All Stories

  1. Impacts of the Hunga Tonga-Hunga Ha'apai Eruption: Insights from the SOCOLv4 ESM about past and future
  2. Sensitivity and linearity of surface temperature response to solar irradiation changes
  3. Global impacts of an extreme Solar Particle Event under different geomagnetic field strengths
  4. Simplified parameterization of GCR/SEP-produced 10Be using CCM SOCOL-AERv2-BE
  5. Preface to Monitoring the Earth Radiation Budget and Its Implication to Climate Simulations: Recent Advances and Discussions
  6. Stratospherically induced circulation changes under the extreme conditions of the no-Montreal-Protocol scenario
  7. Annual Cycle of Total Ozone Content in the Southern Hemisphere Using the Chemistry-Climate Model SOCOLv3
  8. Weakening of springtime Arctic ozone depletion with climate change
  9. Mesospheric Ozone Depletion Depending on Different Levels of Geomagnetic Disturbances and Seasons
  10. Future Climate Under CMIP6 Solar Activity Scenarios
  11. Evaluating the Uncertainties of the Global Atmospheric Sulphur Budget in a Multi-Model Framework
  12. Modelling of atmospheric transport of SEP-induced cosmogenic 10Be  using CCM SOCOL-AER2-BE
  13. Montreal Protocol's impact on the ozone layer and climate
  14. Stratosphere-troposphere coupling under the extreme conditions of the No-Montreal-Protocol scenario
  15. Energetic Particle Precipitation Influence on Tidal Variations of Thermosphere Parameters in September 2017
  16. Montreal Protocol's impact on the ozone layer and climate
  17. Preface to Monitoring the Earth Radiation Budget and its Implication to Climate Simulations: Recent Advances and Discussions
  18. The future ozone trends in changing climate simulated with SOCOLv4
  19. Weakening of springtime Arctic ozone depletion with climate change
  20. Numerical modelling of relative contribution of planetary waves to the atmospheric circulation
  21. Stratospherically induced tropospheric circulation changes under the extreme conditions of the No-Montreal-Protocol scenario
  22. Atmospheric Response to EEP during Geomagnetic Disturbances
  23. Numerical modeling of relative contribution of planetary waves to the atmospheric circulation
  24. Analysis of Factors Affecting the Interannual Variability of Antarctic Ozone
  25. Atmospheric Chemical Composition Response to Energetic Electron Precipitations
  26. The historical ozone trends simulated with the SOCOLv4 and their comparison with observations and reanalyses
  27. The future ozone trends in changing climate simulated with SOCOLv4
  28. Montreal Protocol's impact on the ozone layer and climate
  29. Zonal Mean Distribution of Cosmogenic Isotope (7Be, 10Be, 14C, and 36Cl) Production in Stratosphere and Troposphere
  30. Measurements and Modelling of Total Ozone Columns near St. Petersburg, Russia
  31. The historical ozone trends simulated with the SOCOLv4 and their comparison with observations and reanalysis
  32. On the Possibility of Modeling the IMF By-Weather Coupling through GEC-Related Effects on Cloud Droplet Coalescence Rate
  33. September 2017 Solar Flares Effect on the Middle Atmosphere
  34. Exceptional middle latitude electron precipitation detected by balloon observations: implications for atmospheric composition
  35. An Inventory of Global Rocket Launch Emissions and Projected Near-Future Impacts on Stratospheric Ozone
  36. Atmospheric response to solar flares, coronal mass ejections and magnetospheric energetic particle precipitation during September 2017
  37. Heppa III Intercomparison Experiment on Electron Precipitation Impacts: 2. Model‐Measurement Intercomparison of Nitric Oxide (NO) During a Geomagnetic Storm in April 2010
  38. Application of CCM SOCOL-AERv2-BE to cosmogenic beryllium isotopes: description and validation for polar regions
  39. Modeling the Sulfate Aerosol Evolution After Recent Moderate Volcanic Activity, 2008–2012
  40. Iodine chemistry in the chemistry–climate model SOCOL-AERv2-I
  41. Exceptional middle latitude electron precipitation detected by balloon observations: implications for atmospheric composition
  42. Modeling the Sulfate Aerosol Evolution after Recent Moderate Volcanic Activity, 2008-2012
  43. Iodine chemistry in the chemistry-climate model SOCOL-AERv2-iodine
  44. Chemistry-climate model SOCOL-AERv2-BEv1 with the cosmogenic Beryllium-7 isotope cycle
  45. Modelling aspects of the sulfate aerosol evolution after recent volcanic activity
  46. The response of stratospheric ozone and dynamics to changes in atmospheric oxygen
  47. Atmospheric production and transport of 7Be activity by cosmic rays: Modelling with the chemistry-climate model SOCOLv3.0 and comparison with direct measurements
  48. The response of mesospheric H<sub>2</sub>O and CO to solar irradiance variability in models and observations
  49. The response of mesospheric H<sub>2</sub>O and CO to solar irradiance variability in the models and observations
  50. Study of the dependence of long-term stratospheric ozone trends on local solar time
  51. Preface: Ozone Evolution in the Past and Future
  52. Revisited Reference Solar Proton Event of 23 February 1956: Assessment of the Cosmogenic‐Isotope Method Sensitivity to Extreme Solar Events
  53. Ozone Layer Evolution in the Early 20th Century
  54. A machine learning examination of hydroxyl radical differences among model simulations for CCMI-1
  55. Attribution of Chemistry-Climate Model Initiative (CCMI) ozone radiative flux bias from satellites
  56. The representation of ionospheric potential in the global chemistry-climate model SOCOL
  57. Inter-model comparison of global hydroxyl radical (OH) distributions and their impact on atmospheric methane over the 2000–2016 period
  58. The dependence of four-peak longitudinal structure of the tropical electric field on the processes in the lower atmosphere and geomagnetic field configuration
  59. Spectra of high energy electron precipitation and atmospheric ionization rates retrieval from balloon measurements
  60. The effect of atmospheric nudging on the stratospheric residual circulation in chemistry–climate models
  61. Improved tropospheric and stratospheric sulfur cycle in the aerosol–chemistry–climate model SOCOL-AERv2
  62. Clear-sky ultraviolet radiation modelling using output from the Chemistry Climate Model Initiative
  63. Reactive nitrogen (NO<sub><i>y</i></sub>) and ozone responses to energetic electron precipitation during Southern Hemisphere winter
  64. Global EAGLE Model as a Tool for Studying the Influence of the Atmosphere on the Electric Field in the Equatorial Ionosphere
  65. Evaluating the Relationship between Interannual Variations in the Antarctic Ozone Hole and Southern Hemisphere Surface Climate in Chemistry–Climate Models
  66. Improved tropospheric and stratospheric sulfur cycle in the aerosol-chemistry-climate model SOCOL-AERv2
  67. Supplementary material to "Improved tropospheric and stratospheric sulfur cycle in the aerosol-chemistry-climate model SOCOL-AERv2"
  68. Tidal and Planetary Waves in the Lower Thermosphere and Ionosphere Simulated with the EAGLE Model for the January 2009 Sudden Stratospheric Warming Conditions
  69. The Upper Stratospheric Solar Cycle Ozone Response
  70. The influence of mixing on the stratospheric age of air changes in the 21st century
  71. Ionization of the Polar Atmosphere by Energetic Electron Precipitation Retrieved From Balloon Measurements
  72. Identification of the mechanisms responsible for anomalies in the tropical lower thermosphere/ionosphere caused by the January 2009 sudden stratospheric warming
  73. Impact of middle range energy electron precipitations on polar winter ozone losses
  74. Reactive nitrogen (NO<sub><i>y</i></sub>) and ozone responses to energetic electron precipitation during Southern Hemisphere winter
  75. Tropospheric ozone in CCMI models and Gaussian process emulation to understand biases in the SOCOLv3 chemistry–climate model
  76. Erratum to: Ionospheric Effects of the Sudden Stratospheric Warming in 2009: Results of Simulation with the First Version of the EAGLE Model
  77. Supplementary material to "The influence of mixing on stratospheric circulation changes in the 21st century"
  78. The influence of mixing on stratospheric circulation changes in the 21st century
  79. Revisiting the Mystery of Recent Stratospheric Temperature Trends
  80. No robust evidence of future changes in major stratospheric sudden warmings: a multi-model assessment from CCMI
  81. The representation of solar cycle signals in stratospheric ozone – Part 2: Analysis of global models
  82. Stratospheric aerosol evolution after Pinatubo simulated with a coupled size-resolved aerosol–chemistry–climate model, SOCOL-AERv1.0
  83. Revised historical solar irradiance forcing
  84. Effect of Precipitating Energetic Particles on the Ozone Layer and Climate
  85. Global Variations in Critical Frequency of the F2 Layer in Various Models of Solar EUV Radiation
  86. Ionospheric Effects of the Sudden Stratospheric Warming in 2009: Results of Simulation with the First Version of the EAGLE Model
  87. Supplementary material to "Tropospheric ozone in CCMI models and Gaussian emulation to understand biases in the SOCOLv3 chemistry-climate model"
  88. Tropospheric ozone in CCMI models and Gaussian emulation to understand biases in the SOCOLv3 chemistry-climate model
  89. Estimates of ozone return dates from Chemistry-Climate Model Initiative simulations
  90. Stratospheric Injection of Brominated Very Short-Lived Substances: Aircraft Observations in the Western Pacific and Representation in Global Models
  91. Large-scale tropospheric transport in the Chemistry–Climate Model Initiative (CCMI) simulations
  92. Quantifying the effect of mixing on the mean age of air in CCMVal-2 and CCMI-1 models
  93. The Response of the Ozone Layer to Quadrupled CO2 Concentrations
  94. Tropospheric jet response to Antarctic ozone depletion: An update with Chemistry-Climate Model Initiative (CCMI) models
  95. Implications of potential future grand solar minimum for ozone layer and climate
  96. Multi-model comparison of the volcanic sulfate deposition from the 1815 eruption of Mt. Tambora
  97. Evidence for a continuous decline in lower stratospheric ozone offsetting ozone layer recovery
  98. Ozone sensitivity to varying greenhouse gases and ozone-depleting substances in CCMI-1 simulations
  99. Size-Resolved Stratospheric Aerosol Distributions after Pinatubo Derived from a Coupled Aerosol-Chemistry-Climate Model
  100. Stratospheric ozone loss over the Eurasian continent induced by the polar vortex shift
  101. Impacts of Mt Pinatubo volcanic aerosol on the tropical stratosphere in chemistry–climate model simulations using CCMI and CMIP6 stratospheric aerosol data
  102. The PMIP4 contribution to CMIP6 – Part 3: The last millennium, scientific objective, and experimental design for the PMIP4 <i>past1000</i> simulations
  103. Deriving Global OH Abundance and Atmospheric Lifetimes for Long-Lived Gases: A Search for CH3 CCl3 Alternatives
  104. Formaldehyde in the Tropical Western Pacific: Chemical Sources and Sinks, Convective Transport, and Representation in CAM-Chem and the CCMI Models
  105. Reconciling differences in stratospheric ozone composites
  106. Implications of potential future grand solar minimum for ozone layer and climate
  107. On the aliasing of the solar cycle in the lower stratospheric tropical temperature
  108. Chemistry-climate model simulations of the Mt. Pinatubo eruption using CCMI and CMIP6 stratospheric aerosol data
  109. Ozone sensitivity to varying greenhouse gases and ozone-depleting substances in CCMI simulations
  110. Supplementary material to "Ozone sensitivity to varying greenhouse gases and ozone-depleting substances in CCMI simulations"
  111. Tropical circulation and precipitation response to ozone depletion and recovery
  112. Atmospheric impacts of the strongest known solar particle storm of 775 AD
  113. Reconciling differences in stratospheric ozone composites
  114. HEPPA-II model–measurement intercomparison project: EPP indirect effects during the dynamically perturbed NH winter 2008–2009
  115. Review of the global models used within phase 1 of the Chemistry–Climate Model Initiative (CCMI)
  116. Decadal to multi-decadal scale variability of Indian summer monsoon rainfall in the coupled ocean-atmosphere-chemistry climate model SOCOL-MPIOM
  117. Modeling of the middle atmosphere response to 27-day solar irradiance variability
  118. An upper-branch Brewer–Dobson circulation index for attribution of stratospheric variability and improved ozone and temperature trend analysis
  119. Multidecadal variations of the effects of the Quasi-Biennial Oscillation on the climate system
  120. Response of the AMOC to reduced solar radiation – the modulating role of atmospheric chemistry
  121. Foreword: Special issue on “Effects of the solar wind and interplanetary disturbances on the Earth's atmosphere and climate”
  122. The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate
  123. The role of methane in projections of 21st century stratospheric water vapour
  124. Review of the global models used within the Chemistry-Climate Model Initiative (CCMI)
  125. Supplementary material to "Review of the global models used within the Chemistry-Climate Model Initiative (CCMI)"
  126. The Model Intercomparison Project on the climatic response to Volcanic forcing (VolMIP): experimental design and forcing input data for CMIP6
  127. A mid-latitude stratosphere dynamical index for attribution of stratospheric variability and improved ozone and temperature trend analysis
  128. The role of methane in projections of 21st century stratospheric water vapour
  129. Evaluation of the inter-annual variability of stratospheric chemical composition in chemistry-climate models using ground-based multi species time series
  130. Multidecadal Variations of the Effects of the Quasi-Biennial Oscillation on the Climate System
  131. Supplementary material to "Multidecadal Variations of the Effects of the Quasi-Biennial Oscillation on the Climate System"
  132. Evaluation of simulated photolysis rates and their response to solar irradiance variability
  133. Solar irradiance observations with PREMOS filter radiometers on the PICARD mission: In-flight performance and data release
  134. High solar cycle spectral variations inconsistent with stratospheric ozone observations
  135. Application of the models of the middle and upper atmosphere to simulation of total electron content perturbations caused by the 2009 stratospheric warming
  136. Solar signals in CMIP-5 simulations: effects of atmosphere-ocean coupling
  137. A perturbed parameter model ensemble to investigate Mt. Pinatubo's 1991 initial sulfur mass emission
  138. Southward shift of the northern tropical belt from 1945 to 1980
  139. The impacts of volcanic aerosol on stratospheric ozone and the Northern Hemisphere polar vortex: separating radiative-dynamical changes from direct effects due to enhanced aerosol heterogeneous chemistry
  140. Energetic Particle Influence on the Earth’s Atmosphere
  141. Drivers of the tropospheric ozone budget throughout the 21st century under the medium-high climate scenario RCP 6.0
  142. The impact of volcanic aerosols on stratospheric ozone and the Northern Hemisphere polar vortex: separating radiative from chemical effects under different climate conditions
  143. Solar signals in CMIP-5 simulations: the ozone response
  144. Solar signals in CMIP-5 simulations: the stratospheric pathway
  145. A perturbed parameter model ensemble to investigate 1991 Mt Pinatubo's initial sulfur mass emission
  146. Global atmospheric sulfur budget under volcanically quiescent conditions: Aerosol‐chemistry‐climate model predictions and validation
  147. Drivers of the tropospheric ozone budget throughout the 21st century under the medium-high climate scenario RCP 6.0
  148. Evaluation of the ECHAM family radiation codes performance in the representation of the solar signal
  149. The stratospheric response to external factors based on MERRA data using linear multivariate linear regression analysis
  150. Variability of Sun-like stars: reproducing observed photometric trends
  151. Impact of solar versus volcanic activity variations on tropospheric temperatures and precipitation during the Dalton Minimum
  152. The coupled atmosphere-chemistry-ocean model SOCOL-MPIOM
  153. Multimodel estimates of atmospheric lifetimes of long-lived ozone-depleting substances: Present and future
  154. Northern hemispheric winter warming pattern after tropical volcanic eruptions: Sensitivity to the ozone climatology
  155. Climate and chemistry effects of a regional scale nuclear conflict
  156. A global historical ozone data set and prominent features of stratospheric variability prior to 1979
  157. The SOCOL version 3.0 chemistry–climate model: description, evaluation, and implications from an advanced transport algorithm
  158. Impact of a potential 21st century “grand solar minimum” on surface temperatures and stratospheric ozone
  159. Influence of the sunspot cycle on the Northern Hemisphere wintertime circulation from long upper-air data sets
  160. The role of the solar irradiance variability in the evolution of the middle atmosphere during 2004-2009
  161. Climate and chemistry effects of a regional scale nuclear conflict
  162. Role of external factors in the evolution of the ozone layer and stratospheric circulation in 21st century
  163. Montreal Protocol Benefits simulated with CCM SOCOL
  164. The place of the Sun among the Sun-like stars
  165. Supplementary material to "A global historical ozone data set and signatures of El Niño and the 11-yr solar cycle"
  166. Uncertainties in modelling the stratospheric warming following Mt. Pinatubo eruption
  167. Volcanic forcing for climate modeling: a new microphysics-based dataset covering years 1600–present
  168. Reconstruction of daily erythemal UV radiation values for the last century – The benefit of modelled ozone
  169. The sensitivity of stratospheric ozone changes through the 21st century to N<sub>2</sub>O and CH<sub>4</sub>
  170. Influence of a Carrington-like event on the atmospheric chemistry, temperature and dynamics
  171. The benefit of modeled ozone data for the reconstruction of a 99‐year UV radiation time series
  172. The effectiveness of N2O in depleting stratospheric ozone
  173. Detection of Solar Rotational Variability in the Large Yield RAdiometer (LYRA) 190 – 222 nm Spectral Band
  174. Influence of the Precipitating Energetic Particles on Atmospheric Chemistry and Climate
  175. Observed and simulated time evolution of HCl, ClONO<sub>2</sub>, and HF total column abundances
  176. Signature of the 27-day solar rotation cycle in mesospheric OH and H<sub>2</sub>O observed by the Aura Microwave Limb Sounder
  177. The nature of Arctic polar vortices in chemistry-climate models
  178. Principal Possibility of the Successful Nowcast and Short-Term Forecast in the Middle Atmosphere Based on the Observed UV Irradiance
  179. Modeling of the atmospheric response to a strong decrease of the solar activity
  180. Improved predictability of the troposphere using stratospheric final warmings
  181. Composition changes after the "Halloween" solar proton event: the High Energy Particle Precipitation in the Atmosphere (HEPPA) model versus MIPAS data intercomparison study
  182. Projections of UV radiation changes in the 21st century: impact of ozone recovery and cloud effects
  183. Simulation of changes in global ozone and atmospheric dynamics in the 21st century with the chemistry-climate model SOCOL
  184. Climate change projections and stratosphere–troposphere interaction
  185. Evaluation of radiation scheme performance within chemistry climate models
  186. Influence of Galactic Cosmic Rays on atmospheric composition and dynamics
  187. A new approach to the long-term reconstruction of the solar irradiance leads to large historical solar forcing
  188. Multimodel climate and variability of the stratosphere
  189. Sensitivity of the Earth’s middle atmosphere to short-term solar variability and its dependence on the choice of solar irradiance data set
  190. The atmospheric effects of October 2003 solar proton event simulated with the chemistry–climate model SOCOL using complete and parameterized ion chemistry
  191. Attribution of observed changes in stratospheric ozone and temperature
  192. Multimodel assessment of the factors driving stratospheric ozone evolution over the 21st century
  193. Evidence for changes in stratospheric transport and mixing over the past three decades based on multiple data sets and tropical leaky pipe analysis
  194. Chemistry-climate model simulations of spring Antarctic ozone
  195. Decline and recovery of total column ozone using a multimodel time series analysis
  196. Multimodel assessment of the upper troposphere and lower stratosphere: Tropics and global trends
  197. Multimodel assessment of the upper troposphere and lower stratosphere: Extratropics
  198. Impact of stratospheric ozone on Southern Hemisphere circulation change: A multimodel assessment
  199. The potential to narrow uncertainty in projections of stratospheric ozone over the 21st century
  200. Multi-model assessment of stratospheric ozone return dates and ozone recovery in CCMVal-2 models
  201. Chemistry–Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes
  202. Anthropogenic forcing of the Northern Annular Mode in CCMVal-2 models
  203. Review of the formulation of present-generation stratospheric chemistry-climate models and associated external forcings
  204. NLTE solar irradiance modeling with the COSI code
  205. Radiative transfer with scattering for domain-decomposed 3D MHD simulations of cool stellar atmospheres
  206. Stratosphere‐troposphere coupling and annular mode variability in chemistry‐climate models
  207. Quantitative assessment of Southern Hemisphere ozone in chemistry-climate model simulations
  208. A model of the impact of solar proton events on the ionic and gaseous composition of the mesosphere
  209. Geomagnetic activity and polar surface air temperature variability
  210. The impact of geoengineering aerosols on stratospheric temperature and ozone
  211. Variability of large-scale atmospheric circulation indices for the northern hemisphere during the past 100 years
  212. Evaluating how photochemistry and transport determine stratospheric inorganic chlorine in coupled chemistry‐climate models
  213. The Impact of Stratospheric Ozone Recovery on Tropopause Height Trends
  214. Diurnal changes in middle atmospheric H2O and O3: Observations in the Alpine region and climate models
  215. Stratospheric winter climate response to ENSO in three chemistry‐climate models
  216. Coupled chemistry climate model simulations of the solar cycle in ozone and temperature
  217. The Impact of Stratospheric Ozone Recovery on the Southern Hemisphere Westerly Jet
  218. Response of the Earth’s Atmosphere to the Solar Irradiance Variability
  219. Simulation of the stratospheric ozone and temperature response to the solar irradiance variability during sun rotation cycle
  220. Assessment of temperature, trace species, and ozone in chemistry‐climate model simulations of the recent past
  221. Influence of solar wind on ozone and circulation in the middle atmosphere: A model study
  222. LYRA, a solar UV radiometer on Proba2
  223. Retrieval of stratospheric NO2vertical profiles from ground‐based zenith‐sky DOAS measurements: Results for the MANTRA 1998 field campaign
  224. Atmospheric response to NOy source due to energetic electron precipitation
  225. Assessment of the ozone and temperature variability during 1979–1993 with the chemistry-climate model SOCOL
  226. Influence of solar 11-year variability on chemical composition of the stratosphere and mesosphere simulated with a chemistry-climate model
  227. Modeling of the Joule heating influence on the circulation and ozone concentration in the middle atmosphere
  228. An assessment of the statistical significance of the total ozone changes simulated with global chemical transport model MEZON
  229. Parameterization of the heating in the middle stratosphere due to solar wind-induced electric currents
  230. Chemical and dynamical response to the 11‐year variability of the solar irradiance simulated with a chemistry‐climate model
  231. Atmospheric response to the observed increase of solar UV radiation from solar minimum to solar maximum simulated by the University of Illinois at Urbana‐Champaign climate‐chemistry model
  232. Assessing 1D Atmospheric Solar Radiative Transfer Models: Interpretation and Handling of Unresolved Clouds
  233. Climate/chemistry effects of the Pinatubo volcanic eruption simulated by the UIUC stratosphere/troposphere GCM with interactive photochemistry
  234. The University of Illinois, Urbana‐Champaign three‐dimensional stratosphere‐troposphere general circulation model with interactive ozone photochemistry: Fifteen‐year control run climatology
  235. Assessment of the effect of the Montreal Protocol on atmospheric ozone
  236. Geographical Distributions of Temperature Change for Scenarios of Greenhouse Gas and Sulfur Dioxide Emissions
  237. Description and performance of the UIUC 24‐layer stratosphere/troposphere general circulation model
  238. Plume transformation index (PTI) of the subsonic aircraft exhausts and their dependence on the external conditions
  239. Radiative forcing by volcanic aerosols from 1850 to 1994
  240. The UIUC three‐dimensional stratospheric chemical transport model: Description and evaluation of the simulated source gases and ozone
  241. Lightning production of NOX and ozone
  242. Three-dimensional simulations of ozone in the stratosphere and comparison with UARS data
  243. Calculation of longwave radiation fluxes in atmospheres