CAJ | 학술논문

利用TOMS臭氧资料和NCAR/NCEP再分析海温资料，分析研究了斯堪的纳维亚地区的臭氧亏损状况及其季节变化规律，指出在斯堪的纳维亚地区上空存在一个严重的臭氧亏损区。该臭氧亏损有明显的季节变化：冬季最强，夏季最弱。同时研究了北大西洋海温分布和季节变化，指出其与斯堪的纳维亚地区臭氧亏损有极好的负相关。因此，认为可以用北大西洋海温的季节变化来估计斯堪的纳维亚地区气候尺度的臭氧亏损变化。
이용TOMS취양자료화NCAR/NCEP재분석해온자료，분석연구료사감적납유아지구적취양우손상황급기계절변화규률，지출재사감적납유아지구상공존재일개엄중적취양우손구。해취양우손유명현적계절변화：동계최강，하계최약。동시연구료북대서양해온분포화계절변화，지출기여사감적납유아지구취양우손유겁호적부상관。인차，인위가이용북대서양해온적계절변화래고계사감적납유아지구기후척도적취양우손변화。
The distribution and seasonal variation of ozone loss over Scandinavia are analyzed using the TOMS ozone data and NCAR/NCEP reanalysis data. It reveals that there exists a strong ozone low over the Scandinavian and its adjacent areas. The ozone low varies with the season, and changes strongest in winter and weakest in summer. The relationship of the North Atlantic surface temperature (SST) with the ozone low shows a close correlation (negative). Therefore, we may estimate the ozone loss over the Scandinavian area using the North Atlantic SST as a predictor on a global climate change.