Today＇s idea of the so-called fin-de-sibcle is still somewhat inexact and incomplete. This lack of precision originates from a deeply rooted methodological approach which consists of considering the respective develo...Today＇s idea of the so-called fin-de-sibcle is still somewhat inexact and incomplete. This lack of precision originates from a deeply rooted methodological approach which consists of considering the respective developments of literature, art, and science in isolation, without paying attention to any interference or reciprocal contamination. This defective method also affects the overlaps and contacts between high culture and popular culture. Despite the progress made over recent years, there are few researchers who approach their objective with a real awareness of the complexity of a time period which saw the appearance of mass culture in the current sense and an unprecedented boom in scientific and technological development.1 To this end, the example of the great German philosopher Walter Benjamin and his studies on Paris during the 19th century----collected in the essays on the great French poet Charles Baudelaire and especially in the monumental and unfinished work The Arcades Project--is, without doubt, a model to follow. Taking the path suggested by Benjamin, this article sets out a revision of the novel Bruges-la-Morte （1892） by the Belgian writer Georges Rodenbach, considered one of the major exponents of thefin-de-sikcle decadence, which goes beyond the usual approach of a symbolist reading, by paying special attention to the frictions between literature and technology on one hand, and between literature and popular entertainment on the other.展开更多
Sigalit Landau is an international sculpture,video,installation,and performance artist,born in Jerusalem,and raised also in the USA and the UK.The infernal main space in her installation“The Dining Hall”(2007,KW Ins...Sigalit Landau is an international sculpture,video,installation,and performance artist,born in Jerusalem,and raised also in the USA and the UK.The infernal main space in her installation“The Dining Hall”(2007,KW Institute for Contemporary Art,Berlin)is filled with images resembling human remains engaged in riotous consumption from huge iron pots,in physical circus-like tricks,and copulation,surrounded by huge fleshy-like constructions.While the immediate association may be that of an apocalyptic catastrophe in relation to the Holocaust,the reference is multifaceted,as this study seeks to show.There is a strong connotation of corporeality,gluttony,digestion,decay,and abjection combined with licentiousness,and a proximity between death and pleasure.This multiplicity of contexts is embedded in the term décadence,in its connection with Antiquity and mostly with ancient Rome,and calls to mind the Roman Menippean 1st century CE text Satyricon by Petronius.A comparative analysis of Landau’s installation in relation to Satyricon opens up the way to a broad interpretation,revealing much topical and conceptual parallelism that reveals Landau’s engagement with a kind of decadence typical to the contemporary condition and that of Israel in particular.A prominent feature of her installation is that of victimhood and its influence on the Israeli occupation policy and conduct.Consequently,Landau’s installation is interpreted here as an allegory of a particular state of mind,reflecting both decadence and victimhood.展开更多
Till date,no study on trends in extreme sea surface temperature(SST)for different return periods has been done over the Gulf of Tonkin(GoT).Based on a 84-year(1940–2023)ERA5 Reanalysis data sets,this study for the fi...Till date,no study on trends in extreme sea surface temperature(SST)for different return periods has been done over the Gulf of Tonkin(GoT).Based on a 84-year(1940–2023)ERA5 Reanalysis data sets,this study for the first time,examined the spatio-temporal pattern in extreme SST for different return periods.Findings showed that more significant moderate to fast warming trends(0.1–0.16°C per decade(dec-1))only existed for the 2 year return period.Temporal trends in the 99th percentile SST are insignificant for all return periods.By using the linear regression method,the variability in extreme SST was obtained.Results showed that moderate warming trends dominated a large portion of GoT.Stronger trends,up to 0.018°C yr-1 are noticed near Guangdong,Haikou and southern Sanya in south China.Extreme SST exhibited a slow warming trend of 0.008°C per year(yr-1)all through the study years.The SST is most stable in most waters in the southern GoT and few waters surrounding Dongfang.Temporal warming rates of SST revealed that 1940–1958,1976–1994 and 2003–2012 were years of more coastal upwelling and could affect aquatic lives.The strongest warming rate of 0.07°C dec-1 occurred during 1994–2003.The GoT appeared warmer during spring.Spatial decadal variability of SST revealed that moderate warming trends occurred in few regions in the southern GoT and in larger portion of the central and northern GoT.The rise in SST between 1980 and 2020 in the GoT is not limited to increased anthropogenic activities.展开更多
Since the mid-20th century,the Mongolian Plateau(MP)has experienced decadal droughts coupled with extreme heatwaves,severely affecting regional ecology and social development.However,the mechanisms behind these decada...Since the mid-20th century,the Mongolian Plateau(MP)has experienced decadal droughts coupled with extreme heatwaves,severely affecting regional ecology and social development.However,the mechanisms behind these decadalscale compound heatwavedrought events remain debated.Here,using reconstructions and simulations from the Community Earth System Model Last Millennium Ensemble,we demonstrate that,over the last millennium,decadal droughts on the MP occurred under both warm and cold conditions,differing from recent compound heatwavedrought events.We found that by examining temperature changes during these drought periods,the distinct influences of external forcings and internal variability can be simply and effectively distinguished.Specifically,colddry events were primarily driven by volcanic eruptions that weakened the East Asian summer monsoon and midlatitude westerlies,reducing moisture transport to the MP.In contrast,warmdry events were predominantly induced by internal variability,notably the negative phase of the Atlantic Multidecadal Oscillation and the expansion of the Barents Sea ice extent.The recent extreme compound event was probably influenced by the combined effects of anthropogenic forcings and internal variability.These findings deepen our understanding of how external forcings and internal variability affect decadal drought events on the MP and highlight that recent compound events are unprecedented in the context of the last millennium.展开更多
The Australian monsoon system plays a pivotal role in the tropical climate system by modulating the El Niño-Southern Oscillation(ENSO)development through multi-scale ocean-atmosphere interactions.This study ident...The Australian monsoon system plays a pivotal role in the tropical climate system by modulating the El Niño-Southern Oscillation(ENSO)development through multi-scale ocean-atmosphere interactions.This study identifies a significant decadal weakening of the Australian cross-equatorial flow intensity over the past two decades,attributed to the concurrent westward shift of the Australian High(AH)during austral winter.These decadal changes in the Australian monsoon reduce tropical Pacific atmospheric convection and the associated westerly wind anomalies over the centralto-western Pacific,which are crucial precursors for ENSO development.This process diminishes air-sea coupling feedback,including the thermocline feedback and the Ekman feedback,ultimately decreasing the strength of warm ENSO(El Niño)events.Using the Community Earth System Model,we confirm the close linkage between the Australian monsoon and ENSO on the decadal timescale.These findings provide new insights into the coupled relationship between ENSO and monsoon variability,offering a valuable framework for understanding ENSO’s longterm modulation and improving future climate predictions.展开更多
El Niño is frequently followed by La Niña,while La Niña tends to sustain into the next year or even longer,exhibiting a notable phase transition asymmetry(TA)of El Niño-Southern Oscillation(ENSO).T...El Niño is frequently followed by La Niña,while La Niña tends to sustain into the next year or even longer,exhibiting a notable phase transition asymmetry(TA)of El Niño-Southern Oscillation(ENSO).This study explores the potential influences of tropical Indian Ocean(TIO)decadal variability on TA based on a comparative analysis of the relationship between the TIO sea surface temperature anomalies(SSTA)and ENSO during different periods.Generally,the TIO SSTA strengthened TA before the 1980s,corresponding to a highly positive relationship between the whole TIO SSTA and ENSO.However,the weakening effect was exhibited after the 1980s when the correlation diminished.After the late 1990s,ENSO was only positively correlated with western TIO,with the westerly exhibit of the SSTA center leading to smaller impacts on TA.Moreover,TIO SSTA tends to weaken TA by promoting the transition efficiency of La Niña,while bringing little effect on that of El Niño.Physically,compared to the mid-1970s,TIO SSTA triggered westerly wind anomalies during the autumn and winter of the La Niña development phase in the central equatorial Pacific in the late 1990s,which sped up the decay of La Niña.It then regenerated westerly anomalies in the following winter,facilitating the development of El Niño.This study quantifies the impact of the TIO SSTA on TA in seasonal signals and investigates the decadal variability of such influence,aiming to further understand phase transition asymmetry and offer valuable insights for the prediction of multi-year La Niña.展开更多
The global monsoon system,encompassing the Asian-Australian,African,and American monsoons,sustains two-thirds of the world’s population by regulating water resources and agriculture.Monsoon anomalies pose severe risk...The global monsoon system,encompassing the Asian-Australian,African,and American monsoons,sustains two-thirds of the world’s population by regulating water resources and agriculture.Monsoon anomalies pose severe risks,including floods and droughts.Recent research associated with the implementation of the Global Monsoons Model Intercomparison Project under the umbrella of CMIP6 has advanced our understanding of its historical variability and driving mechanisms.Observational data reveal a 20th-century shift:increased rainfall pre-1950s,followed by aridification and partial recovery post-1980s,driven by both internal variability(e.g.,Atlantic Multidecadal Oscillation)and external forcings(greenhouse gases,aerosols),while ENSO drives interannual variability through ocean-atmosphere interactions.Future projections under greenhouse forcing suggest long-term monsoon intensification,though regional disparities and model uncertainties persist.Models indicate robust trends but struggle to quantify extremes,where thermodynamic effects(warming-induced moisture rise)uniformly boost heavy rainfall,while dynamical shifts(circulation changes)create spatial heterogeneity.Volcanic eruptions and proposed solar radiation modification(SRM)further complicate predictions:tropical eruptions suppress monsoons,whereas high-latitude events alter cross-equatorial flows,highlighting unresolved feedbacks.The emergent constraint approach is booming in terms of correcting future projections and reducing uncertainty with respect to the global monsoons.Critical challenges remain.Model biases and sparse 20th-century observational data hinder accurate attribution.The interplay between natural variability and anthropogenic forcings,along with nonlinear extreme precipitation risks under warming,demands deeper mechanistic insights.Additionally,SRM’s regional impacts and hemispheric monsoon interactions require systematic evaluation.Addressing these gaps necessitates enhanced observational networks,refined climate models,and interdisciplinary efforts to disentangle multiscale drivers,ultimately improving resilience strategies for monsoon-dependent regions.展开更多
In August 2024,the United Nations General Assembly adopted resolution 78/321 to declare the period from 2025 to 2034 as the“Decade of Action for Cryospheric Sciences”.This action was championed by the Republic of Fr...In August 2024,the United Nations General Assembly adopted resolution 78/321 to declare the period from 2025 to 2034 as the“Decade of Action for Cryospheric Sciences”.This action was championed by the Republic of France and the Republic of Tajikistan,with support from over 30 member states,underscoring the urgent need for an international scientific collaboration to mitigate the far-reaching effects of cryospheric changes on ecosystems,water security,and global climate stability.A dedicated brainstorming session during the March 2025 celebrations in Paris convened over 1,000 policymakers,scientists,and stakeholders to outline the priorities for the Decade of Action.The session aimed to foster cross-border partnerships and strengthen the integration of cryospheric science into global climate adaptation strategies.Joint task force teams developed an integrated governance framework through discussions across five domains—scientific research,socioeconomic impacts,education,policy advocacy,and finance.The Decade of Action for Cryospheric Sciences represents a critical shift from observation to intervention,mobilizing global stakeholders to translate scientific consensus into concrete measures against cryosphere decline.The initiative responds to urgent calls from UNESCO and international partners for coordinated action on cryosphere preservation.展开更多
Marine heatwaves(MHWs)have become increasingly frequent and persistent in the context of global warming and the related underlying mechanisms are strongly region-dependent.We employed the NOAA(National Oceanic and Atm...Marine heatwaves(MHWs)have become increasingly frequent and persistent in the context of global warming and the related underlying mechanisms are strongly region-dependent.We employed the NOAA(National Oceanic and Atmospheric Administration)CRW(Coral Reef Watch)daily mean sea surface temperature dataset spanning from 1985 to 2022 to comprehensively analyze the fundamental attributes and evolving patterns of marine heatwaves in the offshore waters of China.Eight pronounced marine heatwaves from frequently affected sensitive regions were investigated to explore their formation mechanisms.The relationship between the occurrences of marine heatwave and large-scale climate mode in the region was explored.Results show that the western Pacific subtropical high plays an essential role in triggering marine heatwaves in Chinese offshore waters,with an anomalous downward shortwave radiation flux acting to warm the sea surface,which is remotely associated to the large-scale sea surface temperature state.Distinct mechanisms for the MHWs were identified in the northern and southern offshore waters of China.MHWs in high latitudes(such as the Bohai Sea and the Yellow Sea)mainly occur during the negative phase of the Pacific Decadal Oscillation(PDO),while those in low latitudes(such as the South China Sea)are more common in about 5-month lags behind the El Niño,for which we purposed a mechanism to describe the main differences in the formation of MHWs in China and discussed the related implications.展开更多
The frequency and duration of observed concurrent hot and dry events(HDEs) over China during the growing season(April–September) exhibit significant decadal changes across the mid-1990s. These changes are characteriz...The frequency and duration of observed concurrent hot and dry events(HDEs) over China during the growing season(April–September) exhibit significant decadal changes across the mid-1990s. These changes are characterized by increases in HDE frequency and duration over most of China, with relatively large increases over southeastern China(SEC), northern China(NC), and northeastern China(NEC). The frequency of HDEs averaged over China in the present day(PD,1994–2011) is double that in the early period(EP, 1964–81);the duration of HDEs increases by 60%. Climate experiments with the Met Office Unified Model(MetUM-GOML2) are used to estimate the contributions of anthropogenic forcing to HDE decadal changes over China. Anthropogenic forcing changes can explain 60%–70% of the observed decadal changes,suggesting an important anthropogenic influence on HDE changes over China across the mid-1990s. Single-forcing experiments indicate that the increase in greenhouse gas(GHG) concentrations dominates the simulated decadal changes,increasing the frequency and duration of HDEs throughout China. The change in anthropogenic aerosol(AA) emissions significantly decreases the frequency and duration of HDEs over SEC and NC, but the magnitude of the decrease is much smaller than the increase induced by GHGs. The changes in HDEs in response to anthropogenic forcing are mainly due to the response of climatological mean surface air temperatures. The contributions from changes in variability and changes in climatological mean soil moisture and evapotranspiration are relatively small. The physical processes associated with the response of HDEs to GHG and AA changes are also revealed.展开更多
Observational analyses demonstrate that the Ural persistent positive height anomaly event(PAE) experienced a decadal increase around the year 2000, exhibiting a southward displacement afterward. These decadal variatio...Observational analyses demonstrate that the Ural persistent positive height anomaly event(PAE) experienced a decadal increase around the year 2000, exhibiting a southward displacement afterward. These decadal variations are related to a large-scale circulation shift over the Eurasian Continent. The effects of underlying sea ice and sea surface temperature(SST) anomalies on the Ural PAE and the related atmospheric circulation were explored by Atmospheric Model Intercomparison Project(AMIP) experiments from the Coupled Model Intercomparison Project Phase 6 and by sensitivity experiments using the Atmospheric General Circulation Model(AGCM). The AMIP experiment results suggest that the underlying sea ice and SST anomalies play important roles. The individual contributions of sea ice loss in the Barents-Kara Seas and the SST anomalies linked to the phase transition of the Pacific Decadal Oscillation(PDO) and Atlantic Multidecadal Oscillation(AMO) are further investigated by AGCM sensitivity experiments isolating the respective forcings.The sea ice decline in Barents-Kara Seas triggers an atmospheric wave train over the Eurasian mid-to-high latitudes with positive anomalies over the Urals, favoring the occurrence of Ural PAEs. The shift in the PDO to its negative phase triggers a wave train propagating downstream from the North Pacific. One positive anomaly lobe of the wave train is located over the Ural Mountains and increases the PAE there. The negative-to-positive transition of the AMO phase since the late-1990s causes positive 500-h Pa height anomalies south of the Ural Mountains, which promote a southward shift of Ural PAE.展开更多
The subtropical North and South Pacific Meridional Modes(NPMM and SPMM)are well known precursors of El Niño-Southern Oscillation(ENSO).However,relationship between them is not constant.In the early 1980,the relat...The subtropical North and South Pacific Meridional Modes(NPMM and SPMM)are well known precursors of El Niño-Southern Oscillation(ENSO).However,relationship between them is not constant.In the early 1980,the relationship experienced an interdecadal transition.Changes in this connection can be attributed mainly to the phase change of the Pacific decadal oscillation(PDO).During the positive phase of PDO,a shallower thermocline in the central Pacific is responsible for the stronger trade wind charging(TWC)mechanism,which leads to a stronger equatorial subsurface temperature evolution.This dynamic process strengthens the connection between NPMM and ENSO.Associated with the negative phase of PDO,a shallower thermocline over southeastern Pacific allows an enhanced wind-evaporation-SST(WES)feedback,strengthening the connection between SPMM and ENSO.Using 35 Coupled Model Intercomparison Project Phase 6(CMIP6)models,we examined the NPMM/SPMM performance and its connection with ENSO in the historical runs.The great majority of CMIP6 models can reproduce the pattern of NPMM and SPMM well,but they reveal discrepant ENSO and NPMM/SPMM relationship.The intermodal uncertainty for the connection of NPMM-ENSO is due to different TWC mechanism.A stronger TWC mechanism will enhance NPMM forcing.For SPMM,few models can simulate a good relationship with ENSO.The intermodel spread in the relationship of SPMM and ENSO owing to SST bias in the southeastern Pacific,as WES feedback is stronger when the southeastern Pacific is warmer.展开更多
Under global warming,understanding the long-term variation in different types of heatwaves is vital for China’s preparedness against escalating heat stress.This study investigates dry and wet heatwave shifts in easte...Under global warming,understanding the long-term variation in different types of heatwaves is vital for China’s preparedness against escalating heat stress.This study investigates dry and wet heatwave shifts in eastern China over recent decades.Spatial trend analysis displays pronounced warming in inland midlatitudes and the Yangtze River Valley,with increased humidity in coastal regions.EOF results indicate intensifying dry heatwaves in northern China,while the Yangtze River Valley sees more frequent dry heatwaves.On the other hand,Indochina and regions north of 25°N also experience intensified wet heatwaves,corresponding to regional humidity increases.Composite analysis is conducted based on different situations:strong,frequent dry or wet heatwaves.Strong dry heatwaves are influenced by anticyclonic circulations over northern China,accompanied by warming SST anomalies around the coastal midlatitudes of the western North Pacific(WNP).Frequent dry heatwaves are related to strong subsidence along with a strengthened subtropical high over the WNP.Strong and frequent wet heatwaves show an intensified Okhotsk high at higher latitudes in the lower troposphere,and a negative circumglobal teleconnection wave train pattern in the upper troposphere.Decaying El Niño SST patterns are observed in two kinds of wet heatwave and frequent dry heatwave years.Risk analysis indicates that El Niño events heighten the likelihood of these heatwaves in regions most at risk.As global warming continues,adapting and implementing mitigation strategies toward extreme heatwaves becomes crucial,especially for the aforementioned regions under significant heat stress.展开更多
Background: Characterisation of cotton-based cropping systems is essential for understanding and improving cotton production in Côte d’Ivoire. The aim of this study was to determine the effects of cropping pract...Background: Characterisation of cotton-based cropping systems is essential for understanding and improving cotton production in Côte d’Ivoire. The aim of this study was to determine the effects of cropping practices on seed cotton yields. A survey of a network of 600 growers in all the cotton-growing areas was carried out to gather information on the type of soil preparation (manual, harnessed and motorised), the sowing decade, the previous crop, the cotton variety, the sowing density, the date of fertilizer application (NPK and urea), the number of weeding operations, the number of insecticide treatments and, finally, the seedcotton yield. Results: The results showed that during the last cotton season (2023-2024), the sowing decades, crop precedents and a number of insecticide treatments had a highly significant effect on yield. Sowing in the first, second and third decade of June (1 to 10 June, 11 to 20 June and 21 to 30 June respectively). In addition, the best yields were obtained by growers who applied NPKSB base fertilizer and cover fertilizer (urea) within the sowing period at 10 days before sowing (0 - 10 days before sowing) and 45 - 60 days before sowing, respectively. In addition, better yields of close to 2 tons per hectare (1725 kg/ha) were observed among growers who applied a dozen insecticide treatments (eleven more than the six recommended by the research and development services). Conclusion: Further analysis will be carried out, taking into account parameters such as plot size, fertilizer doses (NPK and urea), climatic parameters (rainfall and temperature), agro-ecological zones and the physico-chemical parameters of the growers’ soils. With this in mind, the Ivorian cotton companies will be able to provide farmers with a decision-making tool to help them monitor cultivation operations and improve farm performance.展开更多
The West African Monsoon (WAM) is characterized by strong decadal and multi-decadal variability and the impacts can be catastrophic for the local populations. One of the factors put forward to explain this variability...The West African Monsoon (WAM) is characterized by strong decadal and multi-decadal variability and the impacts can be catastrophic for the local populations. One of the factors put forward to explain this variability involves the role of atmospheric dynamics, linked in particular to the Saharan Heat Low (SHL). This article addresses this question by comparing the sets of preindustrial control and historical simulation data from climate models carried out in the framework of the CMIP5 project and observations data over the 20<sup>th</sup> century. Through multivariate statistical analyses, it was established that decadal modes of ocean variability and decadal variability of Saharan atmospheric dynamics significantly influence decadal variability of monsoon precipitation. These results also suggest the existence of external anthropogenic forcing, which is superimposed on the decadal natural variability inducing an intensification of the signal in the historical simulations compared to preindustrial control simulations. We have also shown that decadal rainfall variability in the Sahel, once the influence of oceanic modes has been eliminated, appears to be driven mainly by the activity of the Arabian Heat Low (AHL) in the central Sahel, and by the structure of the meridional temperature gradient over the inter-tropical Atlantic in the western Sahel.展开更多
Based on temperature data of meteorological stations from 1971 to 2008 in Tibet,the temporal and spatial variation of maximum andminimum temperature in Tibet was analyzed.The results showed that both maximum temperatu...Based on temperature data of meteorological stations from 1971 to 2008 in Tibet,the temporal and spatial variation of maximum andminimum temperature in Tibet was analyzed.The results showed that both maximum temperature andminimum temperature increased distinctly,the warming amplitude of winter was the highest among the four seasons,and next came spring.The increment ofminimum temperature was visibly over that of maximum temperature,particularlyminimum temperature in winter with significant increment.For spatial variation,maximum temperature in most stations increased except particular stations,while theminimum temperature in all stations rose.In addition,the space variation law ofminimum temperature,being more obvious thanminimum temperature,increased from southeast to northwest with different spatial changes in various seasons.From decadal variation,both maximum andminimum temperature appeared increase from 1970s to the first eight years in the 21st century,and the rise ofminimum temperature was significant greater than maximum temperature.The increase of maximum andminimum temperature was the highest from 2001 to 2008,whereas the lowest in 1970s.展开更多
China has been experiencing widespread air pollution due to rapid industrialization and urbanization in recent decades.The two major concerns of ambient air quality in China are particulate matter(PM)and tropospheric ...China has been experiencing widespread air pollution due to rapid industrialization and urbanization in recent decades.The two major concerns of ambient air quality in China are particulate matter(PM)and tropospheric ozone(O3).With the implementation of air pollution prevention and control actions in the last five years,the PM pollution in China has been substantially reduced.In contrast,under the conditions of the urban air pollution complex,the elevated O3 levels in city clusters of eastern China,especially in warm seasons,have drawn increasing attention.Emissions of air pollutants and their precursors not only contribute to regional air quality,but also alter climate.Climate change in turn can change chemical processes,long-range transport,and local meteorology that influence air pollution.Compared to PM,less is known about O3 pollution and its climate effects over China.Here,we present a review of the main findings from the literature over the period 2011-18 with regard to the characteristics of O3 concentrations in China and the mechanisms that drive its interannual to decadal variations,aiming to identify robust conclusions that may guide decision-making for emissions control and to highlight critical knowledge gaps.We also review regional and global modeling studies that have investigated the impacts of tropospheric O3 on climate,as well as the projections of future tropospheric O3 owing to climate and/or emission changes.展开更多
By dint of grid information from 1948 to 2007,the summer monsoon in Afro-Asian area and the precipitation in corresponding atmosphere circulation situation during the strong and weak Afro-Asian monsoon period are stud...By dint of grid information from 1948 to 2007,the summer monsoon in Afro-Asian area and the precipitation in corresponding atmosphere circulation situation during the strong and weak Afro-Asian monsoon period are studied.The results suggest that the strong or weak Afro-Asian monsoon has pretty good corresponding relation with summer precipitation in Afro-Asian area.When summer monsoon weakens year after year,precipitation also decreases every year.展开更多
文摘Today＇s idea of the so-called fin-de-sibcle is still somewhat inexact and incomplete. This lack of precision originates from a deeply rooted methodological approach which consists of considering the respective developments of literature, art, and science in isolation, without paying attention to any interference or reciprocal contamination. This defective method also affects the overlaps and contacts between high culture and popular culture. Despite the progress made over recent years, there are few researchers who approach their objective with a real awareness of the complexity of a time period which saw the appearance of mass culture in the current sense and an unprecedented boom in scientific and technological development.1 To this end, the example of the great German philosopher Walter Benjamin and his studies on Paris during the 19th century----collected in the essays on the great French poet Charles Baudelaire and especially in the monumental and unfinished work The Arcades Project--is, without doubt, a model to follow. Taking the path suggested by Benjamin, this article sets out a revision of the novel Bruges-la-Morte （1892） by the Belgian writer Georges Rodenbach, considered one of the major exponents of thefin-de-sikcle decadence, which goes beyond the usual approach of a symbolist reading, by paying special attention to the frictions between literature and technology on one hand, and between literature and popular entertainment on the other.
文摘Sigalit Landau is an international sculpture,video,installation,and performance artist,born in Jerusalem,and raised also in the USA and the UK.The infernal main space in her installation“The Dining Hall”(2007,KW Institute for Contemporary Art,Berlin)is filled with images resembling human remains engaged in riotous consumption from huge iron pots,in physical circus-like tricks,and copulation,surrounded by huge fleshy-like constructions.While the immediate association may be that of an apocalyptic catastrophe in relation to the Holocaust,the reference is multifaceted,as this study seeks to show.There is a strong connotation of corporeality,gluttony,digestion,decay,and abjection combined with licentiousness,and a proximity between death and pleasure.This multiplicity of contexts is embedded in the term décadence,in its connection with Antiquity and mostly with ancient Rome,and calls to mind the Roman Menippean 1st century CE text Satyricon by Petronius.A comparative analysis of Landau’s installation in relation to Satyricon opens up the way to a broad interpretation,revealing much topical and conceptual parallelism that reveals Landau’s engagement with a kind of decadence typical to the contemporary condition and that of Israel in particular.A prominent feature of her installation is that of victimhood and its influence on the Israeli occupation policy and conduct.Consequently,Landau’s installation is interpreted here as an allegory of a particular state of mind,reflecting both decadence and victimhood.
文摘Till date,no study on trends in extreme sea surface temperature(SST)for different return periods has been done over the Gulf of Tonkin(GoT).Based on a 84-year(1940–2023)ERA5 Reanalysis data sets,this study for the first time,examined the spatio-temporal pattern in extreme SST for different return periods.Findings showed that more significant moderate to fast warming trends(0.1–0.16°C per decade(dec-1))only existed for the 2 year return period.Temporal trends in the 99th percentile SST are insignificant for all return periods.By using the linear regression method,the variability in extreme SST was obtained.Results showed that moderate warming trends dominated a large portion of GoT.Stronger trends,up to 0.018°C yr-1 are noticed near Guangdong,Haikou and southern Sanya in south China.Extreme SST exhibited a slow warming trend of 0.008°C per year(yr-1)all through the study years.The SST is most stable in most waters in the southern GoT and few waters surrounding Dongfang.Temporal warming rates of SST revealed that 1940–1958,1976–1994 and 2003–2012 were years of more coastal upwelling and could affect aquatic lives.The strongest warming rate of 0.07°C dec-1 occurred during 1994–2003.The GoT appeared warmer during spring.Spatial decadal variability of SST revealed that moderate warming trends occurred in few regions in the southern GoT and in larger portion of the central and northern GoT.The rise in SST between 1980 and 2020 in the GoT is not limited to increased anthropogenic activities.
基金supported by the National Natural Science Foundation of China(Grant Nos.42130604)the National Key Research and Development Program of China(Grant No.2023YFF0804704)+2 种基金the National Natural Science Foundation of China(Grant Nos.42105044)Swedish STINT(Grant No.CH2019-8377)the Priority Academic Program Development of Jiangsu Higher Education Institutions(Grant No.164320H116)。
文摘Since the mid-20th century,the Mongolian Plateau(MP)has experienced decadal droughts coupled with extreme heatwaves,severely affecting regional ecology and social development.However,the mechanisms behind these decadalscale compound heatwavedrought events remain debated.Here,using reconstructions and simulations from the Community Earth System Model Last Millennium Ensemble,we demonstrate that,over the last millennium,decadal droughts on the MP occurred under both warm and cold conditions,differing from recent compound heatwavedrought events.We found that by examining temperature changes during these drought periods,the distinct influences of external forcings and internal variability can be simply and effectively distinguished.Specifically,colddry events were primarily driven by volcanic eruptions that weakened the East Asian summer monsoon and midlatitude westerlies,reducing moisture transport to the MP.In contrast,warmdry events were predominantly induced by internal variability,notably the negative phase of the Atlantic Multidecadal Oscillation and the expansion of the Barents Sea ice extent.The recent extreme compound event was probably influenced by the combined effects of anthropogenic forcings and internal variability.These findings deepen our understanding of how external forcings and internal variability affect decadal drought events on the MP and highlight that recent compound events are unprecedented in the context of the last millennium.
基金The National Natural Science Foundation of China under contract Nos 42105052 and 42376016the Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai)under contract No.SML2024SP012.
文摘The Australian monsoon system plays a pivotal role in the tropical climate system by modulating the El Niño-Southern Oscillation(ENSO)development through multi-scale ocean-atmosphere interactions.This study identifies a significant decadal weakening of the Australian cross-equatorial flow intensity over the past two decades,attributed to the concurrent westward shift of the Australian High(AH)during austral winter.These decadal changes in the Australian monsoon reduce tropical Pacific atmospheric convection and the associated westerly wind anomalies over the centralto-western Pacific,which are crucial precursors for ENSO development.This process diminishes air-sea coupling feedback,including the thermocline feedback and the Ekman feedback,ultimately decreasing the strength of warm ENSO(El Niño)events.Using the Community Earth System Model,we confirm the close linkage between the Australian monsoon and ENSO on the decadal timescale.These findings provide new insights into the coupled relationship between ENSO and monsoon variability,offering a valuable framework for understanding ENSO’s longterm modulation and improving future climate predictions.
基金National Natural Science Foundation of China(42288101,42192564)Project of Ministry of Science and Technology of the People’s Republic of China(2020YFA0608802)Guangdong Major Project of Basic and Applied Basic Research(2020B0301030004)。
文摘El Niño is frequently followed by La Niña,while La Niña tends to sustain into the next year or even longer,exhibiting a notable phase transition asymmetry(TA)of El Niño-Southern Oscillation(ENSO).This study explores the potential influences of tropical Indian Ocean(TIO)decadal variability on TA based on a comparative analysis of the relationship between the TIO sea surface temperature anomalies(SSTA)and ENSO during different periods.Generally,the TIO SSTA strengthened TA before the 1980s,corresponding to a highly positive relationship between the whole TIO SSTA and ENSO.However,the weakening effect was exhibited after the 1980s when the correlation diminished.After the late 1990s,ENSO was only positively correlated with western TIO,with the westerly exhibit of the SSTA center leading to smaller impacts on TA.Moreover,TIO SSTA tends to weaken TA by promoting the transition efficiency of La Niña,while bringing little effect on that of El Niño.Physically,compared to the mid-1970s,TIO SSTA triggered westerly wind anomalies during the autumn and winter of the La Niña development phase in the central equatorial Pacific in the late 1990s,which sped up the decay of La Niña.It then regenerated westerly anomalies in the following winter,facilitating the development of El Niño.This study quantifies the impact of the TIO SSTA on TA in seasonal signals and investigates the decadal variability of such influence,aiming to further understand phase transition asymmetry and offer valuable insights for the prediction of multi-year La Niña.
基金supported by the National Key Research and Development Program of China(Grant No.2020YFA0608904)the International Partnership Program of the Chinese Academy of Sciences(Grant Nos.060GJHZ2023079GC and 134111KYSB20160031)+1 种基金supported by the Office of Science,U.S.Department of Energy(DOE)Biological and Environmental Research as part of the Regional and Global Model Analysis program area through the Water Cycle and Climate Extremes Modeling(WACCEM)scientific focus areaoperated for DOE by Battelle Memorial Institute under contract DE-AC05-76RL01830。
文摘The global monsoon system,encompassing the Asian-Australian,African,and American monsoons,sustains two-thirds of the world’s population by regulating water resources and agriculture.Monsoon anomalies pose severe risks,including floods and droughts.Recent research associated with the implementation of the Global Monsoons Model Intercomparison Project under the umbrella of CMIP6 has advanced our understanding of its historical variability and driving mechanisms.Observational data reveal a 20th-century shift:increased rainfall pre-1950s,followed by aridification and partial recovery post-1980s,driven by both internal variability(e.g.,Atlantic Multidecadal Oscillation)and external forcings(greenhouse gases,aerosols),while ENSO drives interannual variability through ocean-atmosphere interactions.Future projections under greenhouse forcing suggest long-term monsoon intensification,though regional disparities and model uncertainties persist.Models indicate robust trends but struggle to quantify extremes,where thermodynamic effects(warming-induced moisture rise)uniformly boost heavy rainfall,while dynamical shifts(circulation changes)create spatial heterogeneity.Volcanic eruptions and proposed solar radiation modification(SRM)further complicate predictions:tropical eruptions suppress monsoons,whereas high-latitude events alter cross-equatorial flows,highlighting unresolved feedbacks.The emergent constraint approach is booming in terms of correcting future projections and reducing uncertainty with respect to the global monsoons.Critical challenges remain.Model biases and sparse 20th-century observational data hinder accurate attribution.The interplay between natural variability and anthropogenic forcings,along with nonlinear extreme precipitation risks under warming,demands deeper mechanistic insights.Additionally,SRM’s regional impacts and hemispheric monsoon interactions require systematic evaluation.Addressing these gaps necessitates enhanced observational networks,refined climate models,and interdisciplinary efforts to disentangle multiscale drivers,ultimately improving resilience strategies for monsoon-dependent regions.
基金support from USA NSF Grant OPP2213875NASA Grant 80NSSC22K1707.
文摘In August 2024,the United Nations General Assembly adopted resolution 78/321 to declare the period from 2025 to 2034 as the“Decade of Action for Cryospheric Sciences”.This action was championed by the Republic of France and the Republic of Tajikistan,with support from over 30 member states,underscoring the urgent need for an international scientific collaboration to mitigate the far-reaching effects of cryospheric changes on ecosystems,water security,and global climate stability.A dedicated brainstorming session during the March 2025 celebrations in Paris convened over 1,000 policymakers,scientists,and stakeholders to outline the priorities for the Decade of Action.The session aimed to foster cross-border partnerships and strengthen the integration of cryospheric science into global climate adaptation strategies.Joint task force teams developed an integrated governance framework through discussions across five domains—scientific research,socioeconomic impacts,education,policy advocacy,and finance.The Decade of Action for Cryospheric Sciences represents a critical shift from observation to intervention,mobilizing global stakeholders to translate scientific consensus into concrete measures against cryosphere decline.The initiative responds to urgent calls from UNESCO and international partners for coordinated action on cryosphere preservation.
基金Supported by the National Natural Science Foundation of China(No.41905089)the Laoshan Laboratory(No.LSKJ202202404)+1 种基金the Startup Foundation for Introducing Talent of NUIST,Jiangsu Innovation Research Group(No.JSSCTD202346)the Undergraduates Innovation and Entrepreneurship Training Program of Jiangsu Province(No.202310300087Y)。
文摘Marine heatwaves(MHWs)have become increasingly frequent and persistent in the context of global warming and the related underlying mechanisms are strongly region-dependent.We employed the NOAA(National Oceanic and Atmospheric Administration)CRW(Coral Reef Watch)daily mean sea surface temperature dataset spanning from 1985 to 2022 to comprehensively analyze the fundamental attributes and evolving patterns of marine heatwaves in the offshore waters of China.Eight pronounced marine heatwaves from frequently affected sensitive regions were investigated to explore their formation mechanisms.The relationship between the occurrences of marine heatwave and large-scale climate mode in the region was explored.Results show that the western Pacific subtropical high plays an essential role in triggering marine heatwaves in Chinese offshore waters,with an anomalous downward shortwave radiation flux acting to warm the sea surface,which is remotely associated to the large-scale sea surface temperature state.Distinct mechanisms for the MHWs were identified in the northern and southern offshore waters of China.MHWs in high latitudes(such as the Bohai Sea and the Yellow Sea)mainly occur during the negative phase of the Pacific Decadal Oscillation(PDO),while those in low latitudes(such as the South China Sea)are more common in about 5-month lags behind the El Niño,for which we purposed a mechanism to describe the main differences in the formation of MHWs in China and discussed the related implications.
基金the University of Reading, funded by the UK–China Research and Innovation Partnership Fund through the Met Office Climate Science for Service Partnership (CSSP) China as part of the Newton Fundsupported by the National Natural Science Foundation of China (Grant Nos. 42030603 and 42175044)+1 种基金supported by CSSP-China. NPK was supported by an Independent Research Fellowship from the Natural Environment Research Council (Grant No. NE/L010976/1)supported by the National Centre for Atmospheric Science via the NERC/GCRF programme “Atmospheric hazards in developing countries: risk assessment and early warnings ” (ACREW)。
文摘The frequency and duration of observed concurrent hot and dry events(HDEs) over China during the growing season(April–September) exhibit significant decadal changes across the mid-1990s. These changes are characterized by increases in HDE frequency and duration over most of China, with relatively large increases over southeastern China(SEC), northern China(NC), and northeastern China(NEC). The frequency of HDEs averaged over China in the present day(PD,1994–2011) is double that in the early period(EP, 1964–81);the duration of HDEs increases by 60%. Climate experiments with the Met Office Unified Model(MetUM-GOML2) are used to estimate the contributions of anthropogenic forcing to HDE decadal changes over China. Anthropogenic forcing changes can explain 60%–70% of the observed decadal changes,suggesting an important anthropogenic influence on HDE changes over China across the mid-1990s. Single-forcing experiments indicate that the increase in greenhouse gas(GHG) concentrations dominates the simulated decadal changes,increasing the frequency and duration of HDEs throughout China. The change in anthropogenic aerosol(AA) emissions significantly decreases the frequency and duration of HDEs over SEC and NC, but the magnitude of the decrease is much smaller than the increase induced by GHGs. The changes in HDEs in response to anthropogenic forcing are mainly due to the response of climatological mean surface air temperatures. The contributions from changes in variability and changes in climatological mean soil moisture and evapotranspiration are relatively small. The physical processes associated with the response of HDEs to GHG and AA changes are also revealed.
基金jointly supported by the National Key Research and Development Program of China (Grant No.2018YFA0606403)the National Natural Science Foundation of China (Grant No.41790473)the Beijing Natural Science Foundation (8234068)。
文摘Observational analyses demonstrate that the Ural persistent positive height anomaly event(PAE) experienced a decadal increase around the year 2000, exhibiting a southward displacement afterward. These decadal variations are related to a large-scale circulation shift over the Eurasian Continent. The effects of underlying sea ice and sea surface temperature(SST) anomalies on the Ural PAE and the related atmospheric circulation were explored by Atmospheric Model Intercomparison Project(AMIP) experiments from the Coupled Model Intercomparison Project Phase 6 and by sensitivity experiments using the Atmospheric General Circulation Model(AGCM). The AMIP experiment results suggest that the underlying sea ice and SST anomalies play important roles. The individual contributions of sea ice loss in the Barents-Kara Seas and the SST anomalies linked to the phase transition of the Pacific Decadal Oscillation(PDO) and Atlantic Multidecadal Oscillation(AMO) are further investigated by AGCM sensitivity experiments isolating the respective forcings.The sea ice decline in Barents-Kara Seas triggers an atmospheric wave train over the Eurasian mid-to-high latitudes with positive anomalies over the Urals, favoring the occurrence of Ural PAEs. The shift in the PDO to its negative phase triggers a wave train propagating downstream from the North Pacific. One positive anomaly lobe of the wave train is located over the Ural Mountains and increases the PAE there. The negative-to-positive transition of the AMO phase since the late-1990s causes positive 500-h Pa height anomalies south of the Ural Mountains, which promote a southward shift of Ural PAE.
基金Supported by the National Natural Science Foundation of China(NSFC)(No.41976027)。
文摘The subtropical North and South Pacific Meridional Modes(NPMM and SPMM)are well known precursors of El Niño-Southern Oscillation(ENSO).However,relationship between them is not constant.In the early 1980,the relationship experienced an interdecadal transition.Changes in this connection can be attributed mainly to the phase change of the Pacific decadal oscillation(PDO).During the positive phase of PDO,a shallower thermocline in the central Pacific is responsible for the stronger trade wind charging(TWC)mechanism,which leads to a stronger equatorial subsurface temperature evolution.This dynamic process strengthens the connection between NPMM and ENSO.Associated with the negative phase of PDO,a shallower thermocline over southeastern Pacific allows an enhanced wind-evaporation-SST(WES)feedback,strengthening the connection between SPMM and ENSO.Using 35 Coupled Model Intercomparison Project Phase 6(CMIP6)models,we examined the NPMM/SPMM performance and its connection with ENSO in the historical runs.The great majority of CMIP6 models can reproduce the pattern of NPMM and SPMM well,but they reveal discrepant ENSO and NPMM/SPMM relationship.The intermodal uncertainty for the connection of NPMM-ENSO is due to different TWC mechanism.A stronger TWC mechanism will enhance NPMM forcing.For SPMM,few models can simulate a good relationship with ENSO.The intermodel spread in the relationship of SPMM and ENSO owing to SST bias in the southeastern Pacific,as WES feedback is stronger when the southeastern Pacific is warmer.
基金supported by the National Natural Science Foundation of China(Grant Nos.42120104001,42192563 and 42005010)the Hong Kong RGC General Research Fund 11300920.
文摘Under global warming,understanding the long-term variation in different types of heatwaves is vital for China’s preparedness against escalating heat stress.This study investigates dry and wet heatwave shifts in eastern China over recent decades.Spatial trend analysis displays pronounced warming in inland midlatitudes and the Yangtze River Valley,with increased humidity in coastal regions.EOF results indicate intensifying dry heatwaves in northern China,while the Yangtze River Valley sees more frequent dry heatwaves.On the other hand,Indochina and regions north of 25°N also experience intensified wet heatwaves,corresponding to regional humidity increases.Composite analysis is conducted based on different situations:strong,frequent dry or wet heatwaves.Strong dry heatwaves are influenced by anticyclonic circulations over northern China,accompanied by warming SST anomalies around the coastal midlatitudes of the western North Pacific(WNP).Frequent dry heatwaves are related to strong subsidence along with a strengthened subtropical high over the WNP.Strong and frequent wet heatwaves show an intensified Okhotsk high at higher latitudes in the lower troposphere,and a negative circumglobal teleconnection wave train pattern in the upper troposphere.Decaying El Niño SST patterns are observed in two kinds of wet heatwave and frequent dry heatwave years.Risk analysis indicates that El Niño events heighten the likelihood of these heatwaves in regions most at risk.As global warming continues,adapting and implementing mitigation strategies toward extreme heatwaves becomes crucial,especially for the aforementioned regions under significant heat stress.
文摘Background: Characterisation of cotton-based cropping systems is essential for understanding and improving cotton production in Côte d’Ivoire. The aim of this study was to determine the effects of cropping practices on seed cotton yields. A survey of a network of 600 growers in all the cotton-growing areas was carried out to gather information on the type of soil preparation (manual, harnessed and motorised), the sowing decade, the previous crop, the cotton variety, the sowing density, the date of fertilizer application (NPK and urea), the number of weeding operations, the number of insecticide treatments and, finally, the seedcotton yield. Results: The results showed that during the last cotton season (2023-2024), the sowing decades, crop precedents and a number of insecticide treatments had a highly significant effect on yield. Sowing in the first, second and third decade of June (1 to 10 June, 11 to 20 June and 21 to 30 June respectively). In addition, the best yields were obtained by growers who applied NPKSB base fertilizer and cover fertilizer (urea) within the sowing period at 10 days before sowing (0 - 10 days before sowing) and 45 - 60 days before sowing, respectively. In addition, better yields of close to 2 tons per hectare (1725 kg/ha) were observed among growers who applied a dozen insecticide treatments (eleven more than the six recommended by the research and development services). Conclusion: Further analysis will be carried out, taking into account parameters such as plot size, fertilizer doses (NPK and urea), climatic parameters (rainfall and temperature), agro-ecological zones and the physico-chemical parameters of the growers’ soils. With this in mind, the Ivorian cotton companies will be able to provide farmers with a decision-making tool to help them monitor cultivation operations and improve farm performance.
文摘The West African Monsoon (WAM) is characterized by strong decadal and multi-decadal variability and the impacts can be catastrophic for the local populations. One of the factors put forward to explain this variability involves the role of atmospheric dynamics, linked in particular to the Saharan Heat Low (SHL). This article addresses this question by comparing the sets of preindustrial control and historical simulation data from climate models carried out in the framework of the CMIP5 project and observations data over the 20<sup>th</sup> century. Through multivariate statistical analyses, it was established that decadal modes of ocean variability and decadal variability of Saharan atmospheric dynamics significantly influence decadal variability of monsoon precipitation. These results also suggest the existence of external anthropogenic forcing, which is superimposed on the decadal natural variability inducing an intensification of the signal in the historical simulations compared to preindustrial control simulations. We have also shown that decadal rainfall variability in the Sahel, once the influence of oceanic modes has been eliminated, appears to be driven mainly by the activity of the Arabian Heat Low (AHL) in the central Sahel, and by the structure of the meridional temperature gradient over the inter-tropical Atlantic in the western Sahel.
文摘Based on temperature data of meteorological stations from 1971 to 2008 in Tibet,the temporal and spatial variation of maximum andminimum temperature in Tibet was analyzed.The results showed that both maximum temperature andminimum temperature increased distinctly,the warming amplitude of winter was the highest among the four seasons,and next came spring.The increment ofminimum temperature was visibly over that of maximum temperature,particularlyminimum temperature in winter with significant increment.For spatial variation,maximum temperature in most stations increased except particular stations,while theminimum temperature in all stations rose.In addition,the space variation law ofminimum temperature,being more obvious thanminimum temperature,increased from southeast to northwest with different spatial changes in various seasons.From decadal variation,both maximum andminimum temperature appeared increase from 1970s to the first eight years in the 21st century,and the rise ofminimum temperature was significant greater than maximum temperature.The increase of maximum andminimum temperature was the highest from 2001 to 2008,whereas the lowest in 1970s.
基金supported by the National Natural Science Foundation of China(Grant Nos.91744311 and91544219)the National Key Research and Development Program of China(Grant No.2016YFA0600203)the National Natural Science Foundation of China(Grant No.41405138)
文摘China has been experiencing widespread air pollution due to rapid industrialization and urbanization in recent decades.The two major concerns of ambient air quality in China are particulate matter(PM)and tropospheric ozone(O3).With the implementation of air pollution prevention and control actions in the last five years,the PM pollution in China has been substantially reduced.In contrast,under the conditions of the urban air pollution complex,the elevated O3 levels in city clusters of eastern China,especially in warm seasons,have drawn increasing attention.Emissions of air pollutants and their precursors not only contribute to regional air quality,but also alter climate.Climate change in turn can change chemical processes,long-range transport,and local meteorology that influence air pollution.Compared to PM,less is known about O3 pollution and its climate effects over China.Here,we present a review of the main findings from the literature over the period 2011-18 with regard to the characteristics of O3 concentrations in China and the mechanisms that drive its interannual to decadal variations,aiming to identify robust conclusions that may guide decision-making for emissions control and to highlight critical knowledge gaps.We also review regional and global modeling studies that have investigated the impacts of tropospheric O3 on climate,as well as the projections of future tropospheric O3 owing to climate and/or emission changes.
文摘By dint of grid information from 1948 to 2007,the summer monsoon in Afro-Asian area and the precipitation in corresponding atmosphere circulation situation during the strong and weak Afro-Asian monsoon period are studied.The results suggest that the strong or weak Afro-Asian monsoon has pretty good corresponding relation with summer precipitation in Afro-Asian area.When summer monsoon weakens year after year,precipitation also decreases every year.
