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Investigation of vertical wavenumber spectra during sudden stratospheric warming (SSW) events over the Indian region

机译:印度地区突然平流层变暖(SSW)事件中垂直波数谱的研究

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摘要

The vertical wavenumber (VWN) characteristics during sudden stratospheric warming (SSW) events (2003-2016) is investigated for the first time using temperature observation of Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) onboard Thermosphere Ionosphere Mesosphere Energetics Dynamics (TIMED) satellite (for the altitude range of 20-70 km) and ERA-lnterim reanalysis data (for the altitudes of 0.1-20 km). Highly negative VWN spectral slope value (approximately) of -4.82 (at 25° N, 77° E) and -4.41 (at 35° N, 77° E) at 40-50 km altitude is observed during the 2013 SSW event, a sort of which is not perceived in any other SSW events (2003-2016). The combined effect of planetary waves (PWs) with wavenumber 1 and 2 during 2013 SSW may be responsible for such distinctive observation near the peak temperature altitude. This study elicits the importance of polar vortex portraying that lower latitudes are affected if only the vortex splits and presents the first of its kind VWN characteristics during SSW events.
机译:使用宽带排放辐射测量(SABR)船上热圈电离层Messephyshey动态(定时)首次使用温度观察突然平流层变暖(SSW)事件(SSW)事件(2003-2016)期间的垂直波数(SSW)事件(2003-2016)的特性进行研究卫星(适用于20-70公里的高度范围)和ERA-LNTERIM再分析数据(适用于0.1-20 km的海拔。在2013年SSW事件期间观察到,在2013年SSW事件中观察到高度负VWN光谱斜率(大约)的-4.82(在25°N,77°E)和-4.41(在35°N,77°E)中,其中不在任何其他SSW事件中被察觉(2003-2016)。行星波(PWS)与波数1和2在2013 SSW期间的组合效果可能负责峰值温度高度附近的这种独特观察。本研究引发了极地涡流描绘的重要性,如果只有涡流分裂,并且在SSW事件期间仅提供其第一个VWN特性,因此仅受到较低的纬度受到影响。

著录项

  • 来源
    《Remote sensing letters》 |2019年第9期|699-708|共10页
  • 作者单位

    Space and Atmospheric Sciences Division Physical Research Laboratory Ahmedabad India;

    Space and Atmospheric Sciences Division Physical Research Laboratory Ahmedabad India;

    Center for Basic Sciences Pt. Ravishankar Shukla University Raipur India;

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  • 正文语种 eng
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