{"created":"2023-06-20T13:21:27.986631+00:00","id":1681,"links":{},"metadata":{"_buckets":{"deposit":"8ebbc4f7-e86a-43ed-911d-53c914cf6cbb"},"_deposit":{"created_by":21,"id":"1681","owners":[21],"pid":{"revision_id":0,"type":"depid","value":"1681"},"status":"published"},"_oai":{"id":"oai:ir.soken.ac.jp:00001681","sets":["2:429:18"]},"author_link":["0","0","0"],"item_1_creator_2":{"attribute_name":"著者名","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"宮川, 幸治"}],"nameIdentifiers":[{}]}]},"item_1_creator_3":{"attribute_name":"フリガナ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"ミヤガワ, コウジ"}],"nameIdentifiers":[{}]}]},"item_1_date_granted_11":{"attribute_name":"学位授与年月日","attribute_value_mlt":[{"subitem_dategranted":"2010-03-24"}]},"item_1_degree_grantor_5":{"attribute_name":"学位授与機関","attribute_value_mlt":[{"subitem_degreegrantor":[{"subitem_degreegrantor_name":"総合研究大学院大学"}]}]},"item_1_degree_name_6":{"attribute_name":"学位名","attribute_value_mlt":[{"subitem_degreename":"博士（理学）"}]},"item_1_description_12":{"attribute_name":"要旨","attribute_value_mlt":[{"subitem_description":"　　　The OH Meinel band emissions are the brightest night airglow emissions in the near-infrared regions, and peak at mesopause altitudes. Since the intensity distribution in these vibration-rotation bands is quickly equalized to that determined by the local kinetic temperature, the OH rotational temperature can be derived from the spectrum of OH airglow. This technique has been widely used as a conventional and reliable method of temperature measurement in the mesopause region, especially in the middle- and low-latitude regions. However, it is known to be difficult to apply in the polar regions, because auroral emissions contaminate OH airglow spectra. There are a few examples of OH rotational temperature observations conducted in Antarctic for the purposes of studying the relationship between aurora activity and OH rotational temperature. However, highly energetic auroral electrons can reach altitudes just below the mesopause (～90 km) and can cause heating of the neutral atmosphere at that altitude. There are virtually no previous reports that show a quantitative relationship between auroral precipitations and OH rotational temperature.<br />  　　　A fast high-resolution spectrometer designed specifically to observe the spectrum of the OH vibrational-rotational band in the auroral zone has been developed. The OH 8-4 band around the 950-nm wavelength region in the nightglow spectrum was  selected as the most suitable vibration-rotation band for observation in polar regions, based on Arctic survey observations. Its suitability lies in the fact that it is less susceptible to contamination from strong auroral emission. The new spectrometer comprises a fast optical system, a transmission grating and a CCD camera. The operating spectral region just encompasses the OH 8-4 band (900-990 nm) and a moderate spectral resolution of 0.27 nm is realized. A back-illuminated CCD with an infrared-enhanced quantum efficiency (QE) is used as the imaging device. The sensitivity and spectral resolution of the spectrometer were calibrated at the National Institute of Polar Research (NIPR). The instrument was installed in the Optical Building at Syowa Station in February, 2008 by the 49th Japanese Antarctic Research Expedition. The instrumental field-of-view of 4.5 x 0.007 deg is centered on the local magnetic zenith. The nominal exposure time is 1 min.<br /> 　　　The total dataset consists of observations over 153 nights during the 2008 austral winter season at Syowa Station. The dataset shows both short-term (several minutes) and long-term seasonal) variations. Typical temperature trends (high in winter and low in summer) in the polar mesopause region are also evident. These trends are very similar to those observed at the Davis Station which is located at nearly the same latitude as the Syowa Station. In addition to the seasonal trend, large-scale heating and cooling is seen over a period of several days.  Short-term variations which relate to auroral activity can also be observed. Only six nights of data was found to be suitable, in terms of weather conditions and auroral activity, to study the relationship between auroral precipitations and OH airglow variations. In particular, a significant increase in the rotational temperature and a decrease in the airglow intensity related to auroral activity were identified on the night of March 27-28, 2008, but no such variations were seen on other nights. The horizontal magnetic-field disturbance on the night of March 27-28 was the largest observed during the entire winter, and cosmic radio noise absorption was also very strong. These facts indicate that a large flux of high-energy auroral particles precipitated during this night. It is suggested that the observed variations in the OH rotational temperature and airglow intensity were caused by a lowering of the average airglow altitude as a result of OH depletion in the upper part of the layer where high-energy auroral particles can reach.<br /> 　　　Although in normal auroral activity there are no auroral effects, this study reveals the occurrence of rapid fluctuations related to very high auroral activity or hard particle precipitation in the polar mesopause region.","subitem_description_type":"Other"}]},"item_1_description_18":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_1_description_7":{"attribute_name":"学位記番号","attribute_value_mlt":[{"subitem_description":"総研大乙第200号","subitem_description_type":"Other"}]},"item_1_select_14":{"attribute_name":"所蔵","attribute_value_mlt":[{"subitem_select_item":"有"}]},"item_1_select_8":{"attribute_name":"研究科","attribute_value_mlt":[{"subitem_select_item":"複合科学研究科"}]},"item_1_select_9":{"attribute_name":"専攻","attribute_value_mlt":[{"subitem_select_item":"16 極域科学専攻"}]},"item_1_text_10":{"attribute_name":"学位授与年度","attribute_value_mlt":[{"subitem_text_value":"2009"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"MIYAGAWA, Koji","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-02-17"}],"displaytype":"simple","filename":"乙200_要旨.pdf","filesize":[{"value":"437.2 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"要旨・審査要旨","url":"https://ir.soken.ac.jp/record/1681/files/乙200_要旨.pdf"},"version_id":"597b611d-3235-4fcc-a9b9-eae4061f1619"},{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-02-17"}],"displaytype":"simple","filename":"乙200_本文.pdf","filesize":[{"value":"13.4 MB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"本文","url":"https://ir.soken.ac.jp/record/1681/files/乙200_本文.pdf"},"version_id":"d56dd965-d4a6-4fd2-a1bc-2f7ec8d7a7df"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"thesis","resourceuri":"http://purl.org/coar/resource_type/c_46ec"}]},"item_title":"A study on depletion of the upper stratospheric ozone in the Antarctic from Umkehr ozone profile","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"A study on depletion of the upper stratospheric ozone in the Antarctic from Umkehr ozone profile"},{"subitem_title":"A study on depletion of the upper stratospheric ozone in the Antarctic from Umkehr ozone profile","subitem_title_language":"en"}]},"item_type_id":"1","owner":"21","path":["18"],"pubdate":{"attribute_name":"公開日","attribute_value":"2011-01-18"},"publish_date":"2011-01-18","publish_status":"0","recid":"1681","relation_version_is_last":true,"title":["A study on depletion of the upper stratospheric ozone in the Antarctic from Umkehr ozone profile"],"weko_creator_id":"21","weko_shared_id":-1},"updated":"2023-06-20T15:57:10.017248+00:00"}