4.7 Article

Snow Depth and Air Temperature Seasonality on Sea Ice Derived From Snow Buoy Measurements

期刊

FRONTIERS IN MARINE SCIENCE
卷 8, 期 -, 页码 -

出版社

FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2021.655446

关键词

sea ice; snow; buoy; measurement; platform; Arctic (Ocean); Antarctic

资金

  1. Helmholtz infrastructure program ACROSS
  2. Helmholtz infrastructure program FRAM
  3. Helmholtz Alliance Remote Sensing and Earth System Dynamics [HA-310]
  4. EU [640161, 262922]
  5. DFG [NI1096/2-1, NI1096/5-1, AR1236/1]
  6. ESA Sea Ice CCI phase 1 and 2 [AO/1-6772/11/I-AM]
  7. German Ministry of Economics and Technology [50EE1008]

向作者/读者索取更多资源

This study presents a new autonomous platform designed to measure snow depth and other parameters on drifting Arctic and Antarctic sea ice. The dataset includes 79 time series since 2013, showing regional differences in the annual cycle of snow depth on sea ice.
Snow depth on sea ice is an essential state variable of the polar climate system and yet one of the least known and most difficult to characterize parameters of the Arctic and Antarctic sea ice systems. Here, we present a new type of autonomous platform to measure snow depth, air temperature, and barometric pressure on drifting Arctic and Antarctic sea ice. Snow Buoys are designed to withstand the harshest environmental conditions and to deliver high and consistent data quality with minimal impact on the surface. Our current dataset consists of 79 time series (47 Arctic, 32 Antarctic) since 2013, many of which cover entire seasonal cycles and with individual observation periods of up to 3 years. In addition to a detailed introduction of the platform itself, we describe the processing of the publicly available (near real time) data and discuss limitations. First scientific results reveal characteristic regional differences in the annual cycle of snow depth: in the Weddell Sea, annual net snow accumulation ranged from 0.2 to 0.9 m (mean 0.34 m) with some regions accumulating snow in all months. On Arctic sea ice, the seasonal cycle was more pronounced, showing accumulation from synoptic events mostly between August and April and maxima in autumn. Strongest ablation was observed in June and July, and consistently the entire snow cover melted during summer. Arctic air temperature measurements revealed several abovefreezing temperature events in winter that likely impacted snow stratigraphy and thus preconditioned the subsequent spring snow cover. The ongoing Snow Buoy program will be the basis of many future studies and is expected to significantly advance our understanding of snow on sea ice, also providing invaluable in situ validation data for numerical simulations and remote sensing techniques.

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