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Climatology and annual displacement of the upper-level frontal zones in the middle troposphere of the Northern Hemisphere

机译：北半球中部对流层中层额处地区的气候学和年代位移

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O. A. Razorenova; P. A. Shabanov;
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年度 2019
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1. Climatology and Interannual Movements of Upper-Level Frontal Zones in the Middle Troposphere of the Northern Hemisphere [J] . Razorenova O. A., Shabanov P. A. Doklady Earth Sciences . 2019,第PTa2期

机译：北半球中部对流层中层额处地区的气候学和际运动
2. Winter climatology of upper-level frontal zones in the Northern Hemisphere [J] . Razorenova O. A. Russian meteorology and hydrology . 2016,第1期

机译：北半球上层锋区的冬季气候
3. Evidence of a LNO_X influence on middle/upper troposphere ozone‐mixing ratios at Dakar, Senegal during Northern Hemisphere summer season [J] . Gregory S. Jenkins, Moussa Gueye, Mamadou S. Drame, Atmospheric science letters . 2014,第3期

机译：在北半球夏季，LNO _{X 对塞内加尔达喀尔中/上对流层臭氧混合比的影响的证据}
4. The Recent Variability of Atmospheric Ozone in the Middle Latitudes of the Northern Hemisphere and Solar Ultraviolet Radiation [C] . Christos S. Zerefos NATO Advanced Study Institue on Atmospheric Ozone as a Climate Gas . 1995

机译：北半球中部纬度近期大气臭氧变异性，太阳紫外线辐射
5. Classification of Northern Hemisphere stratospheric ozone and water vapor profiles by meteorological regime: Validation, climatology, and trends. [D] . Follette, Melanie Beth. 2007

机译：通过气象制度对北半球平流层臭氧和水蒸气剖面的分类：验证，气候学和趋势。
6. Multi-year composite view of ozone enhancements and stratosphere-to-troposphere transport in dry intrusions of northern hemisphere extratropical cyclones [O] . Lyatt Jaeglé, Robert Wood, Krzysztof Wargan -1

机译：北半球温带气旋干侵入中臭氧增强和平流层至对流层运输的多年综合观点
7. ANNUAL CHANGE IN FRONTAL ZONES IN THE NORTHERN HEMISPHERE [O] . Minoru YOSHIMURA 1967

机译：北半球正面区域的年度变化
8. Role of the Middle Atmosphere in Simulations of the Troposphere during Northern Hemisphere Winter: Differences between High- and Low-Top Models [R] . Sassi, F., Garcia, R. R., Marsh, D., 2010

机译：中北大气在北半球冬季对流层模拟中的作用：高低模型之间的差异

Climatology and annual displacement of the upper-level frontal zones in the middle troposphere of the Northern Hemisphere

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