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Site Overview Data and Observations Map of Research Site
Basin / Site Name
Djankuat Research Basin
Country; Province/State
Russia
Website (if available)
Operational Management
Lomonosov Moscow State University Water problems institute Russian Academy of Sciences
Oversight/Contacts
NameRoleContact Information
Ekaterina Rets
Curator of the Research Catchment in the INARCH Network, Hydrological and meteorological monitoring
Email: ekaterina.p.rets@gmail.com
Viktor Popovnin
Head of the Station, Glaciological monitoring
Email: begemotina@hotmail.com
Basin / Site Location (Centroid Coordinates)
Coordinate Format
Latitude
Longitude
Degrees Minutes Seconds
Decimal Degrees
43.208 N
42.735 E
Purpose / Scientific Focus
The Djankuat glacier was chosen as representative of the central North Caucasus during the International Hydrological Decade (IHD) - research program on water problems launched by UNESCO in 1965 - and is one of 30 ‘reference’ glaciers in the world which has annual mass balance series longer than 50 years. The mass-balance measurements have been carried out on Djankuat glacier since 1967 till now regularly (www.wgms.ch ) based on standard methods. Detailed hydrological and meteorological measurements were included in the monitoring program of the station during the IHD and came to an end in the late 1970s. The comprehensive hydrometeorological observation was resumed in the Djankuat research basin since 2007. Hydrometeorological measurements were done during the ablation season every year since 2007, all-year round hydrological gauge since 2021, and the observational program gradually expanded during 2007–2023 and now goes beyond the standard network hydrological and meteorological observations.
Location (Physiographic Region)
Location (Physiographic Region) Alpine zone of the North Caucasus
Area (km2)
12.4 km2
Elevation (m; Mean, Maximum, Minimum)
between 2600 and 4000 m
Description (Physical–Ecological–Climatic Characteristics)
The Djankuat research basin is situated on the northern slope of the central part of the Main Caucasian Ridge. The climate is moderate continental to high-alpine
Drainage / River System
The Djankuat River is a source of the Adul-Su River – a tributary of the Baksan River which drains into the Caspian Sea via the Terek River.
Site History or Historical Context
The Djankuat glacier was chosen as representative of the central North Caucasus during the International Hydrological Decade (IHD) - research program on water problems launched by UNESCO in 1965 - and is one of 30 ‘reference’ glaciers in the world which has annual mass balance series longer than 50 years.
Years of Data
(1970s) – 2007 – ongoing
Glacierized Area (% and year(s) measured)
In the 2017 glaciers occupied 27% of the territory of the basin. The main glacier with the same name – Djankuat glacier – is the source of the Djankuat River. It is a valley glacier, with the lowest point of the tongue at approximately 2750 m, the elevation of the bergschrund is at 3600 m. The mean elevation of the glacier is 3210 m, the area is 2.42 km2, and its length is 3.0 km. The maximum measured thickness of the glacier is 105 m, and the average thickness is 31 m. The Djankuat River basin also contains three small glaciers with areas less than 0.5 km2: Koyavgan, Via-Tau, and Visyachiy.
Main Land Cover(s)
Alpine highlands with steep slopes and a wide development of coarse-grained deposits, with numerous outcrops of exposed rocks, with alpine lawns in the lower part of the basin and with glacial-nival landscapes in its middle and upper parts
Lithology / Soils
crystalline schists and gneisses; gravelly shallow humus soils
J F M A M J J A S O N D A
Mean Monthly and Annual Temperature (°C)
-7.3; -6.4; -3.2; 2.1; 6.8; 10.0; 12.5; 12.2; 8.5; 3.9; ; -1.3; -5.2; 2.7 (According to the closest all-year round meteorological station in Terskol)
J F M A M J J A S O N D A
Mean Total Monthly and Annual Precipitation (mm)
58; 45; 67; 86; 92; 93; 102; 94; 100; 85; 64; 59; 942 (According to the closest all-year round meteorological station in Terskol)
Snow Characteristics
Stable snow cover is generally observed on the whole basin area from October-November to May. In the accumulation zone of glaciers snow persists through the year. Mean measured snowdepth on the Djankuat Glacier is 3600 mm, Maximum is 11550 mm
Additional Noteworthy Characteristics of Basin/Site
Digital Elevation Model
Available on request
Landcover and Soils
Aleynikova, A. M. Struktura i dinamika prilednikovykh landshaftov Priel'brus'ya / A. M. Aleynikova, M. N. Petrushina // Lod i sneg. – 2011. – № 2(114). – S. 127-134. – EDN PJEMMH. (in Russian)
Stream/River Network
Available on request
Basin Delineation / Shapefile
Available on request
Observation Stations
TypeStation NameLatitudeLongitudeElevationNotes / Details
Meteorological
Djankuat Base Camp AWS
43.208
42.736
2640
Meteorological
Djankuat Glacier AWS 1
43.198
42.757
3000
IV zone of the Djankuat glacier on the ice surface
Meteorological
Djankuat Glacier AWS 2
43.200
42.759
3050
IV zone of the Djankuat glacier on the debris covered ice
Meteorological
Djankuat Glacier AWS 3
43.193
42.759
3200
Hydrological
Djankuat River Base Camp Gauging Station
43.209
42.736
2630
Hydrological
Djankuat River Rock Gauging Station
43.213
42.725
2600
Data Availability and Access
Data and Datasets (Links / DOIs to published or available data and descriptions)
Rets, E. P., Popovnin, V. V., Toropov, P. A., Smirnov, A. M., Tokarev, I. V., Chizhova, J. N., Budantseva N. A. et al. 2019 Djankuat glacier station in the North Caucasus, Russia: a database of glaciological, hydrological, and meteorological observations and stable isotope sampling results during 2007–2017. Earth System Science Data 11, 3, 1463-1481.
Rets, EP; Popovnin, VV; Toropov, PA et al. (2022): Hydrological, meteorological observations and isotopes sampling results during 2019-2020 at Djankuat Glacier Station in the North Caucasus, Russia. https://doi.org/10.1594/PANGAEA.940839
Meteorological Variables and Sensor Details
VariableStation NameSensor(s)Height / Depth (m)Record PeriodMeasurement FrequencyNotes / Details
Air temperature and Relative Humidity
Djankuat Glacier AWS 1
Campbell AWS - Vaisala MT300 sensor
3000
2007-2021
15 min
Operating during June-September
Djankuat Glacier AWS 2
Campbell AWS - Vaisala MT300 sensor
3050
2007-2009
15 min
Operating during June-September
Djankuat Glacier AWS 3
DAVIS AWS
3200
2017
15 min
Operating during June-September
Djankuat Base Camp AWS
DAVIS AWS
2640
2007 - ongoing
15 min
Operating during June-September
Solar Radiation
Djankuat Glacier AWS 1
Campbell AWS -KEEP & ZONNEN radiometers
3000
2007-2021
15 min
Operating during June-September
Djankuat Glacier AWS 2
Campbell AWS -KEEP & ZONNEN radiometers
3050
2007-2009
15 min
Operating during June-September
Longwave Radiation
Djankuat Glacier AWS 1
Campbell AWS - wind sensor
3000
2007-2021
15 min
Operating during June-September
Djankuat Glacier AWS 2
Campbell AWS -KEEP & ZONNEN radiometers
3050
2007-2009
15 min
Operating during June-September
Wind Speed/Direction
Djankuat Glacier AWS 1
Campbell AWS - wind sensor
3000
2007-2021
15 min
Operating during June-September
Djankuat Glacier AWS 2
Campbell AWS - wind sensor
3050
2007-2009
15 min
Operating during June-September
Djankuat Glacier AWS 3
DAVIS AWS
3200
2017
15 min
Operating during June-September
Djankuat Base Camp AWS
DAVIS AWS
2640
2007 - ongoing
15 min
Operating during June-September
Precipitation
Djankuat Base Camp AWS
DAVIS AWS
2640
2007 - ongoing
15 min
Operating during June-September
Atmospheric Pressure
Djankuat Glacier AWS 1
Campbell AWS - Vaisala pressure sensor
3000
2007-2021
15 min
Operating during June-September
Djankuat Glacier AWS 2
Campbell AWS - Vaisala pressure sensor
3050
2007-2009
15 min
Operating during June-September
Djankuat Base Camp AWS
DAVIS AWS
2640
2007 - ongoing
15 min
Operating during June-September
Air temperature, Relative humidity, Mean wind speed, Maximum wind speed, Wind direction, at 0.25, 0.5, 1 and 2 m
Djankuat Glacier AWS 1
DAVIS AWS
3000
Jul – Aug 2017
15 min
Operating during June-September
Three components of wind speed, T - acoustic temperature
Djankuat Glacier AWS 1
Sonic anemometer GILL
3000
Jul – Aug 2013, Jun – Jul 2014, Jun – Aug 2016
10 Hz
Operating during June-September
Hydrological Variables and Sensor Details
VariableStation NameSensor(s)Height / Depth (m)Record PeriodMeasurement FrequencyNotes / Details
Snow Depth
Djankuat Glacier
Probe poles
2850 - 3650
(1970) 2007 – ongoing
1 time yearly at max.
At 250–300 evenly distributed points on the Djankuat Glacier Surface
Snow Water Equivalent
Djankuat Glacier Snowpits
Snow sampling cylinder
2900 - 3300
(1970) 2007 – ongoing
1-5 times in each snowpit yearly
Stake 9, 18, 49, 65/68
Glacier/Snow ablation
Djankuat Glacier
Ablation stakes
2850 - 3650
(1970) 2007 – ongoing
With 1-30 days timestep
At 35–45 evenly distributed points on the Djankuat Glacier Surface
Djankuat Glacier AWS 1
Campbell AWS -Sonic Ranger sensor
3000
2007-2017
15 min
Stream Level/Discharge
Djankuat Glacier AWS 2
Campbell AWS -Sonic Ranger sensor
3050
2007-2009
15 min
Djankuat River Base Camp Gauging Station
Keller DCX-18 VG
2630
2007-ongoing
10 min
Operating during June-September,
Water discharge calculated using salt dilution easurements
Djankuat River Rock Gauging Station
Keller PAA-36XiW CTD with ARC-1
2600
2021-ongoing
10 min
All-year-round operation, Water discharge calculated using salt dilution measurements
Water Quality Variables and Sensor Details
VariableStation NameSensor(s)Height / Depth (m)Record PeriodMeasurement FrequencyNotes / Details
Water Temperature
Djankuat River Base Camp Gauging Station
WTW 3310
2630
2007-ongoing
~6-7 times daily
Operating during June-September
Djankuat River Rock Gauging Station
Keller PAA-36XiW CTD with ARC-1
2600
2021-ongoing
10 min
All-year-round operation
Water Conductivity
Djankuat River Base Camp Gauging Station
WTW 3310
2630
2007-ongoing
~6-7 times daily
Operating during June-September
Djankuat River Rock Gauging Station
Keller PAA-36XiW CTD with ARC-1
2600
2021-ongoing
10 min
All-year-round operation
Isotopes (18O, D)
Djankuat River Base Camp Gauging Station
2013: mass spectrometer, 2014-2016: laser-based spectrometer;
2017 - Cavity Ring-Down Spectroscopy
2630
2013-2017
2 times daily
Operating during June-September
Turbidity
Djankuat River Base Camp Gauging Station
portable turbidity meter HACH 2100P
2600
2007-2021, 2023-ongoing
~6-7 times daily
Operating during June-September
Djankuat River Rock Gauging Station
portable turbidity meter HACH 2100P
2600
2023-ongoing
1-2 times daily
Operating during June-September
Other Hydrological and Cryospheric Measurements and Observations
MeasurementInstrumentation DescriptionSpatial / Temporal Resolution and CoverageNotes / Details
Glacier Ice Thickness
radio-echo sounding and modelling
2012-2013
Lavrentiev I.I., Kutuzov S.S., Petrakov D.A., Popov G.A., Popovnin V.V. Ice thickness, volume and subglacial relief of Djankuat Glacier (Central Caucasus). Ice and Snow. 2014;54(4):7-19. https://doi.org/10.15356/2076-6734-2014-4-7-19
Relevant Modelling Activity (Model Applications, Purpose, Advancements, etc.)
Rets, E., Fomichev, S. and Belozerov, E., 2021, April. Testing different machine learning techniques for runoff routing in a highly glacierized Djankuat river basin (the North Caucasus, Russia). In EGU General Assembly Conference Abstracts (pp. EGU21-4567). Belozerov, E., Rets, E., Petrakov, D. and Popovnin, V., 2020. Modelling glaciers’ melting in Central Caucasus (the Djankuat and Bashkara Glacier case study). In E3S Web of Conferences (Vol. 163, p. 01002). EDP Sciences. Verhaegen, Y., Huybrechts, P., Rybak, O. and Popovnin, V.V., 2020. Modelling the evolution of Djankuat Glacier, North Caucasus, from 1752 until 2100 CE. The Cryosphere, 14(11), pp.4039-4061.
Additional Information (Key Papers, Articles/Media, Photographs, etc.)
Rets, E.P., Popovnin, V.V., Toropov, P.A., Smirnov, A.M., Tokarev, I.V., Chizhova, J.N., Budantseva, N.A., Vasil'chuk, Y.K., Kireeva, M.B., Ekaykin, A.A. and Veres, A.N., 2019. Djankuat glacier station in the North Caucasus, Russia: A database of glaciological, hydrological, and meteorological observations and stable isotope sampling results during 2007–2017. Earth System Science Data, 11(3), pp.1463-1481. Popovnin, V.V., Rezepkin, A.A. and Tielidze, L.G., 2015. Superficial moraine expansion on the Djankuat Glacier snout over the direct glaciological monitoring period. Earth Cryosphere, 19(1), pp.79-87. Verhaegen, Y., Huybrechts, P., Rybak, O. and Popovnin, V.V., 2020. Modelling the evolution of Djankuat Glacier, North Caucasus, from 1752 until 2100 CE. The Cryosphere, 14(11), pp.4039-4061. Tsyplenkov, A., Vanmaercke, M., Collins, A.L., Kharchenko, S. and Golosov, V., 2021. Elucidating suspended sediment dynamics in a glacierized catchment after an exceptional erosion event: The Djankuat catchment, Caucasus Mountains, Russia. Catena, 203, p.105285. Verhaegen, Y., Rybak, O., Popovnin, V. and Huybrechts, P., 2023. Quantifying supraglacial debris-related melt-altering effects on the Djankuat Glacier, Russian Federation, Part 1: comparison of surface energy and mass fluxes over clean and debris-covered ice. Popovnin V.V., Pylayeva T.V. Avalanche feeding of the Djankuat Glacier. Ice and Snow. 2015;55(2):21-32. https://doi.org/10.15356/2076-6734-2015-2-21-32
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