@article{oai:nipr.repo.nii.ac.jp:00003640,
 author = {セコ, カツモト and ワダ, マコト and アオキ, シュンジ and SEKO, Katsumoto and WADA, Makoto and AOKI, Shuhji},
 journal = {Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology},
 month = {May},
 note = {P(論文), Based on the daily variation of T_b of NOAA AVHRR channel-4 data, several characteristic features of the variation of T_b in the Antarctic region were presented. Remarkable differences in the T_b variation between ocean and continent were found. The amplitude of the seasonal cycle of the T_b variation is much larger over the continent than the ocean, because of the strong inversion over the continent in winter. The short term T_b variation within 10 days over the ocean is controlled by synoptic disturbances. The T_b variation over the continent revealed longer periodicity of a few tens of days. The variation is caused by the cloud intrusion into the Antarctic continent.},
 pages = {31--42},
 title = {THE CHARACTERISTIC VARIATION OF T_b IN THE ANTARCTIC REGION REVEALED BY NOAA AVHRR CHANNEL-4 DATA},
 volume = {4},
 year = {1991}
}