Preprints
https://doi.org/10.5194/essd-2020-391
https://doi.org/10.5194/essd-2020-391

  25 Jan 2021

25 Jan 2021

Review status: this preprint is currently under review for the journal ESSD.

Hydrometeorological dataset of West Siberian boreal peatland: a 10-year record from the Mukhrino field station

Egor Dyukarev1,2, Nina Filippova1, Dmitriy Karpov1, Nikolay Shnyrev3, Evgeny Zarov1, Ilya Filippov1, Nadezhda Voropay2,4, Vitaly Avilov5, Arseniy Artamonov6, and Elena Lapshina1 Egor Dyukarev et al.
  • 1Yugra State University, Khanty-Mansiysk, 628012, Russia
  • 2Institute of Monitoring of Climatic and Ecological System SB RAS, Tomsk, 634055, Russia
  • 3Faculty of Soil Science, Lomonosov Moscow State University, Moscow, 119991, Russia
  • 4V. B. Sochava Institute of Geography SB RAS, Irkutsk, 664033, Russia
  • 5A. N. Severtsov Institute of Ecology and Evolution RAS, Moscow, 119071, Russia
  • 6A. M. Obukhov Institute of Atmospheric Physics, Moscow, 119017, Russia

Abstract. Northern peatlands represent one of the largest carbon pools in the biosphere but the carbon they store is increasingly vulnerable to perturbations from climate and land-use change. Meteorological observations taken directly at peatland areas in Siberia are unique and rare, while peatlands are characterized by a specific local climate. This paper presents a hydrological and meteorological dataset collected at the Mukhrino peatland, Khanty-Mansi Autonomous Okrug – Yugra, Russia, over the period of 8 May 2010 to 31 December 2019. Hydrometeorological data were collected from stations located at a small pine-shrub-Sphagnum ridge and Scheuchzeria-Sphagnum hollow at ridge–hollow complexes of ombrotrophic peatland. The monitored meteorological variables include air temperature, air humidity, atmospheric pressure, wind speed and direction, incoming and reflected photosynthetically active radiation, net radiation, soil heat flux, precipitation (rain) and snow depth. A gap-filling procedure based on the Gaussian process regression model with an exponential kernel was developed to obtain continuous time series. For the record from 2010 to 2019, the average mean annual air temperature at the site was −1.0 °C, with the mean monthly temperature of the warmest month (July) recorded as 17.4 °C and for the coldest month (January) −21.5 °C. The average net radiation was about 35.0 W m−2, and the soil heat flux was 2.4 and 1.2 W m−2 for the hollow and the ridge sites, respectively.

The presented data are freely available through Zenodo (https://zenodo.org/record/4323024, last access: 15 December 2020) and can be used in coordination with other hydrological and meteorological datasets to examine the spatio‐temporal effects of meteorological conditions on local hydrological responses across cold regions.

Egor Dyukarev et al.

Status: open (until 22 Mar 2021)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Egor Dyukarev et al.

Data sets

Hydrometeorological dataset of West Siberian boreal peatland: a 10-year records from the Mukhrino field station Dyukarev, E., Filippova, N., Karpov, D., Shnyrev, N., Zarov E., Filippov, I., Voropay, N., Avilov, V., Artamonov A., and Lapshina, E. https://doi.org/10.5281/zenodo.4323024

Egor Dyukarev et al.

Viewed

Total article views: 251 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
202 46 3 251 18 3 5
  • HTML: 202
  • PDF: 46
  • XML: 3
  • Total: 251
  • Supplement: 18
  • BibTeX: 3
  • EndNote: 5
Views and downloads (calculated since 25 Jan 2021)
Cumulative views and downloads (calculated since 25 Jan 2021)

Viewed (geographical distribution)

Total article views: 217 (including HTML, PDF, and XML) Thereof 216 with geography defined and 1 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 07 Mar 2021
Download
Short summary
A hydrological and meteorological dataset collected at the Mukhrino peatland, Khanty–Mansi Autonomous Okrug – Yugra, Russia over the period of 08 May 2010 to 31 December 2019 are presented. Northern peatlands represent one of the largest carbon pools in the biosphere the carbon they store is increasingly vulnerable to perturbation. Meteorological observations directly at peatland areas in Siberia are rare, while peatlands characterized by a specific local climate.