How well must climate models agree with observations?The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.Observed Arctic sea-ice loss directly follows anthropogenic CO2 emission.Arctic: Uncertainties in methane link.Impact of Thermally Driven Turbulence on the Bottom Melting of IceRecovery mechanisms of Arctic summer sea iceThe CMIP6 Sea-Ice Model Intercomparison Project (SIMIP): understanding sea ice through climate-model simulationsPotential climatic transitions with profound impact on EuropeTemporal dynamics of ikaite in experimental sea iceClimate and carbon cycle changes from 1850 to 2100 in MPI-ESM simulations for the Coupled Model Intercomparison Project phase 5Arctic Sea Ice in a 1.5°C Warmer WorldThe prediction of surface temperature in the new seasonal prediction system based on the MPI-ESM coupled climate modelA 1-D modelling study of Arctic sea-ice salinityOn the Potential for Abrupt Arctic Winter Sea Ice LossTuning the climate of a global modelRetrievals of Arctic sea-ice volume and its trend significantly affected by interannual snow variabilityThe Trajectory Towards a Seasonally Ice-Free Arctic OceanVersion 2 of the EUMETSAT OSI SAF and ESA CCI Sea Ice Concentration Climate Data RecordsDrivers of Arctic Ocean warming in CMIP5 modelsReconciling estimates of the ratio of heat and salt fluxes at the ice-ocean interfaceStatistical indicators of Arctic sea-ice stability – prospects and limitationsCorrigendum to insights on past and future sea-ice evolution from combining observations and models [Glob. Planet. Change (2015) 119–132]Seasonal climate forecasts significantly affected by observational uncertainty of Arctic sea ice concentrationControlling high-latitude Southern Ocean convection in climate modelsInsights on past and future sea-ice evolution from combining observations and modelsOn the thermodynamics of melting sea ice versus melting freshwater iceAdvances in understanding and parameterization of small-scale physical processes in the marine Arctic climate system: a reviewInter-hemispheric asymmetry in the sea-ice response to volcanic forcing simulated by MPI-ESM (COSMOS-Mill)Sea-ice extent and its trend provide limited metrics of model performanceCorrigendum to "Advances in understanding and parameterization of small-scale physical processes in the marine Arctic climate system: a review" published in Atmos. Chem. Phys., 14, 9403–9450, 2014Anthropogenic influence on recent circulation-driven Antarctic sea ice changesBiogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea iceDrivers of variability in Arctic sea-ice drift speedTechnical Note: On the use of the mushy-layer Rayleigh number for the interpretation of sea-ice-core dataAssimilation of sea-ice concentration in a global climate model – physical and statistical aspectsArctic sea-ice evolution as modeled by Max Planck Institute for Meteorology's Earth system modelCharacteristics of the ocean simulations in the Max Planck Institute Ocean Model (MPIOM) the ocean component of the MPI-Earth system modelInsights into brine dynamics and sea ice desalination from a 1-D model study of gravity drainagePredictability of large interannual Arctic sea-ice anomaliesThe Transient versus the Equilibrium Response of Sea Ice to Global Warming
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