Physical and stable isotopic properties and growth processes of sea ice collected in the southern Sea of Okhotsk
- 15 September 2000
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 105 (C9) , 22083-22093
- https://doi.org/10.1029/1999jc000013
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- WOCE line P1W in the Sea of Okhotsk: 2. CFCs and the formation rate of intermediate waterJournal of Geophysical Research: Oceans, 1998
- WOCE section P1W in the Sea of Okhotsk: 1. Oceanographic data descriptionJournal of Geophysical Research: Oceans, 1998
- Winter snow cover on sea ice in the Weddell SeaJournal of Geophysical Research: Oceans, 1997
- The origin of the North Pacific Intermediate WaterJournal of Geophysical Research: Oceans, 1997
- Influence of Okhotsk sea‐ice extent on atmospheric circulationGeophysical Research Letters, 1996
- Characteristics and distribution patterns of snow and meteoric ice in the Weddell Sea and their contribution to the mass balance of sea iceAnnales Geophysicae, 1994
- Crystal structure, stable isotopes (δ18O), and development of sea ice in the Ross, Amundsen, and Bellingshausen seas, AntarcticaJournal of Geophysical Research: Oceans, 1994
- An Okhotsk Sea water anomaly: implications for ventilation in the North PacificDeep Sea Research Part A. Oceanographic Research Papers, 1991
- Hydrogen and oxygen isotope fractionation between ice and waterThe Journal of Physical Chemistry, 1968
- Stable isotopes in precipitationTellus, 1964