Kai Qie, Wenshou Tian, Jianchun Bian, Fei Xie, Dan Li
{"title":"Weakened Asian summer monsoon anticyclone related to increased anthropogenic aerosol emissions in recent decades","authors":"Kai Qie, Wenshou Tian, Jianchun Bian, Fei Xie, Dan Li","doi":"10.1038/s41612-025-01026-8","DOIUrl":"https://doi.org/10.1038/s41612-025-01026-8","url":null,"abstract":"<p>The Asian summer monsoon anticyclone (ASMA) traps pollutants from South and East Asia elevated by deep convection, which profoundly influences the atmospheric composition and hence stratospheric chemical processes. Here, we identified a significant weakening of the ASMA in the layer of 70–200 hPa during 1958–2020 and found that the change in anthropogenic aerosol emissions was the dominant external forcing responsible for this weakening trend. Significant increases in anthropogenic aerosol emissions over South and East Asia and decreased aerosol emissions over Central Asia led to a decreased meridional temperature gradient at low-latitudes and an increased meridional temperature gradient at mid-latitudes in the troposphere over the Eurasian continent, resulting in a weakened ASMA. The results based on satellite observations and numerical simulations indicated that the weakened ASMA may affect the spatial distribution of CO and water vapor in the UTLS over Asian summer monsoon region.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"3 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143819346","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}
Shoshiro Minobe, Erik Behrens, Kirsten L. Findell, Norman G. Loeb, Benoit Meyssignac, Rowan Sutton
{"title":"Global and regional drivers for exceptional climate extremes in 2023-2024: beyond the new normal","authors":"Shoshiro Minobe, Erik Behrens, Kirsten L. Findell, Norman G. Loeb, Benoit Meyssignac, Rowan Sutton","doi":"10.1038/s41612-025-00996-z","DOIUrl":"https://doi.org/10.1038/s41612-025-00996-z","url":null,"abstract":"<p>Climate records have been broken with alarming regularity in recent years, but the events of 2023–2024 were exceptional even when accounting for recent climatic trends. Here we quantify these events across multiple variables and show how excess energy accumulation in the Earth system drove the exceptional conditions. Key factors were the positive decadal trend in Earth’s Energy Imbalance (EEI), persistent La Niña conditions beginning in 2020, and the switch to El Niño in 2023. Between 2022 and 2023, the heating from EEI was over 75% larger than during the onset of similar recent El Niño events. We show further how regional processes shaped distinct patterns of record-breaking sea surface temperatures in individual ocean basins. If the recent trend in EEI is maintained, we argue that natural fluctuations such as ENSO cycles will increasingly lead to amplified, record-breaking impacts, with 2023–2024 serving as a glimpse of future climate extremes.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"51 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143789998","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}
Jiale Lou, Youngji Joh, Thomas L. Delworth, Liwei Jia
{"title":"Identifying source of predictability for vapor pressure deficit variability in the southwestern United States","authors":"Jiale Lou, Youngji Joh, Thomas L. Delworth, Liwei Jia","doi":"10.1038/s41612-025-01028-6","DOIUrl":"https://doi.org/10.1038/s41612-025-01028-6","url":null,"abstract":"<p>Atmospheric vapor pressure deficit (VPD) measures the difference between saturation vapor pressure and actual vapor pressure, and its variability is closely related to fire activity in the western United States (US). Here, we assess the forecast skill of monthly VPD variability using a state-of-the-art dynamical forecast system and statistical predictions, such as the persistence forecast and model-analog forecasts. In the model-analog framework, we select analog states resembling the observed initial conditions from the model space, and the subsequent evolution of those initial model-analogs yields forecast ensembles. Dynamical forecasts demonstrate skillful predictions of VPD variability in the western US, exceeding the persistence forecast skill, which indicates additional sources of VPD predictability within the climate system. To quantify the contribution of different climate variables to VPD prediction, we develop a weighted model-analog forecast and evaluate its skill in comparison to VPD-only and unweighted forecasts. Our findings suggest that sea surface temperature is a critical source of VPD predictability over the western US. The optimally weighted model-analog exhibits forecast skill for VPD variability comparable to that of the dynamical forecast system.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"57 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143789728","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}
Bernd Kärcher, Fabian Hoffmann, Adam B. Sokol, Blaž Gasparini, Milena Corcos, Eric Jensen, Rachel Atlas, Aurélien Podglajen, Hugh Morrison, Albert Hertzog, Riwal Plougonven, Kamal Kant Chandrakhar, Wojciech W. Grabowski
{"title":"Dissecting cirrus clouds: navigating effects of turbulence on homogeneous ice formation","authors":"Bernd Kärcher, Fabian Hoffmann, Adam B. Sokol, Blaž Gasparini, Milena Corcos, Eric Jensen, Rachel Atlas, Aurélien Podglajen, Hugh Morrison, Albert Hertzog, Riwal Plougonven, Kamal Kant Chandrakhar, Wojciech W. Grabowski","doi":"10.1038/s41612-025-01024-w","DOIUrl":"https://doi.org/10.1038/s41612-025-01024-w","url":null,"abstract":"<p>Turbulent air motions determine the local environment in which cloud ice crystals form. Homogeneous freezing of aqueous solution droplets is the most fundamental pathway to nucleate ice crystals in cirrus. Lack of knowledge about the role of turbulence in cirrus ice formation limits our understanding of how uncertainties in small-scale cloud processes affect the climatological radiative effect of cirrus. Here we shed first light on how turbulent fluctuations in temperature and supersaturation interact with probabilistic homogeneous freezing. We show that spatial model resolution substantially below 1–10 m is needed to properly simulate homogeneous freezing events. Importantly, microscale turbulence generates large variability in nucleated ice crystal number concentrations. Previous research ascribed this variability to mesoscale dynamical forcing due to gravity waves alone. The turbulence-generated microphysical variability has macrophysical implications. The wide range of predicted cloud radiative heating anomalies in anvil cirrus due to turbulence-ice nucleation interactions, comparable to typical mean values, is potentially large enough to affect the response of tropical cirrus cloud systems to global warming. Our results have ramifications for the multiscale modeling of cirrus clouds and the interpretation of in situ measurements.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"183 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143784833","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}
Gerd A. Folberth, Chris D. Jones, Fiona M. O’Connor, Nicola Gedney, Paul T. Griffiths, Andy J. Wiltshire
{"title":"Drivers of persistent changes in the global methane cycle under aggressive mitigation action","authors":"Gerd A. Folberth, Chris D. Jones, Fiona M. O’Connor, Nicola Gedney, Paul T. Griffiths, Andy J. Wiltshire","doi":"10.1038/s41612-024-00867-z","DOIUrl":"https://doi.org/10.1038/s41612-024-00867-z","url":null,"abstract":"<p>To achieve the Paris climate agreement goals, methane (CH<sub>4</sub>) emission mitigation plays a key role. Therefore, a better understanding of the global methane cycle is indispensable. Here we simulate the global methane cycle fully interactively from 1850 to 2100 with a strong mitigation action scenario (SSP1-2.6) post 2014. We show that the atmospheric methane burden largely recovers to early 20th-century levels, while wetland methane emissions follow a persistent upward trend from 166 Tg(CH<sub>4</sub>) yr<sup>–1</sup> at pre-industrial to 221 Tg(CH<sub>4</sub>) yr<sup>–1</sup> in 2100. The methane lifetime decreases from 9.3 to 7.3 years over the 1850–2100 period. We identify net primary productivity as the main driver behind the wetland methane trend with <i>R</i><sup>2</sup> = 0.7. This implies that important components of the methane cycle (wetland methane, methane lifetime) are subject to Earth system feedbacks, potentially impacting any prospective methane mitigation action. Therefore, methane mitigation strategies will need to consider feedbacks in the Earth system.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"59 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143782422","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":"Seasonal predictability of tropical cyclone frequency over the western North Pacific by a large-ensemble climate model","authors":"Takeshi Doi, Tadao Inoue, Tomomichi Ogata, Masami Nonaka","doi":"10.1038/s41612-025-00995-0","DOIUrl":"https://doi.org/10.1038/s41612-025-00995-0","url":null,"abstract":"<p>We assessed the seasonal prediction skill of tropical cyclone (TC) frequency over the western North Pacific by the large-ensemble SINTEX-F dynamical system. Although the prediction skills were limited, the correlation skill for the June–August prediction issued in early May was statistically significant around Okinawa and Taiwan. Particularly, the high TC activity in summer 2018 was well predicted. We found that the 2018 positive Indian Ocean Dipole (IOD) contributed to the predictability by the dynamical prediction system: suppressed convection in the eastern tropical Indian Ocean enhanced divergent wind from the eastern tropical Indian Ocean to the Okinawa and Taiwan areas. This helped to generate low pressure in the target area, which was favorable to the TC activity. The IOD contributions to the predictability were also seen in the correlation analyses in 1982–2022 and some case studies in 1994 and 1998. This could be useful for actionable early warnings.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"32 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143766351","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":"Driving factors and photochemical impacts of Cl2 in coastal atmosphere of Southeast China","authors":"Gaojie Chen, Xiaolong Fan, Ziyi Lin, Xiaoting Ji, Ziying Chen, Lingling Xu, Jinsheng Chen","doi":"10.1038/s41612-025-01022-y","DOIUrl":"https://doi.org/10.1038/s41612-025-01022-y","url":null,"abstract":"<p>The elevated levels of molecular chlorine (Cl<sub>2</sub>) have been observed both during the daytime or nighttime, yet the key drivers influencing Cl<sub>2</sub> formation remain unclear. In this study, we observed the distinct daytime and nighttime peaks of Cl<sub>2</sub> in coastal atmosphere of Southeast China. Field observations combined with machine learning revealed that daytime Cl<sub>2</sub> generation was driven by nitrate (especially ammonium nitrate) photolysis, and aerosol iron photochemistry, while the N<sub>2</sub>O<sub>5</sub> uptake on aerosols containing chloride contributed to nighttime Cl<sub>2</sub> formation. Around noon, alkane oxidation rates by Cl radicals generated from Cl<sub>2</sub> photolysis surpassed those of OH radicals, leading to a 44% increment in RO<sub>2</sub> radical levels and a 42% enhancement in net O<sub>3</sub> production rates. This study offers new insights into the production and loss processes of Cl<sub>2</sub> in the tropospheric atmosphere, emphasizing its significance in coastal photochemical pollution.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"15 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143758306","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}
Jesse Norris, Stefan Rahimi, Lei Huang, Benjamin Bass, Chad W. Thackeray, Alex Hall
{"title":"Uncertainty of 21st Century western U.S. snowfall loss derived from regional climate model large ensemble","authors":"Jesse Norris, Stefan Rahimi, Lei Huang, Benjamin Bass, Chad W. Thackeray, Alex Hall","doi":"10.1038/s41612-025-01002-2","DOIUrl":"https://doi.org/10.1038/s41612-025-01002-2","url":null,"abstract":"<p>The western United States is dependent on winter snowfall over its major mountain ranges, which gradually melts each year, serving as a natural reservoir for water resources. In a future warmer climate, much of this snowfall could be replaced by rain, making it more challenging to capture and store water. In this study, we utilize an ensemble of dynamically downscaled simulations forced by 14 global climate models (GCMs). These GCMs project wildly different futures, in terms of both temperature and precipitation change, producing significant uncertainty in snowfall projections. Here we exploit the robust statistics of the downscaled ensemble, and diagose the sensitivity of end-of-century snowfall loss across the region to both warming and regional wetting/drying in the driving GCM. The windward slopes of the Sierra Nevada and Cascades are particularly sensitive to warming (losing ~ 15% annual snowfall per degree warming), with little influence of precipitation. By contrast, snowfall loss in the inter-mountain west is less sensitive to warming (~ 5% K<sup>−1</sup>), but is significantly offset/exacerbated by precipitation changes (~ 0.5% snow per 1% precipitation). Combining such sensitivities with the warming and regional precipitation signals in the full CMIP6 ensemble, we can fully quantify likely snowfall loss and its uncertainty at any location, for any emissions scenario. We find that the western U.S. as a whole will lose 34 ± 8% of its total volumetric snowfall by end-of-century under the high-emissions SSP3-7.0 scenario, but 25 ± 6% and 17 ± 6% under the lower-emissions SSP2-4.5 and SSP1-2.6 scenarios.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"22 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143758307","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":"Diverse NPMM conditions deviate the 2023/24 El Niño from the 1997/1998 and 2015/2016 extreme El Niño events","authors":"Yong-Fu Lin, Mengyan Chen, Lingling Liu, Fei Zheng, Ruiqiang Ding, Xin Wang, Chau-Ron Wu, Min-Hui Lo, Huang-Hsiung Hsu, Jiepeng Chen, Ting-Hui Lee, Jin-Yi Yu","doi":"10.1038/s41612-025-01013-z","DOIUrl":"https://doi.org/10.1038/s41612-025-01013-z","url":null,"abstract":"<p>The 2023/24 El Niño commenced with an exceptionally large warm water volume in the equatorial western Pacific, comparable to the extreme 1997/98 and 2015/16 events, but did not develop into a super El Niño. This study highlights the critical role of contrasting Northern Pacific Meridional Mode (NPMM) conditions in this divergence. Warm NPMM conditions during the 1997/98 and 2015/16 events created a positive zonal sea surface temperature (SST) gradient in the equatorial western-central Pacific and enhanced Madden-Julian Oscillation (MJO) propagation, driving sustained westerly wind bursts (WWBs) and downwelling Kelvin waves that intensified both events. In contrast, the cold NPMM during 2023/24 induced a negative SST gradient and suppressed MJO activity, resulting in weaker WWBs and limited eastward wave activity, preventing the event from reaching super El Niño intensity. A 2,200-year CESM1 pre-industrial simulation corroborates these observational findings, underscoring the importance of NPMM interference in improving El Niño intensity predictions.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"1 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143745659","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":"Mechanism driving stronger tropical cyclones in cooler autumn than the hottest summer","authors":"Vineet Kumar Singh, Hye-Ji Kim, Il-Ju Moon","doi":"10.1038/s41612-025-01008-w","DOIUrl":"https://doi.org/10.1038/s41612-025-01008-w","url":null,"abstract":"<p>Warmer sea surface temperatures (SSTs) increase evaporation, convection, and latent heat release in the atmosphere, which favors tropical cyclone (TC) intensification and ultimately leads to stronger storms. However, in this study, we find that the intensity of TCs in the western North Pacific, called typhoons, is on average higher in the colder autumn season than during the warmer summer season. The primary reason for this is that despite the decrease in SSTs during autumn, the deepening of the ocean mixed layer increase the TC heat potential and reduces storm-induced SST cooling. Atmospheric thermodynamic conditions also become more favorable to TC intensification in autumn than in summer due to higher heat and sensible heat fluxes in autumn resulting from the increased air-sea temperature/moist differences at the interface. Lastly, during autumn, the TC’s track shifts towards the equator as a result the TCs in this season travel over more favourable ocean condition which also contribute in the TC intensification. This finding will enhance the understanding of the mechanisms causing seasonal differences in TC intensity, which will aid in TC seasonal forecasting and risk assessment.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"23 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143737039","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}