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Toralf Renkwitz

Publications and source records attributed to Toralf Renkwitz.

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Optical and Radar Observations of the February 2025 Falcon 9 Upper-Stage Re-entry

We investigate the February 19, 2025, re-entry of a Falcon 9 upper stage using optical observations from 43 meteor cameras across central Europe together with radar detections of re-entry plasma obtained with the 32.55 MHz SIMONe Germany multistatic radar system. Optical observations of fragment emissions between 85 and 36 km altitude were used to reconstruct 30 fragment trajectories, identify two main fragment families, and fit ballistic trajectories to estimate kinetic energy loss per unit mass. The optical detection-height distribution peaks near 60 km with a standard deviation of 10 km, and both optical and radar signatures occur in the same broad altitude region as the maximum kinetic-energy loss. Radar echoes were detected at altitudes between 55 and 75 km, and the radar-derived positions are consistent with those obtained from optical observations. Two distinct radar echo types associated with the re-entry plasma were identified: (1) specular trail echoes from overdense wake plasma, with radar cross-sections (RCS) of up to 60 dBsm, and (2) short-lived non-specular trail echoes with RCS values of 20--30 dBsm, exhibiting a delay of 1--2 s compared to optical signatures. The characteristic decay time of both echo types is approximately 1 s. In the radar-echo altitude range, the estimated Knudsen numbers for meter-scale fragments are well below unity, consistent with continuum-flow conditions and shock-driven plasma production rather than ordinary meteor-like impact ionization. These serendipitous radar observations demonstrate that the atmospheric re-entry of other spacecraft, including objects smaller than the Falcon 9 upper stage such as Starlink satellites, may likewise be detectable using comparable multistatic meteor radar systems deployed globally.

physics.space-ph

LOFAR observations of asymmetric quasi-periodic scintillations in the mid-latitude ionosphere

The LOw Frequency ARray (LOFAR) was used to track the propagation of a TID containing embedded plasma structures which generated type 1 asymmetric quasi periodic scintillations (QPS: Maruyama, 1991) over a distance of >1200 km across Northern Europe. Broadband trans ionospheric radio scintillation observations of these phenomena are, to our knowledge, unreported in the literature as is the ability to track asymmetric QPS generating plasma structures over such a distance. Type 1 asymmetric QPS are characterised by an initial broadband signal fade and enhancement which is then followed by 'ringing pattern' interference fringes. These are caused by diffractive fringing as the radio signal transitions through regions of relatively steep plasma density gradient at the trailing edge of the plasma structures. That the QPS retained their characteristics consistently over the full observing window implies that the plasma structures generating them likewise held their form for several hours, and over the full 1200 km distance. The most likely TID propagation altitude of 110 km was consistent with a persistent and non blanketing sporadic E region detected by the Juliusruh ionosondes, and direct measurements from co-located medium frequency radar. Co-temporal GNSS data was used to establish that these plasma density variations were very small, with a maximum likely amplitude of no more than +/- 0.02 TECu deviation from the background average. The observations were made between 0430-0800 UT on 17 December 2018 under very quiet geophysical conditions which possibly indicated a terrestrial source. Given the TID propagation direction, the source was likely located at high-latitude.

physics.space-ph