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Land surface identification near Yakutsk in eastern Siberia using video images taken from a hedgehopping aircraft
Authors:R Suzuki Corresponding author  T Hiyama  J Asanuma  T Ohata
Affiliation:1. Frontier Research System for Global Change , 3173-25 Showamachi, Kanazawa-ku, Yokohama, Kanagawa 236-0001, Japan;2. Hydrospheric Atmospheric Research Center (HyARC) , Nagoya University , Nagoya 464-8601, Japan;3. Terrestrial Environment Research Center , University of Tsukuba , 1-1 Tennodai, Tsukuba, Ibaraki 305-8577, Japan;4. Institute of Low Temperature Science , Hokkaido University , Nishi-8 Kita-19, Kita-ku, Sapporo, Hokkaido 060-0819, Japan;5. Frontier Observational Research System for Global Change , 3173-25 Showamachi, Kanazawa-ku, Yokohama, Kanagawa 236-0001, Japan
Abstract:Aircraft-based remote sensing was carried out over the Lena River region (approximately 100?km horizontal scale) near Yakutsk, in eastern Siberia, on nine days between 24 April and 19 June 2000. A home-use video camera was installed on the aircraft and aerial images of the land surface were recorded. By flying at very low altitudes (100?m and 150?m), we compensated for the low resolution of the camera. In all, 5515 scenes were sampled at 10-s intervals from the video, visually interpreted, and classified. The snow/ice and water cover conditions were also interpreted. The results showed that grassland covers the riverine lowland (RLL) of the Lena River, while the principal form of land cover over the terraces is larch forest (about 61%). There was a remarkable contrast between the left (LBT) and right (RBT) bank terraces of the Lena River, no-forest areas covered 28.8% of the RBT, whereas no-forest areas covered only 13.8% of the LBT. In addition, the LBT had a greater proportion of birch forest than the RBT (15.2% vs 2.5%). The video data over eight days showed that the snow thawed first in the RLL and last in the forested areas of the LBT and RBT. An increase in the area covered by water in the RLL in mid-May was probably due to flooding by the Lena River. Distinguishing insolated from cloud-shadowed scenes of the land surface revealed that the insolation rate was lower over the LBT and RBT than over the RLL. The land-cover database created in this analysis will play an important role as basic, reliable ground-truth information for studies using satellite images.
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