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Summertime "ozone valley" over the Tibetan Plateau derived from ozonesondes and EP/TOMS data
http://hdl.handle.net/2297/12578
http://hdl.handle.net/2297/125789662f8d9-b08a-4f85-b198-f2eda96d773b
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
TE-PR-TOBO-Y-16801.pdf (1.9 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
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| 公開日 | 2017-10-03 | |||||
| タイトル | ||||||
| タイトル | Summertime "ozone valley" over the Tibetan Plateau derived from ozonesondes and EP/TOMS data | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 資源タイプ | ||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
| 資源タイプ | journal article | |||||
| 著者 |
Tobo, Yutaka
× Tobo, Yutaka× Iwasaka, Yasunobu× Zhang, Daizhou× Shi, Guangyu× Kim, Yoon-Suk× Tamura, Koichi× Ohashi, Tetsuya |
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| 提供者所属 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | 金沢大学フロンティアサイエンス機構 | |||||
| 書誌情報 |
Geophysical Research Letters 巻 35, 号 16, p. L16801, 発行日 2008-01-01 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 0094-8276 | |||||
| NCID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AA00657102 | |||||
| DOI | ||||||
| 関連タイプ | isVersionOf | |||||
| 識別子タイプ | DOI | |||||
| 関連識別子 | 10.1029/2008GL034341 | |||||
| 出版者 | ||||||
| 出版者 | American Geophysical Union (AGU) | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | During the Asian summer monsoon period, total ozone over the Tibetan Plateau is much lower than that over the surrounding areas when compared at the same latitudes. This phenomenon called the "ozone valley" was investigated continuously with the use of ozonesondes and Earth Probe/Total Ozone Mapping Spectrometer (EP/TOMS). These measurements reveal that although relatively low ozone mixing ratios extend from the troposphere to the lower stratosphere, those near the tropopause (between about 150 and 70 hPa) largely contribute to lower total ozone over the Tibetan Plateau. Temperatures near the tropopause appear to be correlated with the observed ozone changes. Meteorological analyses show that this phenomenon is accompanied by the upper level monsoon anticyclone, which is characterized by deep convection over South Asia. These results suggest that lower ozone mixing ratios and colder temperatures near the tropopause are primarily due to convection, which is linked to the Asian summer monsoon. Copyright 2008 by the American Geophysical Union. | |||||
| 著者版フラグ | ||||||
| 出版タイプ | AM | |||||
| 出版タイプResource | http://purl.org/coar/version/c_ab4af688f83e57aa | |||||
| 関連URI | ||||||
| 識別子タイプ | DOI | |||||
| 関連識別子 | http://dx.doi.org/10.1029/2008GL034341 | |||||
