Moored meteorological buoy as part of national green-house monitoring system in the Barents Sea

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Abstract

Experimental deployment of surface meteorological moored buoy “Sea-Air-Wave Station” (SAWS) was performed during the expedition “European Arctic – 2024: a geologic annals of environmental and climate change” (96th cruise of RV “Akademik Mstislav Keldysh”) in the north-eastern part of the Barents Sea. Mooring design and instrumentation demonstrated validity of the meteorological buoy for usage as part of National green-house monitoring system.

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About the authors

V. D. Sharmar

Shirsov Institute of Oceanology RAS

Author for correspondence.
Email: sharmar@sail.msk.ru
Russian Federation, Moscow

V. P. Tereschenkov

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

A. V. Gavrikov

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

A. V. Sinitzin

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

M. D. Kravchishina

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

A. A. Klyuvitkin

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

A. N. Novigatsky

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

N. D. Tilinina

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

S. V. Pisarev

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

S. V. Pisarev

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

S. K. Gulev

Shirsov Institute of Oceanology RAS

Email: sharmar@sail.msk.ru
Russian Federation, Moscow

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2. Fig. 1. a) Sea-Air-Wave hydrometeorological Station before installation at station No. 8012, depth 164 m. b) Bottom topography in the section from Novaya Zemlya Island (A) to the islands of Franz Josef Land (B).

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3. Fig. 2. Wind wave parameters measured by the SeaView SVS-603 sensor: significant wave height (a) and average period (b) in comparison with independent synchronous observations obtained using the Spotter wave measuring buoy during the period of setting the buoy from July 31 to August 18, 2024.

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4. 3. Wind speed (according to the Vaisala 05106 sensor) and CO2 concentrations in the drive air layer (according to the Vaisala GMP 343 sensor) and in the surface water layer (according to the AMT CO2 sensor).

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