4.1 Article

Near-tropopause bias in the Russian radiosonde-observed air temperature during the YOPP special observing periods in 2018

期刊

POLAR SCIENCE
卷 27, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.polar.2020.100601

关键词

Observational uncertainty; Radiosonde; Arctic challenge for sustainability; Year of polar prediction

资金

  1. Japanese Ministry of Education, Culture, Sports, Science and Technology (MEXT) through the Arctic Challenge for Sustainability Project (ArCS) [JPMXD1300000000]
  2. Arctic Challenge for Sustainability II (ArCS II) [JPMXD1420318865]
  3. JSPS KAKENHI [18H03745, 18KK0292]
  4. Grants-in-Aid for Scientific Research [18H03745, 18KK0292] Funding Source: KAKEN

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By utilizing enhanced radiosonde observations during the Year of Polar Prediction at Ice Base Cape Baranova in 2018, researchers quantified the observational bias of a nearby station, GMO IM. The study found that the Fedorova station exhibited cold bias in the lower stratosphere during the cold season, as well as a periodic warm/cold bias dipole in the upper troposphere and lower stratosphere. The bias is attributed to errors in radiosonde sensors and radar inaccuracies at Russian observational stations, similar to results found at the Yuzhno-Sakhalinsk station.
Taking advantage of a unique configuration of upper-atmospheric observing stations, we used enhanced radiosonde observations acquired during the Year of Polar Prediction (YOPP) at Ice Base Cape Baranova in 2018 to quantify the observational bias of a nearby station, i.e., GMO IM. E. K. Fedorova located 184 km to the southeast. Radiosonde observations from Fedorova are transmitted to the Global Telecommunications System and thus assimilated into numerical forecast products; however, those from Baranova are not, providing a situation favorable for quantifying observational bias. In comparison with the background field of the ERA5 reanalysis dataset, the Fedorova temperature profile exhibited cold bias in the lower stratosphere during the cold season in addition to a periodic warm/cold bias dipole in the upper troposphere and lower stratosphere. It is concluded that such bias is the product of both radiosonde sensor error and radar inaccuracies at Russian observational stations, given a similar result found at the Yuzhno-Sakhalinsk station.

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