All Stories

  1. More rapid heating of Earth caused by changes in cloud over the ocean
  2. Quantifying the acceleration of multidecadal global sea surface warming driven by Earth’s energy imbalance
  3. Assessment of the global ocean heat content and North Atlantic heat transport over 1993–2020
  4. An Abrupt Decline in Global Terrestrial Water Storage and Its Relationship with Sea Level Change
  5. The 1921 European drought: impacts, reconstruction and drivers
  6. A Machine Learning Framework to Evaluate Vegetation Modeling in Earth System Models
  7. Influence of Meltwater from Labrador Sea ice and icebergs transported via Flemish Cap on the long-term North Atlantic Cold Anomaly
  8. Observational Assessment of Changes in Earth’s Energy Imbalance Since 2000
  9. Substantial cooling effect from aerosol-induced increase in tropical marine cloud cover
  10. Odden ice melt linked to Labrador Sea ice expansions and the Great Salinity Anomalies of 1970-1995
  11. Sea ice involved in pulses of cold, fresh sea water in the North Atlantic
  12. Droughts are blowing in the wind
  13. Significantly wetter or drier future conditions for one to two thirds of the world’s population
  14. An even drier future for the arid lands
  15. Scenario choice impacts carbon allocation projection at global warming levels
  16. Evaluating Vegetation Modeling in Earth System Models with Machine Learning Approaches
  17. Climate sensitivity controls global precipitation hysteresis in a changing CO2 pathway
  18. State of the Climate in 2022
  19. Amplified seasonal range in precipitation minus evaporation
  20. Emerging signals of climate change over Europe
  21. Changes in atmospheric moisture transport over tropical South America: an analysis under a climate change scenario
  22. Evaluating Vegetation Modelling in Earth System Models with Machine Learning Approaches
  23. Heat stored in the Earth system 1960–2020: where does the energy go?
  24. Choice of Forecast Scenario Impacts the Carbon Allocation at the Same Global Warming Levels
  25. Water remains the Achilles heel of climate models and climate change policies
  26. On the Effect of Historical SST Patterns on Radiative Feedback
  27. Heat stored in the Earth system 1960–2020: Where does the energy go?
  28. State of the Climate in 2021
  29. Interruption of the Gulf Stream in 2014 caused the 2014-16 North Atlantic Cold Fresh Anomaly and reciprocal warming/ salinification of the North American coastal region
  30. Global changes in atmospheric moisture since 1979
  31. Consistent Trends in Dry Spell Length in Recent Observations and Future Projections
  32. Worsening drought of Nile basin under shift in atmospheric circulation, stronger ENSO and Indian Ocean dipole
  33. Discrepancies in Simulated Ocean Net Surface Heat Fluxes over the North Atlantic
  34. The Complex and Spatially Diverse Patterns of Hydrological Droughts Across Europe
  35. Observation of the direct effect of aerosols in the South-East Atlantic at high temporal resolution from MSG/SEVIRI
  36. Global changes in water vapor 1979-2020
  37. The complex and spatially diverse patterns of hydrological droughts across Europe
  38. The Physical Climate at Global Warming Thresholds as Seen in the U.K. Earth System Model
  39. Contrasting response of hydrological cycle over land and ocean to a changing CO2 pathway
  40. The 1921 European drought: impacts, reconstruction and drivers
  41. Emerging new climate extremes over Europe
  42. Global Climate
  43. The role of teleconnection patterns in the variability and trends of growing season indices across Europe
  44. Future Changes in Wet and Dry Season Characteristics in CMIP5 and CMIP6 simulations
  45. The 1921 European drought: Impacts, reconstruction and drivers
  46. Aerosol-forced AMOC changes in CMIP6 historical simulations.
  47. The Diurnal Cycle of Precipitation: A Comparison of State-of-the-Art IMERG Observations, CMIP6 Models and ERA5 Reanalysis
  48. Global-scale changes in Earth’s energy budget and implications for the water cycle
  49. Anthropogenic intensification of short-duration rainfall extremes
  50. Cocoa plant productivity in West Africa under climate change: a modelling and experimental study
  51. Advances in understanding large-scale responses of the water cycle to climate change
  52. Advances in understanding large-scale responses of the water cycle to climate change
  53. Observations of planetary heating since the 1980s from multiple independent datasets
  54. Observed variability of intertropical convergence zone over 1998—2018
  55. Variability in the global energy budget and transports 1985–2017
  56. Aerosol‐Forced AMOC Changes in CMIP6 Historical Simulations
  57. Advances in understanding large‐scale responses of the water cycle to climate change
  58. Aerosol-forced AMOC changes in CMIP6 historical simulations.
  59. Global surface energy and water cycle variability 2001-2011 from satellite data
  60. The Diurnal Cycle of Precipitation: A Comparison of State-of-the-Art Observations and Models
  61. New Generation of Climate Models Track Recent Unprecedented Changes in Earth's Radiation Budget Observed by CERES
  62. Changes in atmospheric shortwave absorption as important driver of dimming and brightening
  63. Atmospheric precursors for intense summer rainfall over the United Kingdom
  64. Seasonal Changes in the North Atlantic Cold Anomaly: The Influence of Cold Surface Waters From Coastal Greenland and Warming Trends Associated With Variations in Subarctic Sea Ice Cover
  65. Evaluation of Five Satellite Top-of-Atmosphere Albedo Products over Land
  66. The impact of air–sea coupling and ocean biases on the seasonal cycle of southern West African precipitation
  67. Rainfall decline over Eastern Africa linked to temporarily shorter wet seasons
  68. Later Wet Seasons with More Intense Rainfall over Africa under Future Climate Change
  69. Climatic effects of explosive volcanic eruptions between 1979 and 2015
  70. Publisher Correction: Critical Southern Ocean climate model biases traced to atmospheric model cloud errors
  71. Characterizing the Radiative Effect of Rain Using a Global Ensemble of Cloud Resolving Simulations
  72. Critical Southern Ocean climate model biases traced to atmospheric model cloud errors
  73. The INTENSE project: using observations and models to understand the past, present and future of sub-daily rainfall extremes
  74. Unrealistic Increases in Wind Speed Explain Reduced Eastern Pacific Heat Flux in Reanalyses
  75. Identification of deficiencies in seasonal rainfall simulated by CMIP5 climate models
  76. State of the Climate in 2016
  77. Evaluation of satellite and reanalysis-based global net surface energy flux and uncertainty estimates
  78. Strong constraints on aerosol–cloud interactions from volcanic eruptions
  79. A new, long-term daily satellite-based rainfall dataset for operational monitoring in Africa
  80. Surface flux and ocean heat transport convergence contributions to seasonal and interannual variations of ocean heat content
  81. A multisatellite climatology of clouds, radiation, and precipitation in southern West Africa and comparison to climate models
  82. Interannual variability in the summertime hydrological cycle over European regions
  83. Contrasting fast precipitation responses to tropospheric and stratospheric ozone forcing
  84. Revisiting trends in wetness and dryness in the presence of internal climate variability and water limitations over land
  85. Diagnosing links between atmospheric moisture and extreme daily precipitation over the UK
  86. Recent observed and simulated changes in precipitation over Africa
  87. Combining satellite observations and reanalysis energy transports to estimate global net surface energy fluxes 1985-2012
  88. The DACCIWA Project: Dynamics–Aerosol–Chemistry–Cloud Interactions in West Africa
  89. Metrics for linking emissions of gases and aerosols to global precipitation changes
  90. Observational constraints on atmospheric and oceanic cross-equatorial heat transports: revisiting the precipitation asymmetry problem in climate models
  91. Atmospheric rivers do not explain UK summer extreme rainfall
  92. Metrics for linking emissions of gases and aerosols to global precipitation changes
  93. Changes in Earth's heating rate since 1960 in observations and simulations
  94. Extension of the TAMSAT Satellite-Based Rainfall Monitoring over Africa and from 1983 to Present
  95. The 30 year TAMSAT African Rainfall Climatology And Time series (TARCAT) data set
  96. Current changes in Earth's heating rate
  97. Salinity changes in the World Ocean since 1950 in relation to changing surface freshwater fluxes
  98. Comparing Tropical Precipitation Simulated by the Met Office NWP and Climate Models with Satellite Observations*
  99. Quantifying present and projected future atmospheric moisture transports onto land
  100. Have greenhouse gases intensified the contrast between wet and dry regions?
  101. Future changes in atmospheric rivers and their implications for winter flooding in Britain
  102. Observed and simulated precipitation responses in wet and dry regions 1850–2100
  103. Assessment of intercalibration methods for satellite microwave humidity sounders
  104. Modelling the diurnal cycle of tropical convection across the ‘grey zone’
  105. Improving a convection-permitting model simulation of a cold air outbreak
  106. Physically Consistent Responses of the Global Atmospheric Hydrological Cycle in Models and Observations
  107. Climate Warming–Related Strengthening of the Tropical Hydrological Cycle
  108. The detection of atmospheric rivers in atmospheric reanalyses and their links to British winter floods and the large-scale climatic circulation
  109. Diagnosing atmosphere–land feedbacks in CMIP5 climate models
  110. Co-variation of temperature and precipitation in CMIP5 models and satellite observations
  111. Multisatellite observed responses of precipitation and its extremes to interannual climate variability
  112. Observed changes in top-of-the-atmosphere radiation and upper-ocean heating consistent within uncertainty
  113. Evaluation of satellite-based and model re-analysis rainfall estimates for Uganda
  114. Winter floods in Britain are connected to atmospheric rivers
  115. The Role of Water Vapour in Earth’s Energy Flows
  116. Energetic Constraints on Precipitation Under Climate Change
  117. Changes in water vapor transports of the ascending branch of the tropical circulation
  118. Combining satellite data and models to estimate cloud radiative effect at the surface and in the atmosphere
  119. Clear-sky biases in satellite infrared estimates of upper tropospheric humidity and its trends
  120. Regime dependent changes in global precipitation
  121. Motivation, rationale and key results from the GERBILS Saharan dust measurement campaign
  122. Variability in the summer season hydrological cycle over the Atlantic-Europe region 1979-2007
  123. Examination of long-wave radiative bias in general circulation models over North Africa during May-July
  124. Evaluation of the model representation of the evolution of convective systems using satellite observations of outgoing longwave radiation
  125. Summertime precipitation variability over Europe and its links to atmospheric dynamics and evaporation
  126. Anticipated changes in the global atmospheric water cycle
  127. Current changes in tropical precipitation
  128. A case study of the radiative forcing of persistent contrails evolving into contrail-induced cirrus
  129. How robust are observed and simulated precipitation responses to tropical ocean warming?
  130. Examination of Relationships between Clear-Sky Longwave Radiation and Aspects of the Atmospheric Hydrological Cycle in Climate Models, Reanalyses, and Observations
  131. Overview of observations from the RADAGAST experiment in Niamey, Niger: Meteorology and thermodynamic variables
  132. Atmospheric Warming and the Amplification of Precipitation Extremes
  133. Modeled and observed atmospheric radiation balance during the West African dry season: Role of mineral dust, biomass burning aerosol, and surface albedo
  134. Contrasting interannual variability of atmospheric moisture over Europe during cold and warm seasons
  135. Evaluation of the Met Office global forecast model using Geostationary Earth Radiation Budget (GERB) data
  136. Large discrepancy between observed and simulated precipitation trends in the ascending and descending branches of the tropical circulation
  137. Observations of the diurnal cycle of outgoing longwave radiation from the Geostationary Earth Radiation Budget instrument
  138. Improved simulation of water vapour and clear-sky radiation using 24-hour forecasts from ERA40
  139. Observations of the impact of a major Saharan dust storm on the atmospheric radiation balance
  140. Variability in clear-sky longwave radiative cooling of the atmosphere
  141. The ERA-40 re-analysis
  142. Exploitation of Geostationary Earth Radiation Budget data using simulations from a numerical weather prediction model: Methodology and data validation
  143. The Geostationary Earth Radiation Budget Project
  144. Water vapor variability in the tropics and its links to dynamics and precipitation
  145. Can desert dust explain the outgoing longwave radiation anomaly over the Sahara during July 2003?
  146. Simulation of the Earth's radiation budget by the European Centre for Medium-Range Weather Forecasts 40-year reanalysis (ERA40)
  147. Evaluation of moisture in the Hadley Centre climate model using simulations of HIRS water-vapour channel radiances
  148. Simulations of the effects of interannual and decadal variability on the clear-sky outgoing long-wave radiation spectrum
  149. Inconsistencies between satellite estimates of longwave cloud forcing and dynamical fields from reanalyses
  150. Diagnostic analysis of atmospheric moisture and clear-sky radiative feedback in the Hadley Centre and Geophysical Fluid Dynamics Laboratory (GFDL) climate models
  151. Analysis of moisture variability in the European Centre for Medium-Range Weather Forecasts 15-year reanalysis over the tropical oceans
  152. Can current climate model forcings explain the spatial and temporal signatures of decadal OLR variations?