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THE ARCTIC EXPEDITIONS IN THE 19TH CENTURY
POLAR EXPLORERS (THE 19TH – EARLY 20TH CENTURY) AND CURRENT EXPEDITIONSIN THE ARCTIC (THE 21ST CENTURY)
N.N. Zubov
THE ARCTIC ICE«Glavsevmorput»Publishing-House
Moscow, 1941
Sea Ice Conditions along the Northern Sea Route in the middle of September 1936
THE VEGA CRUISE (July 1878 – July 1879)
MMBI KSC RAS AND SSC RAS RESEARCH IN THE ANTARCTIC IN 2007–2009RESEARCH STATION «BELLINSGAUZEN»
THE MANYCH-KERCH STRAIT IN THE EPOCH OF EXTREME FLOODS DURING THE MELT OF THE SCANDINAVIAN GLACIER
Matishov, G.G. (1987). The World Ocean and the Earth’s Glaciation. Moscow. Mysl’
ACTIVITIES ON THE ATLAS OF CLIMATIC CHANGES(LMEs OF THE RUSSIAN ARCTIC)
Sea Of Azov 153 000+ stationsCaspian Sea 43 000+ stationsBlack Sea 83 000+ stations
WATER TEMPERATURE OBSERVATIONS IN THE BARENTS SEA
17000 stations1938-2002
33000 stations1880-2007
April August
THE BARENTS SEA DATABASE(JANUARY 2013)
NOAA, MMBI KSC RAS, SSC RAS
DATABASE TOFORECAST INNER-
SECULAR FLUCTUATIONS
OF CLIMATE
43 357 STATIONS
42 519 STATIONS
Distribution of Stations
(Measurements of Water
Temperature in the West Bering
Sea LME)
Period:From ХХХХ to
ХХХХ
47 298 stations
SEASONAL FIELDS OF TEMPERATURE AND SALINITY
COLD RECORD IN THE ARCTIC. ICE IN THE BERING SEA REMAINED FOR
MORE THAN 100 DAYS
CHART OF THE ICE SITUATION
IN THE CASPIAN SEA, 14-15.02.2012
25 MARCH 2012
Water temperature
Maximum (in a warm period)
Minimum (in a cold period)
Air temperature
The freeze-up duration
BEGINNING OF THE FREEZE-UP
IN THE TAGANROG BAY (THE SEA OF AZOV) IN
THE EARLY 21st CENTURY
EXTREMELY SEVERE WINTERSIN THE SEA OF AZOV
(44 – 47° N.L.)26 March 2012 11 April 2012
ACTUAL SITUATION OF THE SIBERIAN ANTICYCLONE DEVELOPMENT AND SHIFT TOWARDS THE SOUTHWEST
(17.01.-25.02 2012)(Source: http://www.uni-koeln.de/math-nat-fak/geomet/meteo)
MEAN NEAR-LAND (SURFACE) TEMPERATUREDURING THE PERIOD OF 19.01.12 – 19.02.12
ICE COVERAS OF 12.02. – 18.02.2012
MINIMUM VALUE OF TEMPERATURE FOR 30 DAYS
«VOEIKOV AXIS» («WIND RIDGE») – EUROPEAN SPUR OF THE SIBERIAN ANTICYCLONE
Prevailing wind directions in January
Mean air pressure at the sea level in January in millibars
ABNORMAL ADVECTION
of the Western spur of the Siberian
Anticyclone towards the Pyrenees and of
the Gulfstream towards the Franz
Josef Land
February 2012
INNER-SECULAR CYCLICITY OF CLIMATELong-term temperature and salinity pattern in the Barents Sea. Layer of 0-50 m.
Matishov G., Matishov D., Moiseev D. INFLOW OF ATLANTIC-ORIGIN WATERS TO THE BARENTS SEA ALONG GLACIAL TROUGHS//OCEANOLOGIA, 2009, 51(3)
Матишов Г. Г. ВЛИЯНИЕ ИЗМЕНЧИВОСТИ КЛИМАТИЧЕСКОГО И ЛЕДОВОГО РЕЖИМОВ НА СУДОХОДСТВО//ВЕСТНИК РАН, 2008, 78 (10)
Formation of freshet flows and
floods in water catchment basins
NEAR BOTTOM TEMPERATURE AND FISH DIVERSITY (LATITUDE 70◦, DEPTH OF 250 M)
FEEDING OF VARIOUS SIZE-AGE GROUPS OF BLACK HALIBUT IN THE KARA SEA WATER AREA, 2007 –
2011
A – Southern part of St. Anna Trough
B – Western part of St. Anna Trough
C – Eastern part of St. Anna Trough
D – Western part of Voronin Trough
(Sentyabov, Smirnov, 2010)
ABUNDANCE INCREASE OF THE RED KING (KAMCHATKA) CRAB IN THE BARENTS SEA DUE TO THE WARMING IN THE EARLY 21st CENTURY (BY MMBI KSC RAS AND
PINRO DATA)
SHIFT (DELAY) BY BENTHOS BIOMASS PHASE RELATED TO TEMPERATURE AT THE KOLA TRANSECT
DECREASING DYNAMICS OF GOODS’ TRANSPORTATION ALONG THE NORTHERN SEA ROUTE
(MLN. TONS)
Transportation of ore to China
POPULATION DYNAMICS OF MURMANSKREGION AND MURMANSK
Murmansk Region Murmansk
Thousand people Heads, Regional AdministrationDenisov, G.Ya. Konovalov, L.N. Ptitsyn, V.N. Serokurov, S.L.
Balagurov, A.K. Komarov, E.B. Evdokimov, Yu.A. Dmitrienko, D.V.
Kovtun, M.V.
STOCKMAN PROJECT:MIRAGE OR REALITY?
DEVELOPMENT AND APPROBATION OF A NEW TECHNOLOGY«ON-LINE BIOMONITORING OF THE STATE OF MARINE ENVIRONMENT»
(Dalnezelenetskaya Bay, joint project (TOTAL – MMBI KSC RAS – Akvaplan-niva – University of Bordeaux)
Registration of changes in the movements of the shells of mollusks (mussels and scallops) is continuous and on-line.
In case significant changes are registered, an alarm signal is generated.
OIL AND GAS DEPOSITS(THE YAMAL PENINSULA AND SHELF)
Proposed New Boundaries of the Arctic LMEs(H.R. Skjoldal, Tromso, Norway, January 2011)
Seismic-Acoustic Impact
Impact of Suspension and Drilling Solutions
Impact of Noise produced by Large-Tonnage Vessels
Impact of Water Pumping Impact of Oil
TYPES OF IMPACT ON LMEs
SEA ICE IN THE EAST-SIBERIAN SEAIN AUGUST – A SIGN OF COOLING IN THE ARCTIC
2012 ICE FREE AREA IN AUGUST 20112011
2013 January 29-31 2012 January 15-17
www.aari.ru www.aari.ruIce free
area
ICE SITUATION IN THE ARCTIC
TYPES OF CLIMATEin the period of 1951 – 2010
(The Kola Transect, layer of 0-200 m)
TYPE OF YEAR CRITERION OF THERMAL STATE
Abnormally cold ‐ Δ T °C ˃ 1.5 σ
Cold 0.5 σ < ‐ Δ T °C ≤ 1.5 σ
Averaged/regular ± Δ T °C ≤ 0.5 σ
Warm 0.5 σ < Δ T °C ≤ 1.5 σ
Abnormally warm Δ T °C ˃ 1.5 σ
Δ T – anomaly of water temperatureσ = 0.51 °C – mean quadrate deviation of water temperature for the period of 1951‐2010
INTERNATIONAL COOPERATION
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