Add to ORKGFormation of heavy bottom water through rejection of brine during ide freezing is a regular phenomenon in the Barents Sea, particular on the Novaya Zemlya shelf, but also observed in other shallow localities of the sea. Water with temperature around -1°C and salinity above 34.95 is found moving eastwards on the southern side of the Novaya Zemlya-Franz Josef Land Channel which communicates with the Polar Sea. The relative high salinity is a result of admixture from heavy water formed during the freezing process
The northern Barents Sea is a cold, seasonally ice-covered Arctic shelf sea region that has experien...
Reports results of re-appraisal and interpretation of data from 74 oceanographic stations (of >40...
[1] Formation process of the dense shelf water (DSW) in the Sea of Okhotsk was investigated with an ...
Formation of heavy bottom water through rejection of brine during ide freezing is a regular phenome...
Dense water masses from Arctic shelf seas are an important part of the Arctic thermohaline system. W...
Dense water masses from Arctic shelf seas are an important part of the Arctic thermohaline system. W...
Dense water masses from Arctic shelf seas are an important part of the Arctic thermo-haline system. ...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
Formation of homogeneous water was observed in the surface layer above a depth of 400m in the Ongul ...
Deep water formation may be triggered by the density effect of brines that are released during sea-i...
The maximum dense shelf water salinity formed during winter in the Svalbard Bank area of the north-w...
The northern Barents Sea is a cold, seasonally ice-covered Arctic shelf sea region that has experien...
Reports results of re-appraisal and interpretation of data from 74 oceanographic stations (of >40...
[1] Formation process of the dense shelf water (DSW) in the Sea of Okhotsk was investigated with an ...
Formation of heavy bottom water through rejection of brine during ide freezing is a regular phenome...
Dense water masses from Arctic shelf seas are an important part of the Arctic thermohaline system. W...
Dense water masses from Arctic shelf seas are an important part of the Arctic thermohaline system. W...
Dense water masses from Arctic shelf seas are an important part of the Arctic thermo-haline system. ...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
The Barents Sea throughflow accounts for approximately half of the Atlantic Water advection to the A...
Formation of homogeneous water was observed in the surface layer above a depth of 400m in the Ongul ...
Deep water formation may be triggered by the density effect of brines that are released during sea-i...
The maximum dense shelf water salinity formed during winter in the Svalbard Bank area of the north-w...
The northern Barents Sea is a cold, seasonally ice-covered Arctic shelf sea region that has experien...
Reports results of re-appraisal and interpretation of data from 74 oceanographic stations (of >40...
[1] Formation process of the dense shelf water (DSW) in the Sea of Okhotsk was investigated with an ...