D. Nissenbaum, R. Sarafian, E. Windwer, E. Tas, C. C. Womack, S. S. Brown, Y. Rudich
{"title":"Deriving ozone and PM pollution vertical profiles using lightweight, cost-effective sensors and deep learning","authors":"D. Nissenbaum, R. Sarafian, E. Windwer, E. Tas, C. C. Womack, S. S. Brown, Y. Rudich","doi":"10.1038/s41612-025-01155-0","DOIUrl":"https://doi.org/10.1038/s41612-025-01155-0","url":null,"abstract":"<p>We developed and deployed a drone-based air pollution measurement system composed of cost-effective and lightweight sensors. The system generates high-resolution vertical profiles of various pollutants. During campaigns conducted in 2023, we observed a diurnal cycle of ozone and analyzed extreme particulate matter events, including biomass burning and a rapid dust storm. Our analysis reveals consistent ozone depletion near the surface at night, an advection-related “knee” in the ozone vertical profile at ~100 meters, and significant differences in aerosol size distributions between background, biomass burning, and dust events. An ensemble of autoencoder-based deep learning models with prediction heads identified ground data and a novel combined factor as the most predictive variables for the ozone vertical profiles. These findings demonstrate the value of mobile vertical profiling systems for understanding pollutant distributions and tropospheric dynamics, including the distinction between local and regional ozone influences, with potential applications for air quality monitoring.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"1 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144712341","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":"Enhanced shortwave absorption by water vapor increases effective climate sensitivity via accelerated AMOC recovery","authors":"Doseok Lee, Hanjun Kim, Sarah M. Kang","doi":"10.1038/s41612-025-01169-8","DOIUrl":"https://doi.org/10.1038/s41612-025-01169-8","url":null,"abstract":"<p>Climate models exhibit substantial inter-model spread in climate sensitivity, typically attributed to uncertainty in cloud feedbacks. In contrast, the influence of clear-sky shortwave absorption (SWA) remains underexplored, despite its substantial uncertainty. Using a single-model framework, we systematically perturb SWA and impose CO₂ quadrupling on distinct mean states that differ in SWA, allowing assessment of its impact on both the mean climate and the CO₂-driven response. Enhanced SWA reduces surface shortwave radiation, leading to Arctic cooling. Under higher SWA, CO₂ forcing drives increased advection of colder Arctic air into the subpolar North Atlantic, enhancing turbulent heat loss and facilitating AMOC recovery. This accelerated recovery amplifies warming in the subpolar North Atlantic, strengthens lapse rate and shortwave cloud feedbacks, and ultimately increases climate sensitivity over time. These findings reveal a previously overlooked pathway by which clear-sky SWA modulates long-term climate feedback, underscoring the need to better constrain SWA in climate models.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"68 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144712342","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}
Hao Li, Damián Insua-Costa, Akash Koppa, João Lucas Geirinhas, Jessica Keune, Chiara M. Holgate, Francina Dominguez, Victoria M. H. Deman, Adriaan J. Teuling, Diego G. Miralles
{"title":"Observational evidence of compensatory influences of deforestation on downwind precipitation in Brazilian breadbaskets","authors":"Hao Li, Damián Insua-Costa, Akash Koppa, João Lucas Geirinhas, Jessica Keune, Chiara M. Holgate, Francina Dominguez, Victoria M. H. Deman, Adriaan J. Teuling, Diego G. Miralles","doi":"10.1038/s41612-025-01152-3","DOIUrl":"https://doi.org/10.1038/s41612-025-01152-3","url":null,"abstract":"<p>Stable and predictable wet-season rainfall is crucial for soybean production in Brazil. However, climate and land-use changes, particularly Amazon deforestation, have increased rainfall variability in the region in recent decades. Here, we investigate long-term growing-season rainfall changes over two major soybean breadbaskets in Brazil from the perspective of atmospheric moisture transport. Utilising a novel moisture tracking framework based on a Lagrangian model guided by observations, we identify moisture source regions where evaporation contributed to rainfall over these breadbaskets. Furthermore, we quantify the relative contributions of source evaporation versus atmospheric (thermo)dynamics changes to downwind rainfall variability. Our results indicate that deforestation-induced evaporation declines have negatively impacted downwind rainfall in the breadbasket regions. However, strengthened circulation, evidenced by increased water vapour transport and low-level wind speeds consistent with decreased tree cover, has enhanced moisture transport from upwind regions (including Amazonia and the Atlantic Ocean) to the Brazilian soybean breadbaskets. This highlights the compensatory effects of deforestation on rainfall through decreased evaporation and altered atmospheric (thermo)dynamics, and how these effects may influence downwind soybean productivity in South America. Further understanding these interactions is critical for developing land management strategies to mitigate the agricultural impacts of climate change in the region.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"32 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144684635","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 global survey of stratospheric gravity waves generated by tropical cyclones","authors":"Xu Wang, Yuan Wang, Lifeng Zhang, Yun Zhang, Jiping Guan","doi":"10.1038/s41612-025-01172-z","DOIUrl":"https://doi.org/10.1038/s41612-025-01172-z","url":null,"abstract":"<p>The stratospheric gravity waves generated by tropical cyclones (TC-SGWs) are useful for the monitoring of tropical cyclones (TCs) and are also important for the gravity-wave parameterization in numerical models, as they represent a distinct type of gravity waves. Previous studies on TC-SGWs have not characterized TC-SGW global distribution and corresponding local structure related to the background wind. Here we show the global distribution of the TC-SGWs based on 21 years of Atmospheric Infrared Sounder observations, and reveal three global hotspots of the waves as the North Atlantic-Northeast Pacific, the Northwest Pacific, and the South Pacific-Southern Indian region. We also characterize the local structure of the three hotspots and find that although displaying diverse anisotropic structures, they are all shaped by the combination of filtering and refraction effects of the background wind. Our findings provide a guide for global TC-SGW hotspots and demonstrate the contributions of the background wind, which can further provide a preliminary guide for TC monitoring through satellite observations of TC-SGWs.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"92 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144694125","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}
Damaris Y. T. Tan, Mathew R. Heal, Massimo Vieno, David S. Stevenson, Stefan Reis, Eiko Nemitz
{"title":"Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation","authors":"Damaris Y. T. Tan, Mathew R. Heal, Massimo Vieno, David S. Stevenson, Stefan Reis, Eiko Nemitz","doi":"10.1038/s41612-025-01150-5","DOIUrl":"https://doi.org/10.1038/s41612-025-01150-5","url":null,"abstract":"<p>Open biomass burning has major impacts on the Earth system, including on air quality via the emission of primary fine particulate matter (PM<sub>2.5</sub>). Its effect on secondary inorganic PM<sub>2.5</sub> formation is comparatively little investigated. Simulations with the EMEP MSC-W WRF atmospheric chemistry transport model reveal that global biomass burning emissions lead to elevated annual mean ammonium nitrate (NH<sub>4</sub>NO<sub>3</sub>) concentrations in densely populated regions where biomass burning mostly does not occur. These regions include eastern USA, northwestern Europe, the Indo-Gangetic Plain and eastern China, where NH<sub>4</sub>NO<sub>3</sub> conditional on biomass burning emissions constitutes between 29% and 51% of the annual mean PM<sub>2.5</sub> conditional on biomass burning emissions. Biomass burning emissions of CO, NO<sub><i>x</i></sub> (NO and NO<sub>2</sub>) and volatile organic compounds perturb the HO<sub><i>x</i></sub> (OH and HO<sub>2</sub>) cycle globally, such that there is increased oxidation of anthropogenic NO<sub><i>x</i></sub> to HNO<sub>3</sub>. This results in additional contributions to local-scale secondary NH<sub>4</sub>NO<sub>3</sub> in areas with high emissions of anthropogenic NO<sub><i>x</i></sub> and NH<sub>3</sub>. These teleconnections increase, by up to a factor of two, the contribution of biomass burning emissions to long-term PM<sub>2.5</sub> concentrations, which measurements alone cannot identify as an impact of biomass burning activity. This may become relatively more important as anthropogenic sources of PM<sub>2.5</sub> are reduced and as the wildfire component of biomass burning increases under climate change.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"4 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144677900","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":"Enhanced El Niño predictability from climate mode interactions","authors":"Tamás Bódai","doi":"10.1038/s41612-025-01171-0","DOIUrl":"https://doi.org/10.1038/s41612-025-01171-0","url":null,"abstract":"<p>The conceptual XRO model (XROM) introduced recently by Zhao et al. (Nature, 2024) is extended here by including state dependence of the external noise forcing on ENSO as well as a seasonal modulation of both the additive and state-dependent parts of the forcing. These features of the forecast model, the XDROM+, require the use of Maximum Likelihood Estimation for parameter inference, which is much more costly than fitting the XROM to data by linear regression via matrix inversion. Yet, it pays, yielding the best ENSO forecast skill yet. I also make a few points of caveat via introducing and discussing four concepts, those of the apparent, theoretical maximum, climatological, and true prediction skills. Most importantly, I explain that (i) the true skill—unlike the apparent skill determined from historical data—cannot be defined by a correlation coefficient and demonstrate that (ii) the said two types of skill do not correlate across possible realisations of the statistical process generated by the XDROM+.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"5 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144684638","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}
Shangfeng Chen, Wen Chen, Renguang Wu, Bin Yu, Hans-F Graf, Zhibiao Wang, Xi Cao, Yuqiong Zheng
{"title":"Asymmetric impacts of Arctic sea ice anomalies on El Niño-Southern Oscillation","authors":"Shangfeng Chen, Wen Chen, Renguang Wu, Bin Yu, Hans-F Graf, Zhibiao Wang, Xi Cao, Yuqiong Zheng","doi":"10.1038/s41612-025-01168-9","DOIUrl":"https://doi.org/10.1038/s41612-025-01168-9","url":null,"abstract":"<p>The impact of Arctic sea ice concentration (SIC) anomalies on the global climate system has received considerable attention in recent decades. Observations and model simulations indicate that winter Arctic SIC anomalies in the Greenland-Barents Seas significantly influence on the El Niño-Southern Oscillation (ENSO). However, whether this influence is symmetric remains unclear. Here, we demonstrate that the influence of SIC anomalies on the subsequent ENSO is asymmetric. An increase in SIC significantly affects the development of El Niño, whereas a decrease in SIC has only a weak influence on La Niña. Specifically, a winter SIC increase in the Greenland-Barents Seas induces deep Arctic cooling, which triggers an atmospheric wave train propagating to the subtropical North Pacific. The associated subtropical cyclonic anomaly leads to North Pacific Meridional Mode-like sea surface temperature (SST) warming in spring, which extends to the tropical Pacific via the wind-evaporation-SST feedback in the following summer and subsequently enhances El Niño development by tropical air-sea interaction processes. In contrast, a winter SIC decrease is accompanied by shallow Arctic warming, which is insufficient to generate an atmospheric wave train to modify the subtropical North Pacific oceanic and atmospheric states, and thus has a weak influence on the La Niña development. Further analysis suggests that the asymmetric impacts of Arctic sea ice anomalies on subtropical North Pacific air-sea conditions and ENSO events may also be partly due to differences in the atmospheric mean state between high and low SIC years. This study highlights the asymmetric impact of Arctic SIC anomalies on ENSO and tropical climate, emphasizing the need to consider these asymmetries when assessing global climate responses to Arctic sea ice variability.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"24 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144678151","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}
Alex Borowiak, Andrew D. King, Josephine R. Brown, Tilo Ziehn
{"title":"Revised estimates of temperature changes under net zero CO2 emissions","authors":"Alex Borowiak, Andrew D. King, Josephine R. Brown, Tilo Ziehn","doi":"10.1038/s41612-025-01148-z","DOIUrl":"https://doi.org/10.1038/s41612-025-01148-z","url":null,"abstract":"<p>It is critical that climate changes beyond net zero are well understood to inform policymaking. Here we present a new estimate of post-abrupt net zero CO<sub>2</sub> temperature changes using a method that filters for variability on multiple timescales. Our findings indicate that 50 years after abrupt emission cessation, the multi-model median temperature change is −0.19 °C, with a range spanning from −0.44 °C to 0.04 °C, which is cooler than previous estimates.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"37 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144664549","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}
Pablo Fernández-Castillo, Teresa Losada, Belén Rodríguez-Fonseca, Diego García-Maroto, Elsa Mohino, Luis Durán
{"title":"Multidecadal variability of the ENSO early-winter teleconnection to Europe and implications for seasonal forecasting","authors":"Pablo Fernández-Castillo, Teresa Losada, Belén Rodríguez-Fonseca, Diego García-Maroto, Elsa Mohino, Luis Durán","doi":"10.1038/s41612-025-01160-3","DOIUrl":"https://doi.org/10.1038/s41612-025-01160-3","url":null,"abstract":"<p>The impacts of El Niño-Southern Oscillation (ENSO) on the North Atlantic and European sector (NAE) climate are season-dependent and, in some cases, not linear and/or not stationary. Previous studies have found multidecadal variability in ENSO teleconnections to NAE in certain seasons, relating it to changes in the background state. However, the stationarity of the teleconnection and its surface impacts in Europe during early winter remain largely unexplored, a gap intended to be addressed in this study. The observational analysis reveals changes in the teleconnection impacts and mechanisms over recent decades. These changes have strong implications for the assessment of seasonal predictability, hence the performance of the SEAS5 seasonal prediction model is analysed. While SEAS5 does not accurately capture the observed non-stationarity, it displays pronounced multidecadal changes in forecast skill. This implies the emergence of windows of opportunity for seasonal forecasting, where predictability may be higher than initially expected.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"109 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144664566","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}
Florian E. Roemer, Stefan A. Buehler, Kaah P. Menang
{"title":"How to think about the clear-sky shortwave water vapor feedback","authors":"Florian E. Roemer, Stefan A. Buehler, Kaah P. Menang","doi":"10.1038/s41612-025-01144-3","DOIUrl":"https://doi.org/10.1038/s41612-025-01144-3","url":null,"abstract":"<p>Earth’s climate feedback quantifies the response of Earth’s energy budget to temperature changes and thus determines climate sensitivity. The climate feedback is largely controlled by water vapor which absorbs both longwave radiation emitted by Earth and shortwave radiation from the Sun. For the clear-sky shortwave water vapor feedback <i>λ</i><sub>SW</sub>, a gap remains between process understanding and estimates from comprehensive climate models. Therefore, we present a hierarchy of simple models for <i>λ</i><sub>SW</sub>. We show that <i>λ</i><sub>SW</sub> is proportional to the change with temperature in the square of atmospheric transmissivity that depends on the atmospheric concentration of water vapor and its ability to absorb shortwave radiation. The global mean <i>λ</i><sub>SW</sub> is well captured by a simple analytical model that approximates the strong spectral variations in water vapor absorption, whereas its temperature dependence results from spectral details in water vapor absorption. With this study, we expand the conceptual understanding of an important but understudied feedback component.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":"61 1","pages":""},"PeriodicalIF":9.0,"publicationDate":"2025-07-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144664615","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}