Global and Planetary Change最新文献

{"title":"Precipitation lagged behind temperature increase during the Bølling-Allerød interstadial in Northeast China","authors":"Zeyang Zhu ,&nbsp;Jing Wu ,&nbsp;Patrick Rioual ,&nbsp;Jiaxin Lu ,&nbsp;Luo Wang ,&nbsp;Guoqiang Chu ,&nbsp;Jiaqi Liu","doi":"10.1016/j.gloplacha.2025.105032","DOIUrl":"10.1016/j.gloplacha.2025.105032","url":null,"abstract":"<div><div>The Bølling-Allerød (B-A) interstadial (∼14.7–12.85 cal ka BP), the most important warming event of the last deglaciation in the northern hemisphere, is a key time window to study how precipitation changes under the background of rapid warming. However, the relationship between precipitation changes and rapid warming during the B-A interstadial in Northeast (NE) China has remained unclear. Here, we present a multiproxy record spanning the interval 20–10 cal ka BP from a small volcanic lake in NE China and compare it with other records from the same region to clarify the hydroclimatological history of the last deglaciation in NE China. The results suggest that precipitation lagged behind temperature increase during the B-A interstadial in NE China. We attribute this lag to the different forcings at play on the evolution of precipitation and temperature during the B-A, in which the temperature changes were forced by the recovery of the Atlantic Meridional Overturning Circulation and the triggered release of stored heat in the North Atlantic from the high latitudes while the precipitation changes were controlled by increasing sea surface temperatures in the low latitudes.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105032"},"PeriodicalIF":4.0,"publicationDate":"2025-08-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144879770","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}

{"title":"Soil moisture active passive data improve sensitivity assessment of permafrost active layer thickness to wildfire disturbance","authors":"Xiao Jiang ,&nbsp;Hongyan Cai ,&nbsp;Xiaohuan Yang","doi":"10.1016/j.gloplacha.2025.105030","DOIUrl":"10.1016/j.gloplacha.2025.105030","url":null,"abstract":"<div><div>Wildfires have intensified permafrost degradation across the pan-Arctic region, underscoring the urgent need for sensitivity assessments of the active layer thickness (ALT) to improve permafrost carbon emission estimates. However, the limited availability of soil parameters hinders simulations of heat transfer processes. Soil moisture active passive (SMAP) data will likely fill these gaps. We utilized the Kudryavtsev model to simulate the volumetric water content-based ALT (VWC-ALT) and SMAP-based ALT (SMAP-ALT) and compared their sensitivities to wildfires. The SMAP-ALT exhibits significant sensitivity compared with the VWC-ALT. Regions with high SMAP-ALT heterogeneity were associated with wildfires, facilitating the differentiation between burned and unburned areas while enabling the characterization of temporal changes and variations in influencing factors during prefire, fire, and postfire periods. These results highlight that SMAP data enhance sensitivity assessment of the ALT concerning wildfires. This approach also holds significant potential for reflecting other environmental disturbances associated with soil moisture, which is crucial for accurately estimating permafrost carbon emissions.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105030"},"PeriodicalIF":4.0,"publicationDate":"2025-08-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144892142","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}

{"title":"A review of magnetostratigraphy around the Permian-Triassic boundary","authors":"Min Zhang ,&nbsp;Huafeng Qin ,&nbsp;Chenglong Deng ,&nbsp;Shu-zhong Shen ,&nbsp;Yongxin Pan","doi":"10.1016/j.gloplacha.2025.105022","DOIUrl":"10.1016/j.gloplacha.2025.105022","url":null,"abstract":"<div><div>The Permian-Triassic transition, marked by Earth's largest mass extinction and intensive volcanisms, represents a critical interval for understanding global environmental crises and biotic turnovers. Magnetostratigraphy provides a unique tool for correlating marine and terrestrial records, yet inconsistencies in polarity sequences and limited chronostratigraphic precision have hindered robust global correlations. Here we synthesize and rigorously evaluate magnetostratigraphic data across the late Lopingian (Late Permian) to the earliest Triassic from China, North American, central European Basin, Karoo Basin, East European Platform and Siberian Trap suites — using a unified reliability framework (M-value ≥4). Our reanalysis reveals that the late Permian Changhsingian Stage is dominated by normal polarity magnetozones (P1n to P5n from younger to older), intercalated with four short reversed polarity intervals (P1r to P4r from younger to older). The base of normal polarity interval P1n is interpolated to be ∼252.2 Ma. The end-Permian mass extinction and Permian-Triassic boundary are thus placed in the lower part of the normal magnetozone P1n. Three additional magnetozones (T1r, T1n and T2r from younger to older) are recognized in the earliest Triassic Induan Stage. The distinct normal polarity P1n across the Permian-Triassic boundary can serve as a potential marker for improving correlation of the Permian-Triassic interval between marine and non-marine sequences. In future, improved measurement technology for isolating primary remanent magnetizations, more rigorous cross-checking of high-resolution magnetostratigraphic sequences and high-precision geochronological constraints are necessary to refine a reliable magnetostratigraphic timescale during the Permian-Triassic transition.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105022"},"PeriodicalIF":4.0,"publicationDate":"2025-08-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144879771","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}

{"title":"Functional traits from pollen and plant assemblages show complex relationships on the Tibetan Plateau: A deep insight into plant functional paleoecology","authors":"Mengna Liao,&nbsp;Yili Jin,&nbsp;Kai Li,&nbsp;Jian Ni","doi":"10.1016/j.gloplacha.2025.105031","DOIUrl":"10.1016/j.gloplacha.2025.105031","url":null,"abstract":"<div><div>Functional paleoecology offers a novel approach that bridges the gap between Quaternary paleoecology and modern ecology, but the feasibility of applying functional trait-based approaches to pollen data remains underexplored. In this study, we compiled datasets of plant communities, plant functional traits, and pollen counts obtained from 207 sites across the Tibetan Plateau to evaluate the accuracy of pollen-based functional traits in reflecting functional trait composition and functional diversity within their surrounding plant communities. Our findings reveal that, across the broad scale of the entire study area, community-weighted means (CWMs) of each plant functional trait estimated from pollen data show significant correlations with those estimated from plant assemblages. However, this conclusion does not apply uniformly to all vegetation types. For instance, in alpine meadow, leaf thickness (LT), specific leaf area (SLA), leaf nitrogen content (LNC), and leaf phosphorus content (LPC) show non-significant correlations between CWMs derived from pollen data and those derived from plant assemblages. Functional diversity indices (FDs) generally show very weak correlations (<em>R</em>^<em>2</em> &lt; 0.2) between pollen- and plant-based estimations, with the exception of functional richness, which displays significant correlations across the entire study area (regardless of vegetation type) and in four of the seven vegetation types analyzed. The results demonstrate that both the pollen-inferred CWMs of plant functional traits and pollen-inferred FDs show significant correlations with temperature and precipitation. However, only LT, LPC, and functional divergence estimated from pollen assemblages adequately capture the trends in plant-derived CWMs and FDs along temperature and precipitation gradients. Our study underscores the potential of pollen data for reconstructing temporal trends in plant functional traits through the integration of functional trait approaches. Nevertheless, the application of plant functional paleoecology necessitates careful selection of functional traits and functional diversity indices, as well as a consideration of vegetation context when interpreting changes in pollen-inferred functional trait composition and functional diversity.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105031"},"PeriodicalIF":4.0,"publicationDate":"2025-08-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144864920","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}

{"title":"Seasonally dependent changes in the North Pacific subtropical anticyclone during the mid-Holocene: Dominant role of mid-latitude baroclinicity","authors":"Shanshan Liu ,&nbsp;Dabang Jiang","doi":"10.1016/j.gloplacha.2025.105028","DOIUrl":"10.1016/j.gloplacha.2025.105028","url":null,"abstract":"<div><div>Understanding mechanisms behind North Pacific subtropical anticyclone (NPSA) changes is pivotal for interpreting mid-Holocene climate variations. This study investigates NPSA changes between mid-Holocene and preindustrial periods using simulations from 15 Coupled Model Intercomparison Project Phase 6 (CMIP6) models. The results reveal pronounced seasonal disparities: the NPSA weakens and contracts in spring but strengthens and expands in summer. These variations stem from orbitally induced changes in meridional and zonal thermal structures, which modulate the NPSA by redistributing precipitation-released latent heat and by altering the North Pacific westerly jet. In spring, reduced insolation shifts North Pacific baroclinic zones southward, as indicated by meridional temperature gradient changes, and attenuates land–sea contrasts in surface equivalent potential temperature (<em>θ</em>_e). The southward-shifted baroclinic zone displaces the westerly jet southward, accounting for NPSA weakening over its northern–central sector, while the attenuated land–sea <em>θ</em>_e contrast enhances oceanic convective precipitation, weakening the NPSA's eastern flank. In summer, the NPSA intensification primarily results from reduced large-scale precipitation over the North Pacific due to diminished mid-latitude baroclinicity caused by increased insolation. This summertime NPSA intensification is additionally fueled by enhanced convective precipitation over Asian land and diminished convective precipitation over the North Pacific, associated with orbitally amplified land–sea <em>θ</em>_e contrasts. This study highlights the primary role of altered meridional temperature gradients, which largely determine atmospheric baroclinicity, in shaping the NPSA, rather than the previously emphasized land–sea thermal contrasts. The simulation plausibly explains discrepancies in NPSA changes inferred from proxies in the western and eastern North Pacific.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105028"},"PeriodicalIF":4.0,"publicationDate":"2025-08-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144879772","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}

{"title":"Continental weathering linked to climate warming at the Sakmarian to Artinskian transition","authors":"Yanan Li ,&nbsp;Longyi Shao ,&nbsp;Christopher R. Fielding ,&nbsp;Tracy D. Frank ,&nbsp;Zhaorui Ye ,&nbsp;Jing Lu ,&nbsp;Kuan Yang ,&nbsp;Shuai Wang","doi":"10.1016/j.gloplacha.2025.105025","DOIUrl":"10.1016/j.gloplacha.2025.105025","url":null,"abstract":"<div><div>Assessing the patterns of climate change and their complex interactions with continental weathering throughout geological history offers profound insights into the mechanisms of the Earth's dynamic climate system. The Artinskian Warming Event (AWE) was characterized by a progressive rise in paleotemperatures during the late Paleozoic Ice Age (LPIA), coinciding with the retreat of large-scale Gondwanan ice sheets and profound transformations in the terrestrial ecosystems of Euramerica. Despite these observations, the exact chronology, nature, and geographical extent of the AWE are yet to be precisely defined. The contribution of continental weathering to the accumulation of atmospheric <em>p</em>CO₂ concentrations, which subsequently facilitated the melting of major LPIA ice centers by the mid-late Cisuralian, remains a topic of ongoing debate. To comprehensively trace the global extent of the AWE and to examine the potential causal link between climate and weathering processes during the Sakmarian to Artinskian transition, a detailed record of weathering trends in low-latitude mudstones has been established from the Dacheng coalfield in Hebei Province, North China. This far-field dataset, along with the near-field sedimentological record from eastern Australia, as well as published weathering trends and additional climate records from a spectrum of low to high latitude regions, has been compiled and synthesized for comprehensive analysis. The results reveal a globally notable rise in chemical weathering intensities and mean surface temperatures across the Sakmarian to Artinskian transition, while chemical weathering intensities significantly decreased in the earliest Artinskian within the Dacheng coalfield and parts of North China, consistent with the AWE-recorded aridification. These patterns are in alignment with the processes of deglaciation, increased sea surface temperature, and sea-level high-stand, along with shifts in biodiversity and changes in the abundance of marine and terrestrial ecosystems. The perturbations in the carbon cycle across a wide geographical area further substantiate the AWE as a global event. LIP volcanism supplied an initial CO₂ pulse, while the subsequent sustained decline in silicate weatherability during the earliest Artinskian, driven by low-latitude aridification, enabled prolonged escalation of atmospheric <em>p</em>CO₂ levels. This phenomenon is believed to have contributed to the onset of the AWE. The findings of this study will enhance our understanding of the AWE and the climate-weathering relationship during the demise of the LPIA.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105025"},"PeriodicalIF":4.0,"publicationDate":"2025-08-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144879774","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}

{"title":"Weakened ENSO-precipitation teleconnection over southern Africa during the Last Interglacial: A modeling perspective","authors":"Jialu Ma ,&nbsp;Qing Yan ,&nbsp;Huijun Wang","doi":"10.1016/j.gloplacha.2025.105024","DOIUrl":"10.1016/j.gloplacha.2025.105024","url":null,"abstract":"<div><div>Precipitation in southern Africa has major impacts on local socio-economic development owing to the strong dependency on rain-fed agriculture, and its interannual variability is controlled by the El Niño-Southern Oscillation (ENSO). To help comprehend their linkage in a warmer future, here we investigate how the ENSO-southern African precipitation teleconnection in austral summer may vary during the Last Interglacial (LIG; ∼130–115 ka BP). Based on the model outputs from Paleoclimate Modeling Intercomparison Project Phase 4, we demonstrated that southern African precipitation in austral summer was negatively correlated with ENSO during the LIG (e.g., reduced precipitation during an El Niño event), similar to modern conditions, but the linkage was weakened by ∼42 % relative to the preindustrial in terms of the regression coefficient. The weakened ENSO-precipitation teleconnection was forced primarily by the El Niño-driven anomalous low-level cyclone over southern Africa during the LIG, which was also observed in the moisture flux pattern. The abnormal cyclone was associated with anomalous ascents and increased regional precipitation, supported by moisture budget analysis, which hence dampened the negative linkage between ENSO and precipitation seen in the present day. The anomalous atmospheric circulations might be linked to the dampened ENSO variability during the LIG by inducing a weakened Gill-type response in the central Pacific and associated secondary forcings in the Atlantic. Our results may help obtain a deeper comprehension of ENSO-southern African precipitation teleconnection in the orbitally induced warmer climate.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105024"},"PeriodicalIF":4.0,"publicationDate":"2025-08-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144879773","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}

{"title":"Altitude weakens the drought resistance-resilience tradeoff across northern ecosystems","authors":"Yuting Yang ,&nbsp;Xie He ,&nbsp;Yunfei Feng ,&nbsp;Ben Niu ,&nbsp;Jianshuang Wu ,&nbsp;Meng Li","doi":"10.1016/j.gloplacha.2025.105026","DOIUrl":"10.1016/j.gloplacha.2025.105026","url":null,"abstract":"<div><div>Ecosystem stability during droughts determined by two key attributes: resistance and resilience, which often exhibit a tradeoff across species to biome scales. However, under extreme environmental stress, ecosystems may activate multidimensional stabilization mechanisms that weaken this tradeoff. In this study, we hypothesize that high-altitude ecosystems, shaped by greater climatic heterogeneity and harsher abiotic constraints, display a weaker resistance–resilience tradeoff compared to lowland systems. Focusing on northern terrestrial ecosystems (≥ 30° N), we integrate drought indices with eddy covariance data and remote sensing observations to map the spatial patterns of drought resistance, resilience, and their tradeoffs. Our analysis confirms that the resistance–resilience tradeoff is widespread, yet weakens with increasing altitude. Using explainable machine learning, we identify altitude as the dominant driver of spatial variability in tradeoff strength. Crucially, this effect is biome-dependent: in arid biomes (shrublands, savannas, and grasslands), altitude is a key predictor, whereas in humid biomes (forests and wetlands), climatic variables play a stronger role. Aridity-gradient analysis further reveals that altitude's explanatory power declines in wetter environments. For nearly all biomes, with the exception of wetlands, the resistance–resilience tradeoff weakens with increasing altitude. Finally, Earth System Models (ESMs) from the CMIP6 ensemble fail to capture this altitudinal variability, limiting their predictive accuracy. Our findings highlight the critical role of altitude-driven stability dynamics in shaping drought responses.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105026"},"PeriodicalIF":4.0,"publicationDate":"2025-08-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144841534","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}

{"title":"Anomalous warm winters on the southeastern Tibetan Plateau during the 8.2 ka cold event: Implications for recent warming amplification","authors":"Wenmin Yu,&nbsp;Xiaojian Zhang","doi":"10.1016/j.gloplacha.2025.105027","DOIUrl":"10.1016/j.gloplacha.2025.105027","url":null,"abstract":"<div><div>Holocene climate changes exhibited pronounced millennial-scale oscillations in response to the slowdown of the Atlantic meridional overturning circulation (AMOC). Millennial-scale temperature variations on the southeastern Tibetan Plateau remain an ongoing topic of scientific debate. This study explores winter temperature variations on the southeastern Tibetan Plateau during the 8.2 ka cold event using climate simulations driven by North Atlantic freshwater forcing. Our hosing simulations reveal anomalous winter warming on the southeastern Tibetan Plateau in response to the AMOC weakening during the 8.2 ka cold event. This anomalous warming was due to mid-tropospheric southwesterly anomalies extending from the tropical Indian Ocean to the southeastern Tibetan Plateau, leading to significant warm advection into the southeastern Tibetan Plateau. These mid-tropospheric southwesterly anomalies were induced by the intensification of the southern bypassing flows, which originated from an anomalous anticyclone over the tropical Indian Ocean. The anomalous anticyclone resulted from a Rossby-like wave train originating in the North Atlantic, which was triggered by the North Atlantic cooling due to the AMOC weakening. Hence, the AMOC weakening induced anomalous winter warming on the southeastern Tibetan Plateau during the 8.2 ka cold event. Analogous to the 8.2 ka cold event, the southeastern Tibetan Plateau experiences increased winter temperatures due to the weakening of the AMOC. The weakened AMOC has probably amplified the winter warming on the southeastern Tibetan Plateau in recent decades.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105027"},"PeriodicalIF":4.0,"publicationDate":"2025-08-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144860623","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}

{"title":"Reconciling inconsistent trends of geochemical and environmental magnetic records from East Asian sediments based on modern calibration","authors":"Li Xing ,&nbsp;Peng Gao ,&nbsp;Junsheng Nie ,&nbsp;Xueping Ren ,&nbsp;Hansheng Wang ,&nbsp;Bo Cao ,&nbsp;Baotian Pan","doi":"10.1016/j.gloplacha.2025.105023","DOIUrl":"10.1016/j.gloplacha.2025.105023","url":null,"abstract":"<div><div>An accurate understanding of the effects of temperature/precipitation variations on geochemical and magnetic indicators within soils is fundamental to reconstructing the evolution of the Asian monsoon. Here, we investigate correlations between temperature/precipitation and geochemical/magnetic parameters in a Qilian Shan elevation transect. Our results suggest that the geochemical indicators of chemical weathering intensity are dominantly controlled by precipitation at low altitudes, but, at higher altitudes, temperature replaces precipitation as the primary controlling factor. In contrast, magnetic indicators consistently reflect precipitation influences across elevations. We explore this framework to address contradictions between magnetic and geochemical records from the Chinese Loess Plateau, proposing that late Neogene geochemical variations may reflect temperature shifts during global cooling, while magnetic changes align with precipitation, modulated by CO₂ and tectonic paleogeography. We advocate for an integrated approach to reconstructing terrestrial temperature and precipitation histories.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105023"},"PeriodicalIF":4.0,"publicationDate":"2025-08-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144865038","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}