10.1594/PANGAEA.973301Hoppmann, MarioMarioHoppmann0000-0003-1294-9531Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, BremerhavenScholz, DanielDanielScholzNicolaus, MarcelMarcelNicolaus0000-0003-0903-1746Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, BremerhavenPANGAEA2024autonomous platformbuoydriftSea icesnow depthDATE/TIMELATITUDELONGITUDESnow heightPressure, atmosphericTemperature, airTemperature, technicalGlobal positioning system, time since last fixQuality flag, snow heightQuality flag, atmospheric pressureQuality flag, air temperatureQuality flag, technical temperatureQuality flag, positionSnow buoyPS138PolarsternCurrent sea ice maps for Arctic and Antarctic (meereisportal.de)International Arctic Buoy Program (IABP)Multidisciplinary Ice-based Distributed Observatory (MIDO)Pan-Arctic observing System of Systems: Implementing Observations for societal Needs (Arctic_PASSION)Physical Oceanography @ AWI (AWI_PhyOce)Sea Ice Physics @ AWI (AWI_SeaIce)2023-08-30T08:00:00/2024-05-17T06:00:00Dataset10.57738/BzPM_0788_202410.1594/PANGAEA.963843100208 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalSnow height was measured by the Snow Buoy 2023S124, an autonomous platform, drifting on Arctic sea ice, deployed during the RV Polarstern expedition PS138. The resulting time series describes the evolution of snow height as a function of place and time between 30 Aug 2023 and 17 May 2024 in sample intervals of 1 hour. The Snow Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on leveled second year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed and contains quality flags for different kinds for erroneous data. Flag values are the sum of individual error codes. The value of 0 refers to no error. Quality flag, position: The geographic position is flagged +1 if the drift velocity, as derived from the GPS longitude and latitude, exceeds a threshold of 10 deg latitude or 50 deg longitude per time step; +2 if the position exceeds extreme values, such as longitude > 360 deg; +4 if the position is exactly 0.0. Quality flag, snow: The snow height is flagged for each sensor +1 for manual corrections during processing (e.g. sensor issues); +2 if the snow accumulation exceeds 0.1 m per hour; +4 if the difference in snow height is larger than 0.03 m compared to values within the last and next 2 hours; +32 if the value exceeds the height of sensor on the platform at 1.5 m. Quality flag, temperature: The air temperature is flagged +1 for manual corrections during processing (e.g. sensor issues); + 32 if the value is below – 50 °C. Quality flag, pressure: The barometric pressure is flagged +1 for manual corrections during processing (e.g. sensor issues).40.8778135.876484.657488.063Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhavenhttps://doi.org/10.13039/501100003207AWI_PS138_03Physical and Chemical OceanographyAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhavenhttps://doi.org/10.13039/501100003207AWI_PS138_04Sea Ice PhysicsAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhavenhttps://doi.org/10.13039/501100003207AWI_PS138_09HybridIceHorizon 2020 of the European Commissionhttps://doi.org/10.13039/501100007601101003472Pan-Arctic observing System of Systems: Implementing Observations for societal Needs (Arctic PASSION)