UV Transient Atmospheric Events Observed Far From Thunderstorms by the Vernov Satellite

Usually a thunderstorm region with lightning activity is necessary for the formation of known types of upper atmospheric transient luminous events (TLEs: sprites, emission of light and very low frequency perturbation, blue jets, etc.) with well-recognizable visible emissions. However, some “far-from-thunderstorm” transient events have been detected in some experiments. Measurements of transient atmospheric events (TAEs) were made on board the Vernov satellite by the sensitive UV and IR detector. Remote observation from the satellite’s orbit provided measurements all over the globe and allowed us to study events associated with thunderstorms (lightning, TLEs) and unusual UV flashes (UV TAEs) far from thunderstorm regions. More than 8500 UV TAEs were measured by the Vernov satellite over the globe. Forty seven far-from-thunderstorm TAEs were selected having no lightning discharges during 1 h in a radius of 1000 km around the location of the event according to the Worldwide Lightning Location Network (WWLLN) and Vaisala Global Lightning Data Set (GLD360) data. Special attention was given to six events with complicated temporal structure and low luminosity in the IR channel. Their properties and atmospheric conditions were studied in detail. The analysis of cloud cover in addition to the lightning location networks data demonstrated the low probability of any lightning in the region of measurements.

[1]  U. Inan,et al.  Lightning-induced electron precipitation , 1984, Nature.

[2]  R. Nemzek,et al.  Observation and interpretation of fast sub‐visual light pulses from the night sky , 1989 .

[3]  M. Panasyuk,et al.  Vernov Satellite Data of Transient Atmospheric Events , 2017 .

[4]  D. Hampton,et al.  Blue Jets: their relationship to lightning and very large hailfall, and their physical mechanisms for their production , 1998 .

[5]  Y. C. Wang,et al.  Gigantic jets between a thundercloud and the ionosphere , 2003, Nature.

[6]  Umran S. Inan,et al.  Satellite observations of lightning‐induced electron precipitation , 1998 .

[7]  L. Tkachev,et al.  Preliminary results from the TUS ultra-high energy cosmic ray orbital telescope: Registration of low-energy particles passing through the photodetector , 2017 .

[8]  C. Rodger,et al.  Location accuracy of long distance VLF lightning locationnetwork , 2004 .

[9]  Yukihiro Takahashi,et al.  Elves : Lightning-induced transient luminous events in the lower ionosphere , 1996 .

[10]  Yoav Yair,et al.  Lightning Related Transient Luminous Events at High Altitude in the Earth’s Atmosphere: Phenomenology, Mechanisms and Effects , 2012 .

[11]  Y. Takahashi,et al.  ISUAL far‐ultraviolet events, elves, and lightning current , 2010 .

[12]  Richard E. Orville,et al.  Absolute Spectral Irradiance Measurements of Lightning from 375 to 880 nm , 1984 .

[13]  Umran S. Inan,et al.  Long‐range lightning geolocation using a VLF radio atmospheric waveform bank , 2010 .

[14]  R. Trapp Mesoscale Convective Systems , 2013 .

[15]  V. V. Klimenko,et al.  Global transients in ultraviolet and red-infrared ranges from data of Universitetsky-Tatiana-2 satellite , 2011 .

[16]  I. H. Park,et al.  The TUS Detector of Extreme Energy Cosmic Rays on Board the Lomonosov Satellite , 2017, Space Science Reviews.

[17]  Yukihiro Takahashi,et al.  Radiative emission and energy deposition in transient luminous events , 2008 .

[18]  H. Ögelman Millisecond time scale atmospheric light pulses associated with solar and magnetospheric activity , 1973 .

[19]  Y. Takahashi,et al.  On the Global Occurrence and Impacts of Transient Luminous Events (TLEs) , 2009 .

[20]  Umran S. Inan,et al.  Effects of thunderstorm‐driven runaway electrons in the conjugate hemisphere: Purple sprites, ionization enhancements, and gamma rays , 2001 .

[21]  O. Yaron,et al.  Space shuttle observation of an unusual transient atmospheric emission , 2005 .

[22]  Yukihiro Takahashi,et al.  Global distributions and occurrence rates of transient luminous events , 2008 .

[23]  T. E. Nelson,et al.  Submillisecond imaging of sprite development and structure , 2006 .

[24]  R. Marshall,et al.  Elve doublets and compact intracloud discharges , 2015 .

[25]  H. Salazar,et al.  Ultraviolet radiation detector of the MSU research educational microsatellite Universitetskii-Tat’yana , 2006 .

[26]  Yang Jing,et al.  Ground-Based Observations of Unusual Atmospheric Light Emissions , 2014 .

[27]  T. H. Allin,et al.  Optical observations geomagnetically conjugate to sprite-producing lightning discharges , 2005 .

[28]  Kristen L. Corbosiero,et al.  An evaluation of the Worldwide Lightning Location Network (WWLLN) using the National Lightning Detection Network (NLDN) as ground truth , 2010 .

[29]  V. N. Blinov,et al.  First results of investigating the space environment onboard the Universitetskii-Tatyana satellite , 2007 .

[30]  Yukihiro Takahashi,et al.  Electric fields and electron energies inferred from the ISUAL recorded sprites , 2005 .

[31]  M. Taylor,et al.  Statistical analysis of space-time relationships between sprites and lightning , 2003 .