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- W1664340655 abstract "Sea ice cover plays an important role in the Earth climate system because, i) it controls the ice-albedo feedback mechanism that amplifies the climate response at high latitude regions. ii) growth (melt) rate affects the salt (freshwater) flux from sea ice that is significant to global ocean circulation and deep water formation. iii) due to relatively thin ice floating on the deep ocean, it interacts with winds and ocean currents. Resulting sea ice dynamics and circulation are responsible for the ice and freshwater transport in (and export from) the Arctic Ocean. iv) sea ice alters the surface heat and mass budget in the Arctic Ocean, which greatly depend on ice thickness. Clearly, sea ice processes span a wide range of scales from micrometer to thousands of kilometres and a wide range of disciplines. Despite about 200 years of research and observations, the evolution of sea ice and its position in the climate system is not completely understood. Therefore, the prediction of the future climate is unreliable. More observations are required for smalland large-scale processes at longer and continuous time-series. But, field campaigns in the Arctic are challenging due to the complex extreme environment and its inaccessibility. Hence, remote sensing techniques are crucial as they can provide global homogeneous coverage and continuous time-series." @default.
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- W1664340655 date "2009-05-01" @default.
- W1664340655 modified "2023-09-24" @default.
- W1664340655 title "Arctic sea ice Freeboard Heights From ICESat Laser Altimetry" @default.
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