alexander Kokhanovsky,&nbsp;Tom Goren,&nbsp;Edward Gryspeerdt,&nbsp;Otto Hasekamp,&nbsp;Hailing Jia,&nbsp;Anton Lopatin,&nbsp;Johannes Quaas,&nbsp;Zengxin Pan,&nbsp;Odran Sourdeval","doi":"10.1029/2022RG000799","DOIUrl":"10.1029/2022RG000799","url":null,"abstract":"<p>Atmospheric aerosols affect the Earth's climate in many ways, including acting as the seeds on which cloud droplets form. Since a large fraction of these particles is anthropogenic, the clouds' microphysical and radiative characteristics are influenced by human activity on a global scale leading to important climatic effects. The respective change in the energy budget at the top of the atmosphere is defined as the effective radiative forcing due to aerosol-cloud interaction (ERF<sub>aci</sub>). It is estimated that the ERF<sub>aci</sub> offsets presently nearly 1/4 of the greenhouse-induced warming, but the uncertainty is within a factor of two. A common method to calculate the ERF<sub>aci</sub> is by the multiplication of the susceptibility of the cloud radiative effect to changes in aerosols by the anthropogenic change of the aerosol concentration. This has to be done by integrating it over all cloud regimes. Here we review the various methods of the ERF<sub>aci</sub> estimation. Global measurements require satellites' global coverage. The challenge of quantifying aerosol amounts in cloudy atmospheres are met with the rapid development of novel methodologies reviewed here. The aerosol characteristics can be retrieved from space based on their optical properties, including polarization. The concentrations of the aerosols that serve as cloud drop condensation nuclei can be also estimated from their impact on the satellite-retrieved cloud drop number concentrations. These observations are critical for reducing the uncertainty in the ERF<sub>aci</sub> calculated from global climate models (GCMs), but further development is required to allow GCMs to properly simulate and benefit these novel observables.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"61 4","pages":""},"PeriodicalIF":25.2,"publicationDate":"2023-10-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135884108","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: 1
The Historical Development of Large-Scale Paleoclimate Field Reconstructions Over the Common Era 大尺度古气候场重建的历史进展
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-09-20 DOI: 10.1029/2022RG000782
Jason E. Smerdon, Edward R. Cook, Nathan J. Steiger

Climate field reconstructions (CFRs) combine modern observational data with paleoclimatic proxies to estimate climate variables over spatiotemporal grids during time periods when widespread observations of climatic conditions do not exist. The Common Era (CE) has been a period over which many seasonally- and annually-resolved CFRs have been produced on regional to global scales. CFRs over the CE were first produced in the 1970s using dendroclimatic records and linear regression-based approaches. Since that time, many new CFRs have been produced using a wide range of proxy data sets and reconstruction techniques. We assess the early history of research on CFRs for the CE, which provides context for our review of advances in CFR research over the last two decades. We review efforts to derive gridded hydroclimatic CFRs over continental regions using networks of tree-ring proxies. We subsequently explore work to produce hemispheric- and global-scale CFRs of surface temperature using multi-proxy data sets, before specifically reviewing recently-developed data assimilation techniques and how they have been used to produce simultaneous reconstructions of multiple climatic fields globally. We then review efforts to develop standardized and digitized databases of proxy networks for use in CFR research, before concluding with some thoughts on important next steps for CFR development.

气候场重建(CFRs)将现代观测数据与古气候代用物相结合,在没有广泛气候条件观测的时间段内估算时空网格上的气候变量。共同年代(CE)是在区域到全球范围内产生许多季节性和年度解决cfr的时期。在20世纪70年代,利用树木气候记录和基于线性回归的方法首次产生了欧洲东部的cfr。从那时起,使用各种代理数据集和重建技术产生了许多新的cfr。我们评估了CE对CFR研究的早期历史,这为我们回顾过去二十年来CFR研究的进展提供了背景。我们回顾了利用树木年轮代用物网络推导大陆地区网格化水文气候CFRs的工作。随后,我们探索了使用多代理数据集生成半球和全球尺度表面温度CFRs的工作,然后专门回顾了最近开发的数据同化技术,以及它们如何用于同时重建全球多个气候场。然后,我们回顾了开发用于CFR研究的标准化和数字化代理网络数据库的努力,最后对CFR发展的下一步重要步骤进行了一些思考。
{"title":"The Historical Development of Large-Scale Paleoclimate Field Reconstructions Over the Common Era","authors":"Jason E. Smerdon,&nbsp;Edward R. Cook,&nbsp;Nathan J. Steiger","doi":"10.1029/2022RG000782","DOIUrl":"10.1029/2022RG000782","url":null,"abstract":"<p>Climate field reconstructions (CFRs) combine modern observational data with paleoclimatic proxies to estimate climate variables over spatiotemporal grids during time periods when widespread observations of climatic conditions do not exist. The Common Era (CE) has been a period over which many seasonally- and annually-resolved CFRs have been produced on regional to global scales. CFRs over the CE were first produced in the 1970s using dendroclimatic records and linear regression-based approaches. Since that time, many new CFRs have been produced using a wide range of proxy data sets and reconstruction techniques. We assess the early history of research on CFRs for the CE, which provides context for our review of advances in CFR research over the last two decades. We review efforts to derive gridded hydroclimatic CFRs over continental regions using networks of tree-ring proxies. We subsequently explore work to produce hemispheric- and global-scale CFRs of surface temperature using multi-proxy data sets, before specifically reviewing recently-developed data assimilation techniques and how they have been used to produce simultaneous reconstructions of multiple climatic fields globally. We then review efforts to develop standardized and digitized databases of proxy networks for use in CFR research, before concluding with some thoughts on important next steps for CFR development.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"61 4","pages":""},"PeriodicalIF":25.2,"publicationDate":"2023-09-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2022RG000782","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135648622","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Geomorphic Process Chains in High-Mountain Regions—A Review and Classification Approach for Natural Hazards Assessment 高山区地貌过程链——自然灾害评价与分类方法综述
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-09-13 DOI: 10.1029/2022RG000791
Peter Mani, Simon Allen, Stephen G. Evans, Jeffrey S. Kargel, Martin Mergili, Dmitry Petrakov, Markus Stoffel

Populations and infrastructure in high mountain regions are exposed to a wide range of natural hazards, the frequency, magnitude, and location of which are extremely sensitive to climate change. In cases where several hazards can occur simultaneously or where the occurrence of one event will change the disposition of another, assessments need to account for complex process chains. While process chains are widely recognized as a major threat, no systematic analysis has hitherto been undertaken. We therefore establish new understanding on the factors that directly trigger or alter the disposition for subsequent events in the chain and derive a novel classification scheme and parameters to aid natural hazard assessment. Process chains in high mountains are commonly associated with glacier retreat or permafrost degradation. Regional differences exist in the nature and rate of sequencing—some process chains are almost instantaneous, while other linkages are delayed. Process chains involving rapid sequences are difficult to predict, and impacts are often devastating. We demonstrate that process chains are triggered most frequently by progressive failures, being the result of gradual landscape weakening and not due to the occurrence of a distinct process. If fluvial processes are part of the process chain the reach (or mobility) of process chains is increased. Increased mobility can also occur if sediment deposition areas along river channels are activated. As climate changes causes glacial environments to transform into sediment-rich paraglacial and fluvial landscapes, it is expected that the mobility of process chains will increase in the future.

高山地区的人口和基础设施面临各种自然灾害,其频率、规模和地点对气候变化极为敏感。在几种危害可能同时发生或一个事件的发生将改变另一个事件的处置的情况下,评估需要考虑复杂的过程链。虽然流程链被广泛认为是一个主要威胁,但迄今为止还没有进行系统的分析。因此,我们建立了对直接触发或改变链中后续事件处置的因素的新理解,并得出了一种新的分类方案和参数来帮助自然灾害评估。高山过程链通常与冰川退缩或永久冻土退化有关。区域差异存在于排序的性质和速度上——一些过程链几乎是瞬时的,而另一些则是延迟的。涉及快速序列的工艺链很难预测,其影响往往是毁灭性的。我们证明了过程链最常被渐进的失败所触发,这是逐渐的景观弱化的结果,而不是由于一个独特过程的发生。如果河流过程是过程链的一部分,则过程链的范围(或流动性)增加。如果河道沿岸的沉积物沉积区被激活,流动性也会增加。由于气候变化导致冰川环境转变为富含沉积物的副冰川和河流景观,预计未来过程链的流动性将增加。
{"title":"Geomorphic Process Chains in High-Mountain Regions—A Review and Classification Approach for Natural Hazards Assessment","authors":"Peter Mani,&nbsp;Simon Allen,&nbsp;Stephen G. Evans,&nbsp;Jeffrey S. Kargel,&nbsp;Martin Mergili,&nbsp;Dmitry Petrakov,&nbsp;Markus Stoffel","doi":"10.1029/2022RG000791","DOIUrl":"10.1029/2022RG000791","url":null,"abstract":"<p>Populations and infrastructure in high mountain regions are exposed to a wide range of natural hazards, the frequency, magnitude, and location of which are extremely sensitive to climate change. In cases where several hazards can occur simultaneously or where the occurrence of one event will change the disposition of another, assessments need to account for complex process chains. While process chains are widely recognized as a major threat, no systematic analysis has hitherto been undertaken. We therefore establish new understanding on the factors that directly trigger or alter the disposition for subsequent events in the chain and derive a novel classification scheme and parameters to aid natural hazard assessment. Process chains in high mountains are commonly associated with glacier retreat or permafrost degradation. Regional differences exist in the nature and rate of sequencing—some process chains are almost instantaneous, while other linkages are delayed. Process chains involving rapid sequences are difficult to predict, and impacts are often devastating. We demonstrate that process chains are triggered most frequently by progressive failures, being the result of gradual landscape weakening and not due to the occurrence of a distinct process. If fluvial processes are part of the process chain the reach (or mobility) of process chains is increased. Increased mobility can also occur if sediment deposition areas along river channels are activated. As climate changes causes glacial environments to transform into sediment-rich paraglacial and fluvial landscapes, it is expected that the mobility of process chains will increase in the future.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"61 4","pages":""},"PeriodicalIF":25.2,"publicationDate":"2023-09-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2022RG000791","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136272246","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Antarctic Sedimentary Basins and Their Influence on Ice-Sheet Dynamics 南极沉积盆地及其对冰盖动力学的影响
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-08-23 DOI: 10.1029/2021RG000767
A. R. A. Aitken, L. Li, B. Kulessa, D. Schroeder, T. A. Jordan, J. M. Whittaker, S. Anandakrishnan, E. J. Dawson, D. A. Wiens, O. Eisen, M. J. Siegert

Knowledge of Antarctica's sedimentary basins builds our understanding of the coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties distinct from basement-dominated regions that impact ice-sheet dynamics, potentially influencing future ice-sheet change. Despite their importance, our knowledge of Antarctic sedimentary basins is restricted. Remoteness, the harsh environment, the overlying ice sheet, ice shelves, and sea ice all make fieldwork challenging. Nonetheless, in the past decade the geophysics community has made great progress in internationally coordinated data collection and compilation with parallel advances in data processing and analysis supporting a new insight into Antarctica's subglacial environment. Here, we summarize recent progress in understanding Antarctica's sedimentary basins. We review advances in the technical capability of radar, potential fields, seismic, and electromagnetic techniques to detect and characterize basins beneath ice and advances in integrated multi-data interpretation including machine-learning approaches. These new capabilities permit a continent-wide mapping of Antarctica's sedimentary basins and their characteristics, aiding definition of the tectonic development of the continent. Crucially, Antarctica's sedimentary basins interact with the overlying ice sheet through dynamic feedbacks that have the potential to contribute to rapid ice-sheet change. Looking ahead, future research directions include techniques to increase data coverage within logistical constraints, and resolving major knowledge gaps, including insufficient sampling of the ice-sheet bed and poor definition of subglacial basin structure and stratigraphy. Translating the knowledge of sedimentary basin processes into ice-sheet modeling studies is critical to underpin better capacity to predict future change.

对南极洲沉积盆地的了解有助于我们理解构造、冰、海洋和气候的耦合演化。沉积盆地具有不同于以基底为主的区域的特性,影响冰盖动力学,可能影响未来的冰盖变化。尽管它们很重要,但我们对南极沉积盆地的了解还是有限的。偏远、恶劣的环境、覆盖的冰盖、冰架和海冰都使野外工作具有挑战性。尽管如此,在过去十年中,地球物理学界在国际协调的数据收集和汇编方面取得了巨大进展,在数据处理和分析方面也取得了平行进展,支持对南极洲冰下环境的新认识。在这里,我们总结了近年来在了解南极洲沉积盆地方面的进展。我们回顾了雷达、势场、地震和电磁技术在探测和表征冰下盆地的技术能力方面的进展,以及包括机器学习方法在内的综合多数据解释的进展。这些新功能允许对南极洲的沉积盆地及其特征进行全大陆范围的测绘,有助于确定该大陆的构造发展。至关重要的是,南极洲的沉积盆地通过动态反馈与上覆冰盖相互作用,有可能导致冰盖快速变化。展望未来,未来的研究方向包括在后勤限制下增加数据覆盖的技术,以及解决主要的知识空白,包括对冰盖床的采样不足和对冰下盆地结构和地层学的不明确定义。将沉积盆地过程的知识转化为冰盖模型研究对于增强预测未来变化的能力至关重要。
{"title":"Antarctic Sedimentary Basins and Their Influence on Ice-Sheet Dynamics","authors":"A. R. A. Aitken,&nbsp;L. Li,&nbsp;B. Kulessa,&nbsp;D. Schroeder,&nbsp;T. A. Jordan,&nbsp;J. M. Whittaker,&nbsp;S. Anandakrishnan,&nbsp;E. J. Dawson,&nbsp;D. A. Wiens,&nbsp;O. Eisen,&nbsp;M. J. Siegert","doi":"10.1029/2021RG000767","DOIUrl":"10.1029/2021RG000767","url":null,"abstract":"<p>Knowledge of Antarctica's sedimentary basins builds our understanding of the coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties distinct from basement-dominated regions that impact ice-sheet dynamics, potentially influencing future ice-sheet change. Despite their importance, our knowledge of Antarctic sedimentary basins is restricted. Remoteness, the harsh environment, the overlying ice sheet, ice shelves, and sea ice all make fieldwork challenging. Nonetheless, in the past decade the geophysics community has made great progress in internationally coordinated data collection and compilation with parallel advances in data processing and analysis supporting a new insight into Antarctica's subglacial environment. Here, we summarize recent progress in understanding Antarctica's sedimentary basins. We review advances in the technical capability of radar, potential fields, seismic, and electromagnetic techniques to detect and characterize basins beneath ice and advances in integrated multi-data interpretation including machine-learning approaches. These new capabilities permit a continent-wide mapping of Antarctica's sedimentary basins and their characteristics, aiding definition of the tectonic development of the continent. Crucially, Antarctica's sedimentary basins interact with the overlying ice sheet through dynamic feedbacks that have the potential to contribute to rapid ice-sheet change. Looking ahead, future research directions include techniques to increase data coverage within logistical constraints, and resolving major knowledge gaps, including insufficient sampling of the ice-sheet bed and poor definition of subglacial basin structure and stratigraphy. Translating the knowledge of sedimentary basin processes into ice-sheet modeling studies is critical to underpin better capacity to predict future change.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"61 3","pages":""},"PeriodicalIF":25.2,"publicationDate":"2023-08-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2021RG000767","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"80517164","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Global Climate Impacts of Land-Surface and Atmospheric Processes Over the Tibetan Plateau 青藏高原陆面和大气过程对全球气候的影响
IF 25.2 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2023-08-09 DOI: 10.1029/2022RG000771
Jianping Huang, Xiuji Zhou, Guoxiong Wu, Xiangde Xu, Qingyun Zhao, Yimin Liu, Anmin Duan, Yongkun Xie, Yaoming Ma, Ping Zhao, Song Yang, Kun Yang, Haijun Yang, Jianchun Bian, Yunfei Fu, Jinming Ge, Yuzhi Liu, Qigang Wu, Haipeng Yu, Binbin Wang, Qing Bao, Kai Qie

The Tibetan Plateau (TP) impacts local and remote atmospheric circulations, wherein it mechanically and thermally affects air masses or airflows. Moreover, the TP provides a key channel for substance transport between the troposphere and the stratosphere. This study reviews recent advances in research regarding land–atmosphere coupling processes over the TP. The TP experiences climate warming and wetting. Climate warming has caused glacier retreat, permafrost degradation, and a general increase in vegetation density, while climate wetting has led to a significant increase in the number of major lakes, primarily through increased precipitation. Local and regional climates are affected by interactions between the land and the atmosphere. Namely, the TP drives surface pollutants to the upper troposphere in an Asian summer monsoon (ASM) anticyclone circulation, before spreading to the lower stratosphere. Further, the thermal forcing of the TP plays an essential role in the ASM. TP forcing can modulate hemispheric-scale atmospheric circulations across all seasons. The TP interacts with remote oceans through a forced atmospheric response and is substantially affected by the evolution of the Earth's climate via promoting Atlantic meridional overturning circulation and eliminating Pacific meridional overturning circulation. The extensive influence of the TP is facilitated by its coupling with the ASM in the summer; whereas its winter influence on climate mainly occurs through Rossby waves. The observed increasing trends of temperature and precipitation over the TP are projected to continue throughout the 21st century.

青藏高原(TP)影响局地和远地大气环流,其中它对气团或气流产生机械和热力影响。此外,TP为对流层和平流层之间的物质输送提供了一个关键通道。本文综述了青藏高原陆地-大气耦合过程的最新研究进展。青藏高原经历了气候变暖和湿润。气候变暖导致冰川退缩、永久冻土退化和植被密度普遍增加,而气候变湿主要通过降水增加导致主要湖泊数量显著增加。局部和区域气候受到陆地和大气之间相互作用的影响。也就是说,在亚洲夏季风(ASM)反气旋环流中,TP驱动地表污染物到对流层上层,然后扩散到平流层下层。此外,高原的热强迫对高原的形成起着重要的作用。总温强迫可以调节所有季节的半球尺度大气环流。青藏高原通过强迫大气响应与遥远的海洋相互作用,并通过促进大西洋经向翻转环流和消除太平洋经向翻转环流而受到地球气候演变的实质性影响。夏季青藏高原与夏季高原的耦合促进了青藏高原的广泛影响;而冬季对气候的影响主要通过罗斯比波发生。观测到的青藏高原温度和降水的增加趋势预计将持续整个21世纪。
{"title":"Global Climate Impacts of Land-Surface and Atmospheric Processes Over the Tibetan Plateau","authors":"Jianping Huang,&nbsp;Xiuji Zhou,&nbsp;Guoxiong Wu,&nbsp;Xiangde Xu,&nbsp;Qingyun Zhao,&nbsp;Yimin Liu,&nbsp;Anmin Duan,&nbsp;Yongkun Xie,&nbsp;Yaoming Ma,&nbsp;Ping Zhao,&nbsp;Song Yang,&nbsp;Kun Yang,&nbsp;Haijun Yang,&nbsp;Jianchun Bian,&nbsp;Yunfei Fu,&nbsp;Jinming Ge,&nbsp;Yuzhi Liu,&nbsp;Qigang Wu,&nbsp;Haipeng Yu,&nbsp;Binbin Wang,&nbsp;Qing Bao,&nbsp;Kai Qie","doi":"10.1029/2022RG000771","DOIUrl":"10.1029/2022RG000771","url":null,"abstract":"<p>The Tibetan Plateau (TP) impacts local and remote atmospheric circulations, wherein it mechanically and thermally affects air masses or airflows. Moreover, the TP provides a key channel for substance transport between the troposphere and the stratosphere. This study reviews recent advances in research regarding land–atmosphere coupling processes over the TP. The TP experiences climate warming and wetting. Climate warming has caused glacier retreat, permafrost degradation, and a general increase in vegetation density, while climate wetting has led to a significant increase in the number of major lakes, primarily through increased precipitation. Local and regional climates are affected by interactions between the land and the atmosphere. Namely, the TP drives surface pollutants to the upper troposphere in an Asian summer monsoon (ASM) anticyclone circulation, before spreading to the lower stratosphere. Further, the thermal forcing of the TP plays an essential role in the ASM. TP forcing can modulate hemispheric-scale atmospheric circulations across all seasons. The TP interacts with remote oceans through a forced atmospheric response and is substantially affected by the evolution of the Earth's climate via promoting Atlantic meridional overturning circulation and eliminating Pacific meridional overturning circulation. The extensive influence of the TP is facilitated by its coupling with the ASM in the summer; whereas its winter influence on climate mainly occurs through Rossby waves. The observed increasing trends of temperature and precipitation over the TP are projected to continue throughout the 21st century.</p>","PeriodicalId":21177,"journal":{"name":"Reviews of Geophysics","volume":"61 3","pages":""},"PeriodicalIF":25.2,"publicationDate":"2023-08-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"82218601","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: 4
期刊
Reviews of Geophysics
全部 Acc. Chem. Res. ACS Applied Bio Materials ACS Appl. Electron. Mater. ACS Appl. Energy Mater. ACS Appl. Mater. Interfaces ACS Appl. Nano Mater. ACS Appl. Polym. Mater. ACS BIOMATER-SCI ENG ACS Catal. ACS Cent. Sci. ACS Chem. Biol. ACS Chemical Health & Safety ACS Chem. Neurosci. ACS Comb. Sci. ACS Earth Space Chem. ACS Energy Lett. ACS Infect. Dis. ACS Macro Lett. ACS Mater. Lett. ACS Med. Chem. Lett. ACS Nano ACS Omega ACS Photonics ACS Sens. ACS Sustainable Chem. Eng. ACS Synth. Biol. Anal. Chem. BIOCHEMISTRY-US Bioconjugate Chem. BIOMACROMOLECULES Chem. Res. Toxicol. Chem. Rev. Chem. Mater. CRYST GROWTH DES ENERG FUEL Environ. Sci. Technol. Environ. Sci. Technol. Lett. Eur. J. Inorg. Chem. IND ENG CHEM RES Inorg. Chem. J. Agric. Food. Chem. J. Chem. Eng. Data J. Chem. Educ. J. Chem. Inf. Model. J. Chem. Theory Comput. J. Med. Chem. J. Nat. Prod. J PROTEOME RES J. Am. Chem. Soc. LANGMUIR MACROMOLECULES Mol. Pharmaceutics Nano Lett. Org. Lett. ORG PROCESS RES DEV ORGANOMETALLICS J. Org. Chem. J. Phys. Chem. J. Phys. Chem. A J. Phys. Chem. B J. Phys. Chem. C J. Phys. Chem. Lett. Analyst Anal. Methods Biomater. Sci. Catal. Sci. Technol. Chem. Commun. Chem. Soc. Rev. CHEM EDUC RES PRACT CRYSTENGCOMM Dalton Trans. Energy Environ. Sci. ENVIRON SCI-NANO ENVIRON SCI-PROC IMP ENVIRON SCI-WAT RES Faraday Discuss. Food Funct. Green Chem. Inorg. Chem. Front. Integr. Biol. J. Anal. At. Spectrom. J. Mater. Chem. A J. Mater. Chem. B J. Mater. Chem. C Lab Chip Mater. Chem. Front. Mater. Horiz. MEDCHEMCOMM Metallomics Mol. Biosyst. Mol. Syst. Des. Eng. Nanoscale Nanoscale Horiz. Nat. Prod. Rep. New J. Chem. Org. Biomol. Chem. Org. Chem. Front. PHOTOCH PHOTOBIO SCI PCCP Polym. Chem.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1