Ice Condition of the Laptev Sea before 1930.
نویسندگان
چکیده
منابع مشابه
Envisat Asar Monitoring of Polynya Processes and Sea Ice Production in the Laptev Sea
The Laptev Sea is one of the main source regions of sea ice in the Arctic Ocean. Most ice forms in winter in a prominent, quasi-permanent flaw lead or polynya (region of open water), separating landfast from drifting sea ice. In winter 2003/2004 we have deployed two seafloor moorings in the polynya, equipped with sensors to continuously observe ice, water, and sediment properties. In parallel, ...
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Ice export from the vast Arctic Siberian shelf is calculated using dO values and salinity data for water samples collected during the International Siberian Shelf Study between August and September 2008 (ISSS-08). The samples represent a wide range of salinities and dO values due to river water inputs and sea ice removal. We estimate the fraction of water that has been removed as ice by interpr...
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The Laptev Sea polynyas in the Siberian Arctic are well recognized as strong ice producers [1, 2] and may play a critical role with regards to sea ice volume changes in the Arctic. These flaw polynyas were studied during two seasonal cycles (2007 – 2009) by the Russian-German research project “Laptev Sea System” [3]. A focus was set on an investigation of the contribution of the West New Siberi...
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ژورنال
عنوان ژورنال: Journal of the Japanese Society of Snow and Ice
سال: 2002
ISSN: 0373-1006,1883-6267
DOI: 10.5331/seppyo.64.641