npj Climate and Atmospheric Science最新文献

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Spatially inhomogeneous response of precipitation δ18O in China to ENSO cycles 中国降水δ18O对ENSO循环的空间非均匀响应
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-05-02 DOI: 10.1038/s41612-025-01057-1
Yushuang Cui, Lide Tian, Zhongyin Cai, Shangjie Wang
{"title":"Spatially inhomogeneous response of precipitation δ18O in China to ENSO cycles","authors":"Yushuang Cui, Lide Tian, Zhongyin Cai, Shangjie Wang","doi":"10.1038/s41612-025-01057-1","DOIUrl":"https://doi.org/10.1038/s41612-025-01057-1","url":null,"abstract":"<p>Water stable isotopes serve as essential natural tracers, offering broad applications in water cycle, atmosphere science and paleoclimate rebuilding. In this study, we created a precipitation stable isotope dataset for 1961–2022 by developing a fusion machine learning model, and mapped the time-series precipitation isoscape (δ<sup>18</sup>O) across the mainland of China over the past 62 years. This dataset allows for a further discussion on spatially different behavior of precipitation δ<sup>18</sup>O to the strong ENSO events, and we found that δ<sup>18</sup>O values are higher in El Niño years and lower in La Niña years in the southern of the line roughly from 30°N 80°E to 40°N 120°E, not fully consistent with the northern region. We also revealed an increasing trend in precipitation δ<sup>18</sup>O in the Western arid region and Eastern monsoon region in the past decades, while no significant trend on the Tibetan Plateau. These findings enhance our understanding of the climatic control mechanisms influencing precipitation isotopes and benefit paleoclimate rebuilding.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"1 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-05-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143901288","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
Compound marine heatwaves and tropical cyclones delay the onset of the Bay of Bengal summer monsoon 复合海洋热浪和热带气旋延迟了孟加拉湾夏季风的发生
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-05-01 DOI: 10.1038/s41612-025-01061-5
Xiong Zhou, Kang Xu, Karumuri Ashok, Jian Shi, Lei Zhang, Jin-Yi Yu, Boqi Liu, Chi-Yung Tam, Hongzhou Xu, Weiqiang Wang
{"title":"Compound marine heatwaves and tropical cyclones delay the onset of the Bay of Bengal summer monsoon","authors":"Xiong Zhou, Kang Xu, Karumuri Ashok, Jian Shi, Lei Zhang, Jin-Yi Yu, Boqi Liu, Chi-Yung Tam, Hongzhou Xu, Weiqiang Wang","doi":"10.1038/s41612-025-01061-5","DOIUrl":"https://doi.org/10.1038/s41612-025-01061-5","url":null,"abstract":"<p>Marine heatwaves (MHWs) and tropical cyclones (TCs) are prominent extreme events in the Bay of Bengal (BoB), whose co-occurrence can amplify their impacts. This study explores the mechanisms behind compound MHW-TC events and their influence on the onset of the BoB summer monsoon (BoBSM). Our findings indicate that compound MHW-TC events initiate with increased downward shortwave radiation and Ekman downwelling during MHW formation, followed by latent heat flux release and Ekman upwelling during the TC lifecycle. The interaction between increased maximum potential intensity and steering flow during compound events results in a westward shift in TC tracks, delaying precipitation and atmospheric latent heat release in the eastern BoB. These factors, as well as the warmer sea surface temperatures in the BoB, hinder the reversal of the mid-to-upper tropospheric meridional temperature gradient, ultimately postponing BoBSM onset. These insights enhance the understanding of MHW-TC interactions and their implications for predicting BoBSM onset.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"49 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143893789","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
Recent weakening of carbon-water coupling in northern ecosystems 近期北方生态系统碳-水耦合减弱
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-30 DOI: 10.1038/s41612-025-01059-z
Fubo Zhao, Wenbo Shi, Jingfeng Xiao, Meng Zhao, Xing Li, Yiping Wu
{"title":"Recent weakening of carbon-water coupling in northern ecosystems","authors":"Fubo Zhao, Wenbo Shi, Jingfeng Xiao, Meng Zhao, Xing Li, Yiping Wu","doi":"10.1038/s41612-025-01059-z","DOIUrl":"https://doi.org/10.1038/s41612-025-01059-z","url":null,"abstract":"<p>The terrestrial carbon and water cycles are deeply intertwined, and their coupling is critical to shaping ecosystem processes and land-atmosphere feedback. Understanding how the carbon-water coupling (CWC) changes, which remains rarely explored, is essential for predicting eco-hydrological responses to climate change. Here, using data from eddy covariance towers and remote sensing, we demonstrate a substantial decline in the CWC strength—measured as the correlation between gross primary production and evapotranspiration—across northern ecosystems over the past two decades. This weakening is primarily driven by rising CO₂ levels, with temperature, solar radiation, and precipitation playing secondary roles. Land surface models in the TRENDY project fail to capture this weakening synchronization, primarily due to their inadequate representation of the effects of elevated atmospheric CO<sub>2</sub> levels. The weakening of this synchronous variation between water and carbon may signify that the ecosystems are reshaping their eco-hydrological balances across the Northern Hemisphere.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"17 3 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143889677","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
A low-dimensional recursive deep learning model for El Niño-Southern Oscillation simulation El Niño-Southern振荡模拟的低维递归深度学习模型
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-27 DOI: 10.1038/s41612-025-01053-5
Jiho Ko, Na-Yeon Shin, Jonghun Kam, Yoo-Geun Ham, Jong-Seong Kug
{"title":"A low-dimensional recursive deep learning model for El Niño-Southern Oscillation simulation","authors":"Jiho Ko, Na-Yeon Shin, Jonghun Kam, Yoo-Geun Ham, Jong-Seong Kug","doi":"10.1038/s41612-025-01053-5","DOIUrl":"https://doi.org/10.1038/s41612-025-01053-5","url":null,"abstract":"<p>In this study, we develop a low-dimensional recursive model using deep learning (DL) to understand the dynamics of the El Niño-Southern Oscillation (ENSO). Unlike most existing research that relies on Coupled General Circulation Models (CGCMs), we explore a DL technique as an alternative approach to simulate ENSO characteristics. To replicate the observed stochastically excited oscillations, we incorporate stochastic noise into the recursive process of the DL model. Our long-term simulations demonstrate that the DL model effectively reproduces ENSO characteristics comparable to those captured by CGCMs. Additionally, we conduct experiments to analyze the interactions between ENSO and the Indian and Atlantic Oceans, evaluating their impacts on ENSO dynamics. Beyond capturing ENSO characteristics, the DL model exhibits skillful ENSO prediction capabilities. Using eXplainable AI (XAI) methods, we identify the contributions of each variable to ENSO predictability. Our findings suggest that this DL model serves as a valuable tool for understanding climate dynamics at a relatively low computational cost, providing an alternative to complex physically-based models.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"16 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143877857","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
Summer 2024 in northern Fennoscandia was very likely the warmest in 2000 years 芬诺斯坎迪亚北部2024年的夏天很可能是2000年来最温暖的
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-26 DOI: 10.1038/s41612-025-01046-4
Mika Rantanen, Samuli Helama, Jouni Räisänen, Hilppa Gregow
{"title":"Summer 2024 in northern Fennoscandia was very likely the warmest in 2000 years","authors":"Mika Rantanen, Samuli Helama, Jouni Räisänen, Hilppa Gregow","doi":"10.1038/s41612-025-01046-4","DOIUrl":"https://doi.org/10.1038/s41612-025-01046-4","url":null,"abstract":"<p>Summer 2024 was exceptionally warm in northern Fennoscandia, with June-August mean temperatures at several long-term weather stations surpassing the long-standing record set in 1937. In this region, summer mean temperatures have been reconstructed from tree-ring proxies, which provide annually resolved and millennium-long records of past climate. Here we show, using in-situ observations and two different tree-ring reconstructions, that summer 2024 was the warmest summer in 2000 years in northern Fennoscandia. Employing an attribution method based on Coupled Model Intercomparison Project Phase 6 climate models, we further estimate that climate change increased the likelihood of this extreme season by a factor of 93 (5–95% uncertainty range 19–881) and increased the temperature an additional 2.1 °C (1.4–2.8 °C). Atmospheric circulation patterns influencing both summers 1937 and 2024 were largely similar, suggesting a comparable large-scale circulation influence. Our findings highlight the impact of climate change for the contemporary heat extremes in Fennoscandia, indicating that the warming of summer climate is emerging from its range of natural climate variability over the last two millennia.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"34 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143877903","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
Disentangling anthropogenic and dynamic contributions to recent ocean warming 解开人为和动力因素对近期海洋变暖的影响
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-26 DOI: 10.1038/s41612-025-01043-7
Jiheun Lee, Rémi Tailleux, Till Kuhlbrodt
{"title":"Disentangling anthropogenic and dynamic contributions to recent ocean warming","authors":"Jiheun Lee, Rémi Tailleux, Till Kuhlbrodt","doi":"10.1038/s41612-025-01043-7","DOIUrl":"https://doi.org/10.1038/s41612-025-01043-7","url":null,"abstract":"<p>As the ocean absorbs over 90% of excess radiative heat, recent ocean warming is shaped by a combination of anthropogenic surface heat gain and dynamical processes redistributing heat. To distinguish these contributions, we introduce a novel framework that decomposes temperature changes into three components: ‘spice’ (density-compensated variability) and ‘heave’ (density-contributing variability), with heave further divided into ‘passive’ (net warming) and ‘dynamic’ (redistribution) contributions. Passive heave captures anthropogenic warming subducted along isopycnals, while spice and dynamic heave, which globally sum to zero, represent heat redistribution. Observations and climate models demonstrate general agreement on passive heave, establishing it as a key oceanic fingerprint of anthropogenic climate change. In contrast, dynamic heave, driven by interannual-to-decadal variability, exhibits significant spatial heterogeneity, with notable discrepancies between models and observations. This framework links ocean heat uptake to sea-level change, with passive heave driving global thermosteric rise and dynamic heave contributing to regional dynamic sea level changes.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"6 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143877858","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
FuXi-DA: a generalized deep learning data assimilation framework for assimilating satellite observations FuXi-DA:用于同化卫星观测数据的广义深度学习数据同化框架
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-26 DOI: 10.1038/s41612-025-01039-3
Xiaoze Xu, Xiuyu Sun, Wei Han, Xiaohui Zhong, Lei Chen, Zhiqiu Gao, Hao Li
{"title":"FuXi-DA: a generalized deep learning data assimilation framework for assimilating satellite observations","authors":"Xiaoze Xu, Xiuyu Sun, Wei Han, Xiaohui Zhong, Lei Chen, Zhiqiu Gao, Hao Li","doi":"10.1038/s41612-025-01039-3","DOIUrl":"https://doi.org/10.1038/s41612-025-01039-3","url":null,"abstract":"<p>Data assimilation (DA), as an indispensable component within contemporary Numerical Weather Prediction (NWP) systems, plays a crucial role in generating the analysis that significantly impacts forecast performance. Nevertheless, developing an efficient DA system poses significant challenges, particularly in establishing intricate relationships between the background field and the vast amount of multi-source observation data within limited operational time windows. Recently, Deep learning-based (DL-based) weather forecast models have shown promise in matching, even surpassing, the leading operational NWP models worldwide. This success motivates the exploration of establishing DL-based DA frameworks. DL models possess multi-modal modeling capabilities, enabling the fusion of multi-source data in the feature space, which is very similar to the process of assimilating multi-source observational data in DA systems. In this study, we introduce FuXi-DA, a generalized DL-based DA framework for assimilating satellite observations. By assimilating data from Advanced Geosynchronous Radiation Imager aboard Fengyun-4B, FuXi-DA consistently mitigates analysis errors and significantly improves forecast performance. Furthermore, FuXi-DA has been validated against established atmospheric physics, demonstrating its consistency and reliability.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"31 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143877902","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
Aerosol inhibition on photochemical surface ozone formation under future climate and air quality scenarios 未来气候和空气质量情景下气溶胶对光化学表面臭氧形成的抑制作用
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-25 DOI: 10.1038/s41612-025-01048-2
G. S. Gopikrishnan, D. M. Westervelt, J. Kuttippurath
{"title":"Aerosol inhibition on photochemical surface ozone formation under future climate and air quality scenarios","authors":"G. S. Gopikrishnan, D. M. Westervelt, J. Kuttippurath","doi":"10.1038/s41612-025-01048-2","DOIUrl":"https://doi.org/10.1038/s41612-025-01048-2","url":null,"abstract":"<p>Aerosols significantly influence tropospheric oxidation and ozone formation by modulating photolysis rates and radical sinks. This study employs the GEOS-Chem model to analyze different aerosol heterogeneous uptake coefficients (0, 0.1, 0.2 and 0.4) and their effects on photochemical ozone levels across global regions under future Shared Socioeconomic Pathways (SSP) scenarios. Lower uptake coefficients lead to an increase in the concentration of radical species like HO<sub>2</sub> and reduce the extent of aerosol-inhibited regime (AIR) in regions such as India and East Asia which are currently within AIR, leading to a notable increase in surface ozone (40–50%), particularly during colder months. Projections for 2046 indicate a global reduction in AIR, resulting from stricter emission controls. By 2096, the extent of AIR further diminishes, with regions like Southeast Asia transitioning to NOx-limited conditions, though aerosol uptake of HO<sub>2</sub> continues to elevate surface ozone levels by 10–15% in heavily aerosol-loaded areas.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"2 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143872930","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
Glacier meltwater has limited contributions to the total runoff in the major rivers draining the Tibetan Plateau 冰川融水对青藏高原主要河流径流量的贡献有限
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-25 DOI: 10.1038/s41612-025-01060-6
Yi Nan, Fuqiang Tian, Jeffrey McDonnell, Guangheng Ni, Lide Tian, Zongxing Li, Denghua Yan, Xinghui Xia, Ting Wang, Songjun Han, Kunbiao Li
{"title":"Glacier meltwater has limited contributions to the total runoff in the major rivers draining the Tibetan Plateau","authors":"Yi Nan, Fuqiang Tian, Jeffrey McDonnell, Guangheng Ni, Lide Tian, Zongxing Li, Denghua Yan, Xinghui Xia, Ting Wang, Songjun Han, Kunbiao Li","doi":"10.1038/s41612-025-01060-6","DOIUrl":"https://doi.org/10.1038/s41612-025-01060-6","url":null,"abstract":"<p>The Tibetan Plateau is the headwaters of several major river basins, but uncertainties exist in the estimated contributions of glacial melt and groundwater to runoff. We present a new tracer-aided glacio-hydrological model constrained by multiple datasets for five major river basins of the Tibetan Plateau. We show that the contribution of glacier melt to the annual runoff is less than 5% in all the five basins at the outlets—much less than previous estimates. Our secondary finding is that the partitioning between surface runoff and groundwater flow varied greatly across the watersheds, with groundwater runoff contributing 35–75% of the annual runoff. The contribution of glacier melt has a strong spatial variability and scale dependency, but the population heavily dependent on it is limited, so a potential significant decrease in water resources due to glacier shrinkage is not a problem that should raise public worries in the Tibetan Plateau.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"8 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143876252","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
Oxygen-rich anionic metal silicate clusters as nucleation seeds for noctilucent clouds 富氧阴离子金属硅酸盐团簇作为夜光云的成核种子
IF 9 1区 地球科学
npj Climate and Atmospheric Science Pub Date : 2025-04-23 DOI: 10.1038/s41612-025-01019-7
Joan Mariñoso Guiu, Joost M. Bakker, Thorsten M. Bernhardt, John M. C. Plane, Stefan T. Bromley, Sandra M. Lang
{"title":"Oxygen-rich anionic metal silicate clusters as nucleation seeds for noctilucent clouds","authors":"Joan Mariñoso Guiu, Joost M. Bakker, Thorsten M. Bernhardt, John M. C. Plane, Stefan T. Bromley, Sandra M. Lang","doi":"10.1038/s41612-025-01019-7","DOIUrl":"https://doi.org/10.1038/s41612-025-01019-7","url":null,"abstract":"<p>Silicate-based meteoric smoke particles (MSPs) resulting from extraterrestrial dust impacting on the upper atmosphere are likely involved in seeding the formation of mesospheric ice-based noctilucent clouds (NLCs). However, the detailed physicochemical properties of MSP seeds remain elusive. Considering that ice formation is sensitive to MSP charging efficiency, here we focus on species which can efficiently capture charge. As in situ MSP characterisation is highly challenging, we mimic atmospheric MSP formation using laser ablation and collisional cooling to produce small anionic magnesium silicate clusters. Our detailed experimental and theoretical characterisation shows that these clusters have unusual oxygen-rich structures. Moreover, the corresponding neutral clusters have extraordinarily high adiabatic electron affinities and 3-18% charging efficiencies, which is remarkably consistent with estimates required by models to simulate atmospheric measurements. Overall, our highly oxidised anionic silicate clusters exhibit all necessary chemical, electronic and optical properties to be highly credible MSP-based seed candidates for NLC nucleation.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"69 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143862915","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
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