EGU22-10368
https://doi.org/10.5194/egusphere-egu22-10368
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Atmospheric Mercury Depletion Events: Assessment Impact of Meteorological Parameters in the Arctic Winter

Fidel Pankratov1, Alexander Mahura2, Vladimir Masloboev1, and Valentin Popov3
Fidel Pankratov et al.
  • 1Institute of Northern Environmental Problems, Kola Science Center, Russian Academy of Sciences, Obninsk, Russian Federation (fidel_ru@mail.ru)
  • 2Institute for Atmospheric and Earth System Research /Physics, Faculty of Science, University of Helsinki
  • 3Research and Production Association “Typhoon” of Roshydromet

In 2001, the mercury analyzer was installed at Amderma (69.450 N, 61.390 E, 49 m above sea level; Yugor Peninsula) in the Nenets Autonomous Okrug (Russia) to carry out continuous measurements of gaseous elemental mercury vapor concentration in the atmospheric surface layer. The data analysis demonstrated that the atmospheric mercury depletion evens (AMDEs, concentration < 1 ng m-3) are observed on a rather limited territory, i.e. along the coast of the Arctic seas. During observational period (2001-2015), the analyzer was placed at three locations at different distances (8.9 km – 2001-2004, 2.5 km – 2005-2010, and 200 m - 2010-2015) from the Kara Sea coast.

For the AMDEs cases, during winters of 2001-2004 the air temperature was in range from -150С to -310С and relative humidity – 68-84%. The dominated atmospheric transport for these cases was mainly observed from the N-N-W direction. The number AMDEs relative to all measurements was about 0.2%. For 2005-2010, the temperature ranged from -10С to -370С and relative humidity – 74-83%. The atmospheric transport – from the E-E-N direction. The number AMDEs relative to all measurements was 2.7%. For 2010-2013, the temperature varied from -220С to -270С and relative humidity – 75-87%. The atmospheric transport – mainly from the S-S-W direction. The number AMDEs relative to all measurements was 26.9%, showing substantial 10-fold increase of AMDEs compared with the previous period. As a result, all cases correspond to range of air temperatures from -10C to -370C and relative humidity of 68-87% for entire monitoring period considered.

For selected considered episode (29-30 Mar 2002), the air temperature varied from -260C to -310C, and when it decreased to the minimum, the effect of mercury depletion was detected with the lowest concentration (0.39 ng m-3). For episode (29 Feb - 1 Mar 2007), the temperature was also decreasing from -160C to -370C, and at reaching the minimum, the mercury concentration was also the lowest (0.12 ng m-3). Moreover, in Dec 2006, for the first time, a significant number of AMDEs cases (23 events) was recorded during the polar night. In Feb 2010 the longer duration (up to 40 hours) AMDEs episodes were observed compared with Jan (up to 15 hours).

Note that all AMDEs are generally observed at lower air temperatures and relative humidity values with respect to the average values.

How to cite: Pankratov, F., Mahura, A., Masloboev, V., and Popov, V.: Atmospheric Mercury Depletion Events: Assessment Impact of Meteorological Parameters in the Arctic Winter, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-10368, https://doi.org/10.5194/egusphere-egu22-10368, 2022.