5.4.1-V.Pushkarev D.Drozdov-YaNAO experts on Belyy Island

5.4.1-V.Pushkarev D.Drozdov-YaNAO experts on Belyy Island

SCIENCE AND INNOVATIONS DEPARTMENT, YANAO ADMINISTRATION
EARTH CRYOSPHERE INSTITUTE SIBERIAN BRANCH RUSSIAN ACADEMY OF SCIENCE
GLOBAL CRYOSPHERE WATCH
«BELYY ISLAND AS POTENTIAL
STATION OF CRYONET»
Dmitry Drozdov
Earth Cryosphere Institute Siberian Branch Russian Academy of Sciense
Russian State Geological Prospecting University n. a. Sergo Ordzhonikidzе (MGRI-RSGPU), Moscow
Tymen State Oil and Gas University
The University of Tyumen
Pavel Orekhov
Earth Cryosphere Institute Siberian Branch Russian Academy of Sciense
Salekhard 2016
LOCATION
N73°33’
E70°05’
GEOLOGICAL CONDITION
LANSCAPES, GEOMORPHOLOGY, PALEOGEOGRAPHY
Typical landscapes of “Belyy” island
Geomorphological scheme
Fluctuation of sea level
and air temperature
during the Holocene
The scheme of sequence of
formation, thawing and
freezing of the coastal
lowlands during the Upper
Pleistocene-Holocene
map of cryogenic
relief type
ecological and geographical analysis
microalgae from sediments of
marine terraces
EARTH CRYOSPHERE, 2014, Vol. XVIII, № 3, p. 33-45
E.Slagoda et all, Cryolithological structure of the
first terrace…
CRYOLITHOLGICAL STRUCTURE AND GEOCRYOLOGICAL CONDITIONS
Cryogenic sedimentary
textures and diagenetic
deformations in sediments
of Belyy island
Cryolithological
cross-section and
сomposition of watersoluble salts in sediments
The temperature of the permafrost in the different
types of landscapes
bh 1
bh 2
bh 3
bh 4
GEOCRYOLOGICAL PROCESSES
COMPLEX BIOLOGICAL AND SOIL RESEARCH
запасы фитомассы в арктических тундрах о.Белый
STUDY OF VEGETATION
•
•
•
•
•
•
geobotanic descriptions
species composition
Structure of plant communities
abundance and species cover
above-ground plant biomass
verification and calibration LAI and NDVI indices with
field spectroradiometer
STUDY OF SOILS
before removal of vegetation mat. Middle: polygonal
Bottom: Soil plugs from center of nonsorted circle
g depth of organic soil horizon.
before removal of vegetation mat. Middle: polygonal
Bottom: Soil plugs from center of nonsorted circle
g depth of organic soil horizon.
•
•
•
•
study of the vertical structure of the soil profile
patterns of distribution of organic matter in the soil profile
distribution type of soil on different elements of the relief
study of the composition of gas released during thawing of the
active layer and the soil
and center of polygons.
STUDY OF ANAMAL POPULATIONS
Page 36
s and center of polygons.
NDVI
• aerial surveys of the wild population of reindeer
• Page 36study of the species composition of the avifauna
• fixing birds species on migration;
• fixation breeding bird species
• study of feeding base of birds raptors
• species composition of small mammals
REPRESENTATIVENESS OF THE STATION
FOR METEOROLOGICAL AND CRYOLOGICAL PARAMETERS
Net of reference stations in Russia
Basic stations location is
arranged so to ensure
the required accuracy of
interpolation of
meteorological data
The reference station is the basic stations with at least 30
years record.
IM. M.V. POPOVA (Russian Federation)
in WMO RA II – Asia
Opened in 1934
WMO index No: 0-20000-0-20667
Coordinates: 73.33°N, 70.06°E, 3,7 m
Observation ( from WMO Pub 9 Vol A):
GOS Global Observing System
GSN Global Surface Network
CLIMAT(C)
RBCN Regional Basic Climatological Networks
RBSN(S) Regional Basic Synoptic Networks
Reference climatological station
Basic climatological station
Supplementary climatological station
ACCESSIBILITY OF STATION BELYY ISLAND
IN THE WINTER
IN THE SUMMER
STAFF AND DATA
Meteorogical station operateв all the year round. The meteorological measurements are
carried out in terms of meteorological standard in 3 hours. Data is transmitted using the
satellite communication system INMARSAT. All work is done by qualified meteorologists
with Roshydromet control. Measurement of the depth of the active layer and the thermal
state of permafrost recording are carried out 2 times a year
INFRASTRUCTURE OF STATION BELYY ISLAND
1
4
Meteorological station
1
2
Plot 1: snow, permafrost,
active layer depth
blue labels show the point of measure ice
thickness on the lake
2 3
5
3
6
Plot 2: snow, permafrost,
active layer depth
4
6
5
Plot 3: snow
Plot 4: snow
Plot 5: snow
All measurements on
the meteorological station
are conducted in accordance
with the standards of the
WMO and Roshydromet.
At additional
sites
observations on the spatial
distribution of the snow
cover in the coastal part (4),
on different type of the relief
(2,3,5), in the valleys of
medium and small rivers
(3,6). The active layer depth
and the temperature of the
permafrost measurement on
plot (2,3)
PERMAFROST AND ACTIVE LAYER DEPTH MEASUREMENTS
Measuring the depth of the active layer at the CALM site
LOAM
OCTOBER
SEPTEMBER
OCTOBER
The temperature of the permafrost in the different types of
landscapes
SEPTEMBER
JULY
JULY
SAND
70
90.2
99.8
СКВ 4
110
130
2015
2014
2013
2012
2011
2010
20
90
СКВ 3
2009
2015
2014
2013
2012
2011
2010
СКВ 2
2009
СКВ 1
91.4
98.1
113.7 111.6
110.5
40
60
80
39.8
54.4 50.1 53.3
60
54.9
59
SNOW MEASUREMENTS
Measurement of the depth and density of snow are heled along the profiles and at plots (sites) placed at
different elements of relief and in river valleys (as addition to standard observations of meteorological station)
Temperature of snowpack profile (°С)
0м
0,3 м 0,6 м 0,9 м 1,2 м 1,5 м возд
0
-2
-3.5
-4
-4.3
-4.9
-5.5
-6
-6
-8
-9.7
-11.3
-10
-12
80.0
960
900
840
0.0
780
0.00
720
20.0
660
0.10
600
40.0
T1
T2
T3
T4
T5
T6
T7
T8
T9
T10
T11
T12
T13
T14
T15
T16
T17
0.20
540
60.0
480
0.28
0.31
420
0.33 0.32 0.33 0.32
360
0.35
300
0.31 0.32
240
0.27
0.29
120
0.34
0.33 0.33 0.33
60
0.30
0.31 0.29
Depth of snow on profile OBS03-200415, sm
0
0.40
100.0
180
Den sity of sn o w o n p r o file OB S03-20 04 15 gr /sm 3
SEA AND LAKE ICE MEASUREMENTS
parameters
sea ice
lake ice
Extent
+
-
Concentration
+
-
Thickness
+
+
Motion
+
-
Melt onset
+
-
Snow depth on ice
+
+
Equipment for ice and water measurements
Lake ice thickness, sm (25 April 2015)
250
200
150
100
50
Series1
thickness of ice
Series2 of lake
Ddepth
OB_OZ_03_03
OB_OZ_03_02
OB_OZ_03_01
OB_OZ_05_01
OB_OZ_04_01
OB_OZ_06_03
OB_OZ_06_02
OB_OZ_06_01
OB_OZ_EX_02
OB_OZ_EX_01
OB_OZ_02_03
OB_OZ_02_04
OB_OZ_02_02
OB_OZ_02_01
OB_OZ_01_04
OB_OZ_01_03
OB_OZ_01_01
0
ATMOSPHERE MEASUREMENTS
MAAT
Date of sustainable transition air temperature through 0°С
average frequency of occurrence wind speed (%)
1966-2013
average annual frequency of occurrence (%)
wind speed 1966-2013
EQUIPMENT FOR MEASUREMENTS
ATMOSPHERE MEASUREMENT PARAMETERS
Air temperature
Humidity
Wind speed and direction
Air pressure
Total precipitation
Rainfall
Snowfall
PERSPECTIVES OF STATIONS “BELYY ISLAND"
With the support of the Government of YANAO, Department of
Science and Innovation YANAO, Russian Centre of Arctic Exploration
and the Russian Academy of Sciences it is planned for the period of
2016-2020 :
• Expanding the geothermal observation network at Belyy Island
• involving Belyy Island station into the international CALM, TSP and
GTN-P projects
• Expanding the number of monitoring parameters and the
organization of integrated monitoring of the coastal dynamics
• Organization of regime hydrochemical and hydrological study of
the rivers and lakes at Belyy Island
• Anticipated expansion of biological research
• Formation of a database on all research conducted at Belyy
Island, followed by the creation of an integrated GIS
Thank you for attention!
Dmitry Drozdov
Earth Cryosphere Institute Siberian Branch Russian
Academy of Sciense
ds_drozdov@mail.ru
Pavel Orekhov
Earth Cryosphere Institute Siberian Branch Russian
Academy of Sciense
orekhov.eci@gmail.com