Ice Base Cape Baranova Primary CryoNet Station Information
The station "Cape Baranova" was initially organized in 1986 by the Arctic and Antarctic Research Institute (AARI) of Roshydroment as a research base to perform and to support ship and air-borne High-Arctic expeditions. The station was closed in 1991 due to lack of funding and reopened in August 2013 as a research stationary base "Ice Base Cape Baranova". The station is situated near the Cape Baranova, Bolshevik island, at a sufficiently high (30 m) shore of the Shokalskij Strait, separated the Bolshevik and October Revolution islands, both belonging to the Severnaya Zemlya archipelago. Station coordinates are 79°16'N, 101°45'E. The Strait near the station is 40 km wide and up to 350 meters deep. Adjacent area is characterized by a wide range of natural ice: fast and drifting sea ice, numerous icebergs, lakes, river ice, and significant (up to 800 m) dome-shaped glaciers. The area near the station is replete with numerous lakes and pronounced polar desert landscape. Fauna is represented by polar bears, foxes, polar wolves, hares, deer, seals, lemmings and numerous colonies of marine and terrestrial migratory birds. Station is characterized by long polar night from 22 October to 22 February and polar day from April 22 to August 22. The air temperature in the summer (June-August) is from 0° to 4°C. In winter (October-April) the temperature range is from -25° to -45° C. Station area is characterized by sustained winds of predominantly southerly direction at an average speed of 10-15 m/s. During the transition period, the wind speed can reach 50 m/s. Soil in the vicinity of the station is mostly composed from rocky shale. The depth of summer thawing does not exceed 30 - 40 cm. The main areas of work planned and partially initiated on the station "Ice Base Cape Baranova" are: routine and special year-round meteorological, sea-ice, oceanographic, hydrological, geophysical, glaciological and biological observations, implementation of a comprehensive monitoring of the state and pollution of the environment, studies of gas exchange in the atmosphere-ice-ocean and the atmosphere-land, completion of special experimental work aimed to investigate the processes that determine climate change in the high latitudes of the Arctic, and the assessment of their impact on the environment and the ecosystem of the Arctic region of Russia. In addition, the station "Ice Base Cape Baranova" will be used as a site to support logistics for research and observations in the high Arctic, including safety of operation of drifting station "North Pole."
Other Networks to Which This CryoNet Station Belongs
GAW, BSRN
Measurement Methods Used
WMO Technical Regulations
JCOMM
Data Information
Are the data quality controlled? yes
How are the data accessible? FTP, HTTP (web), an existing data center
Data availability (may depend on the variable measured): in real-time, in near real-time, delayed more than one year
Publications
Borodkin V.A., Makshtas A.P., Bogorodsky P.V. Coastal fast ice in the Shokalski Strait. Ice and Snow. 2016;56(4):525-532. (In Russ.) DOI:10.15356/2076-6734-2016-4-525-532
Measurements
The measurements made at Ice Base Cape Baranova are listed in the following tables. (Note: If End Year is blank, measurements are ongoing.)
Cryosphere Measurements
Element
Variable
Start Year
End Year
Frequency
Snow
Depth
2013
Continuous
Snow
Snow water equivalent
2013
Continuous
Snow
Snowpack profile
Sporadic
Snow
Extent
2013
Continuous
Snow
Drifting/blowing
2013
Continuous
Snow
Albedo
2013
Continuous
Seaice
Thickness
2013
Continuous
Seaice
Freeboard
Continuous
Seaice
Concentration
2013
Continuous
Seaice
Type
2013
Continuous
Seaice
Form of ice (floe size)
Continuous
Seaice
Stage of development
Continuous
Seaice
Ice phenomena
Continuous
Seaice
Stage of melting
Continuous
Seaice
Motion
2013
Continuous
Seaice
Openings (leads, etc.)
Continuous
Seaice
Draft
2013
Continuous
Seaice
Extent
2013
Continuous
Seaice
Salinity
Continuous
Seaice
Stratigraphy
Continuous
Seaice
Age
2013
Continuous
Seaice
Temperature
2013
Sporadic
Seaice
Temperature profile
Continuous
Seaice
Albedo
2013
Sporadic
Seaice
Melt onset
2013
Continuous
Seaice
Ice chemistry
2013
Sporadic
Freshwater
Thickness
2014
Fragmented
Permafrost
Soil temperature
2014
Fragmented
Permafrost
Active layer depth
2014
Fragmented
Permafrost
Thermal state
2014
Fragmented
Permafrost
Duration of thaw
2014
Fragmented
Permafrost
Onset of seasonal freezing
2014
Fragmented
Permafrost
Depth of seasonal freezing
2014
Fragmented
Glacier
Accumulation
2014
Fragmented
Glacier
Annual mass balance
2014
Fragmented
Glacier
Area
2014
Fragmented
Glacier
Winter mass balance
Not specified
Glacier
Glacial discharge
2014
Fragmented
Glacier
Surface topography
2014
Fragmented
Glacier
Surface temperature
2014
Fragmented
Glacier
Surface albedo
2014
Sporadic
Glacier
Ice/firn temperature
2014
Fragmented
Iceberg
Iceberg position
2013
Fragmented
Iceberg
Size
2013
Fragmented
Iceberg
Iceberg concentration
2013
Fragmented
Iceberg
Sporadic
Iceberg
Sporadic
Iceberg
Draft
Sporadic
Atmosphere Measurements
Element
Variable
Start Year
End Year
Frequency
Met
Air temperature
2013
Continuous
Met
Humidity/vapour pressure
2013
Continuous
Met
Wind speed and direction
2013
Continuous
Met
Air pressure
2013
Continuous
Met
Snowfall
2013
Continuous
Met
Total precipitation
2013
Continuous
Met
Rainfall
2013
Continuous
Met
Trace gases
2014
Continuous
Met
Aerosols
2014
Fragmented
Met
Sensible and latent heat
2014
Fragmented
Radiation
Downwelling shortwave
2014
Continuous
Radiation
Upwelling shortwave
2014
Continuous
Radiation
Downwelling longwave
2014
Continuous
Radiation
Upwelling longwave
2014
Continuous
Radiation
Sunshine duration
2014
Continuous
Measurement Notes and Other Measurements
Category
Description or List
Hydrology
Measurements of river water level and discharge are conducted during the summer period
Ecology
Biological diversity and phenomena observations (zoological, botanical observations at the station and in the surrounding tundra) during short visits in summer
Oceanography
Regular CTD-transects across Vilkitskij Strait and current measurements in selected points
Station is characterized by long polar night from 22 October to 22 February and polar day from April 22 to August 22. The air temperature in the summer (June-August) is from 0° to 4°C. In winter (October-April) the temperature range is from -25° to -45° C. Station area is characterized by sustained winds of predominantly southerly direction at an average speed of 10-15 m/s. During the transition period, the wind speed can reach 50 m/s. Soil in the vicinity of the station is mostly composed from rocky shale. The depth of summer thawing does not exceed 30 - 40 cm.
The main areas of work planned and partially initiated on the station "Ice Base Cape Baranova" are: routine and special year-round meteorological, sea-ice, oceanographic, hydrological, geophysical, glaciological and biological observations, implementation of a comprehensive monitoring of the state and pollution of the environment, studies of gas exchange in the atmosphere-ice-ocean and the atmosphere-land, completion of special experimental work aimed to investigate the processes that determine climate change in the high latitudes of the Arctic, and the assessment of their impact on the environment and the ecosystem of the Arctic region of Russia. In addition, the station "Ice Base Cape Baranova" will be used as a site to support logistics for research and observations in the high Arctic, including safety of operation of drifting station "North Pole."