Determination of sea ice concentration from AVHRR visible and near infrared imagery

Sea ice concentrations are determined from the visible and near infrared albedo of the AVHRR imagery. One method uses only one channel data to interpolate the ice concentration between 0 and 100% corresponding to the open water and the snow cover, respectively. This method yieds an uncertainty owing...

Full description

Saved in:
Bibliographic Details
Published inNankyoku shiryo Vol. 30; no. 2; pp. 89 - 102
Main Authors Takashi Yamanouchi, Kazuya Suzuki, Masatoshi Matsushita, Masanobu Shimizu, Yasuhiko Naito
Format Journal Article
LanguageEnglish
Published National Institute of Polar Research 01.07.1986
Online AccessGet full text

Cover

More Information
Summary:Sea ice concentrations are determined from the visible and near infrared albedo of the AVHRR imagery. One method uses only one channel data to interpolate the ice concentration between 0 and 100% corresponding to the open water and the snow cover, respectively. This method yieds an uncertainty owing to the variation of albedo by the surface condition change. Another method uses two-channel data to derive not only the ice concentration but also the ice surface condition and can eliminate uncertainties involved in the first method. The ice surface condition is expressed by "snow coverage". Air photographs are compared with the satellite data. They are helpful to discuss the surface condition of sea ice. Time variations of the concentration and surface condition of summer sea ice are discussed.
ISSN:0085-7289
2432-079X
DOI:10.15094/0000850