The East Siberian Sea as a transition zone between Pacific‐derived waters and Arctic shelf waters
- 26 May 2005
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 32 (10)
- https://doi.org/10.1029/2005gl022490
Abstract
No abstract availableThis publication has 10 references indexed in Scilit:
- Characterization of Siberian Arctic coastal sediments: Implications for terrestrial organic carbon exportGlobal Biogeochemical Cycles, 2004
- The Organic Carbon Cycle in the Arctic OceanPublished by Springer Nature ,2004
- Organic carbon isotope ratios (δ 13 C) of Arctic Amerasian Continental shelf sedimentsInternational Journal of Earth Sciences, 2000
- A climate shift in seasonal values of meteorological and hydrological parameters for Northeastern AsiaProgress in Oceanography, 2000
- Thermokarst and land-ocean interactions, Laptev sea region, RussiaPermafrost and Periglacial Processes, 2000
- The Dispersion of Siberian River Flows into Coastal Waters: Meteorological, Hydrological and Hydrochemical AspectsPublished by Springer Nature ,2000
- Distribution of Atlantic and Pacific waters in the upper Arctic Ocean: Implications for circulationGeophysical Research Letters, 1998
- Two circulation regimes of the wind‐driven Arctic OceanJournal of Geophysical Research: Oceans, 1997
- Physical and geochemical properties across the Atlantic/Pacific water mass front in the southern Canadian BasinJournal of Geophysical Research: Oceans, 1996
- Carbon and nitrogen cycling within the Bering/Chukchi Seas: Source regions for organic matter effecting AOU demands of the Arctic OceanProgress in Oceanography, 1989