The dynamics of the development of the Lena polynya forming in the Laptev Sea and its impact on navigation conditions in the Arctic, in the Laptev Sea, is investigated. The hypothesis is tested that the timing of polynya may have a significant impact on its average growth rate. The results of the GLORYS12v1 global reanalysis and standard methods of mathematical statistics were used in this test. The validity of the hypothesis was confirmed by the example of the section of the polynya located at the mouth of the major navigable channel of the Lena delta Bykovskaya. Stable tendencies of changing the dates of the polynya formation towards earlier dates in the modern period have been revealed. A high probability of improvement of navigation con...
Synoptic weather systems in the Arctic are studied using a track algorithm based on a feature-tracki...
A simple polynya flux model driven by standard atmospheric forcing is used to investigate the ice fo...
Processes of the exchange of energy and momentum at the sea ice-ocean-atmosphere interface are key p...
Problem of improving the quality of medium- and long-term forecasting of changes in ice conditions i...
Radical environmental changes are forecasted to occur in the Shelf areas of the Siberian Arctic duri...
Polynyas in the Laptev Sea are examined with respect to recurrence and interannual wintertime ice pr...
The Russian icebreaker KAPITAN DRANITSYN carried out the TRANSDRIFT III expedition to the Laptev Sea...
Sea ice is an important vehicle for sediment transport in the Arctic Ocean. On the Laptev Sea shelf ...
Polynyas in the Laptev Sea are examined with respect to recurrence and inter-annual wintertime ice p...
This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the sou...
The ablation of Arctic sea ice makes seasonal navigation possible in the Arctic region, which accoun...
A detailed analysis of hydrographic data from a period of 20 years (1980 99) has shown that the pers...
As a key region of Northeast Passage, the polynya along the Siberian coast in the East Siberian and ...
The hydrography of the Laptev Sea is significantly influenced by river water and sea-ice processes, ...
In this paper we present new data from ship-based measurements and two-year observations from moorin...
Synoptic weather systems in the Arctic are studied using a track algorithm based on a feature-tracki...
A simple polynya flux model driven by standard atmospheric forcing is used to investigate the ice fo...
Processes of the exchange of energy and momentum at the sea ice-ocean-atmosphere interface are key p...
Problem of improving the quality of medium- and long-term forecasting of changes in ice conditions i...
Radical environmental changes are forecasted to occur in the Shelf areas of the Siberian Arctic duri...
Polynyas in the Laptev Sea are examined with respect to recurrence and interannual wintertime ice pr...
The Russian icebreaker KAPITAN DRANITSYN carried out the TRANSDRIFT III expedition to the Laptev Sea...
Sea ice is an important vehicle for sediment transport in the Arctic Ocean. On the Laptev Sea shelf ...
Polynyas in the Laptev Sea are examined with respect to recurrence and inter-annual wintertime ice p...
This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the sou...
The ablation of Arctic sea ice makes seasonal navigation possible in the Arctic region, which accoun...
A detailed analysis of hydrographic data from a period of 20 years (1980 99) has shown that the pers...
As a key region of Northeast Passage, the polynya along the Siberian coast in the East Siberian and ...
The hydrography of the Laptev Sea is significantly influenced by river water and sea-ice processes, ...
In this paper we present new data from ship-based measurements and two-year observations from moorin...
Synoptic weather systems in the Arctic are studied using a track algorithm based on a feature-tracki...
A simple polynya flux model driven by standard atmospheric forcing is used to investigate the ice fo...
Processes of the exchange of energy and momentum at the sea ice-ocean-atmosphere interface are key p...