AIRCRAFT MEASUREMENTS OF ATMOSPHERIC CO_2 CONCENTRATION OVER THE ANTARCTIC REGION

• Main Authors: ナカザワ タカキヨ, ムラヤマ ショウヘイ, タナカ マサユキ, アオキ シュンジ, ヤマノウチ タカシ, カワグチ サダオ, フカボリ マサシ, シオバラ マサタカ, マキノ ユキオ, Takakiyo NAKAZAWA, Shohei MURAYAMA, Masayuki TANAKA, Shuhji AOKI, Takashi YAMANOUCHI, Sadao KAWAGUCHI, Masashi FUKABORI, Masataka SHIOBARA, Yukio MAKINO
• Format: Report
• Language: English
• Published: ABSTRACT 1992
• Subjects: Antarctic; The Antarctic; Austral; Syowa Station; South Pole; Grim; Antarc*; Antarctica; E. Antarctica; Polar meteorology and glaciology; Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology; South pole
• Online Access: https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3715; http://id.nii.ac.jp/1291/00003715/; https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3715&item_no=1&attribute_id=18&file_no=1

Aircraft measurements of the atmospheric CO_2 concentration over Syowa Station (69°00'S, 39°35'E), Antarctica have been continued since January 1983,except in 1985 and 1988. Since the data obtained so far are still insufficient and the measurements were not made in all seasons of all years, there is some uncertainty in the results. Nevertheless, preliminary inspection of the data shows that : (1) the maximum and minimum concentrations of the average seasonal CO_2 cycle in the lower and middle troposphere appear early in October and in mid-April, respectively; (2) in the upper troposphere, the maximum and minimum occur late in September and early in May, respectively; (3) the peak-to-peak amplitude of the seasonal cycle decreases slightly with height except near the ground surface; (4) the CO_2 concentration increases gradually with height the year and the height-dependent difference of the concentration is smaller in austral winter and spring than in remaining seasons of the year. From comparison with the results of ground-fixed measurements at the South Pole and Cape Grim, Tasmania and other aircraft measurements, it is suggested that the northern hemispheric air with high CO_2 concentration is transported to the Antarctic region through the upper troposphere from austral winter to spring, while air with low CO_2 concentration is transported from southern middle latitudes into the Antarctic region through the lower troposphere in remaining seasons.