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Detection of Melt Ponds on Arctic Sea Ice with Optical Satellite Data / by Anja Rösel.

Por: Colaborador(es): Tipo de material: TextoTextoSeries Hamburg Studies on Maritime Affairs, International Max Planck Research School for Maritime Affairs at the University of Hamburg ; 25Editor: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2013Descripción: xvI, 106 páginas 45 ilustraciones, 35 ilustraciones en color. recurso en líneaTipo de contenido:
  • texto
Tipo de medio:
  • computadora
Tipo de portador:
  • recurso en línea
ISBN:
  • 9783642370335
Formatos físicos adicionales: Edición impresa:: Sin títuloClasificación LoC:
  • KZA1002-5205
Recursos en línea:
Contenidos:
Introduction -- Physical characteristics of sea ice -- Optical Remote Sensing -- Melt pond determination from Landsat satellite data -- Melt pond determination from MODIS data -- Summary and outlook -- Glossary.
Resumen: The Arctic sea ice is characterized by profound changes caused by surface melting processes and the formation of melt ponds in summer. Melt ponds contribute to the ice-albedo feedback as they reduce the surface albedo of sea ice, and hence accelerate the decay of Arctic sea ice. To quantify the melting of the entire Arctic sea ice, satellite based observations are necessary. Due to different spectral properties of snow, ice, and water, theoretically, multi-spectral optical sensors are necessary for the analysis of these distinct surface types. This study demonstrates the potential of optical sensors to detect melt ponds on Arctic sea ice. For the first time, an Arctic-wide, multi-annual melt pond data set for the years 2000-2011 has been created and analyzed.
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Springer eBooks

Introduction -- Physical characteristics of sea ice -- Optical Remote Sensing -- Melt pond determination from Landsat satellite data -- Melt pond determination from MODIS data -- Summary and outlook -- Glossary.

The Arctic sea ice is characterized by profound changes caused by surface melting processes and the formation of melt ponds in summer. Melt ponds contribute to the ice-albedo feedback as they reduce the surface albedo of sea ice, and hence accelerate the decay of Arctic sea ice. To quantify the melting of the entire Arctic sea ice, satellite based observations are necessary. Due to different spectral properties of snow, ice, and water, theoretically, multi-spectral optical sensors are necessary for the analysis of these distinct surface types. This study demonstrates the potential of optical sensors to detect melt ponds on Arctic sea ice. For the first time, an Arctic-wide, multi-annual melt pond data set for the years 2000-2011 has been created and analyzed.

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