The transpolar drift as a source of riverine and shelf‐derived trace elements to the central Arctic Ocean
A major surface circulation feature of the Arctic Ocean is the Transpolar Drift (TPD), a current
that transports river‐influenced shelf water from the Laptev and East Siberian Seas toward …
that transports river‐influenced shelf water from the Laptev and East Siberian Seas toward …
Using fluorescent dissolved organic matter to trace and distinguish the origin of Arctic surface waters
Climate change affects the Arctic with regards to permafrost thaw, sea-ice melt, alterations to
the freshwater budget and increased export of terrestrial material to the Arctic Ocean. The …
the freshwater budget and increased export of terrestrial material to the Arctic Ocean. The …
From fresh to marine waters: Characterization and fate of dissolved organic matter in the Lena River Delta Region, Siberia
Connectivity between the terrestrial and marine environment in the Artic is changing as a
result of climate change, influencing both freshwater budgets, and the supply of carbon to …
result of climate change, influencing both freshwater budgets, and the supply of carbon to …
Thin and transient meltwater layers and false bottoms in the Arctic sea ice pack—Recent insights on these historically overlooked features
Estimates of ground-level ozone concentrations have been improved through data fusion of
observations and atmospheric chemistry models. Our previous global ozone estimates for …
observations and atmospheric chemistry models. Our previous global ozone estimates for …
Seasonality of the physical and biogeochemical hydrography in the inflow to the Arctic Ocean through Fram Strait
Eastern Fram Strait and the shelf slope region north of Svalbard is dominated by the
advection of warm, salty and nutrient-rich Atlantic Water (AW). This oceanic heat contributes …
advection of warm, salty and nutrient-rich Atlantic Water (AW). This oceanic heat contributes …
Darkening of the Svalbard fjords waters observed with satellite ocean color imagery in 1997–2019
M Konik, M Darecki, AK Pavlov, S Sagan… - Frontiers in Marine …, 2021 - frontiersin.org
Global warming is not often discussed in the context of light availability within the water
column. However, the light regimes in the Arctic Ocean are controlled by three factors that …
column. However, the light regimes in the Arctic Ocean are controlled by three factors that …
[PDF][PDF] Биооптические характеристики морей, омывающих берега западной половины России, по данным спутниковых сканеров цвета 1998-2017 гг
ОВ Копелевич, ИВ Салинг, СВ Вазюля… - М.: ООО «ВАШ …, 2018 - researchgate.net
Представленная монография подводит итог работы, проведенной сотрудниками
Лаборатории оптики океана Института океанологии им. ПП Ширшова РАН (ИО РАН) по …
Лаборатории оптики океана Института океанологии им. ПП Ширшова РАН (ИО РАН) по …
[HTML][HTML] Surface desalinated layer distribution in the Kara Sea determined by shipboard and satellite data
DI Glukhovets, YA Goldin - Oceanologia, 2020 - Elsevier
This study reports the propagation dynamics of the Kara Sea surface desalinated layer
(SDL) during the summer and autumn seasons. We analysed shipboard measurements data …
(SDL) during the summer and autumn seasons. We analysed shipboard measurements data …
Unexpected winter phytoplankton blooms in the North Atlantic subpolar gyre
In mid-and high-latitude oceans, winter surface cooling and strong winds drive turbulent
mixing that carries phytoplankton to depths of several hundred metres, well below the sunlit …
mixing that carries phytoplankton to depths of several hundred metres, well below the sunlit …
Light in the polar night
How much light is available for biological processes during Polar Night? This question
appears simple enough. But the reality is that conventional light sensors for measuring …
appears simple enough. But the reality is that conventional light sensors for measuring …