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Gerd Baumgarten

Publications and source records attributed to Gerd Baumgarten.

3 recordsLinked to original sources

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

Trajectory and orbit of the unique carbonaceous meteorite Flensburg

The C1-ungrouped carbonaceous chondrite Flensburg fell in Germany on September 12, 2019, in the daytime. We determined the atmospheric trajectory, velocity, and heliocentric orbit using one dedicated AllSky6 meteor camera and three casual video records of the bolide. It was found that the meteorite originated in the vicinity of the 5:2 resonance with Jupiter at heliocentric distance of 2.82 AU. When combined with the bolide energy reported by the U.S. Government sensors (USGS), the pre-atmospheric diameter of the meteoroid was estimated to 2 - 3 meters and the mass to 10,000 - 20,000 kg. The meteoroid fragmented heavily in the atmosphere at heights of 46 - 37 km, under dynamic pressures of 0.7 - 2 MPa. The recovery of just one meteorite suggests that only a very small part of the original mass reached the ground. The bolide velocity vector was compared with that reported by the USGS. There is good agreement in the radiant but the velocity value has been underestimated by the USGS by almost 1 km/s.

astro-ph.EP

Seasonal Cycle of Gravity Wave Potential Energy Density from Lidar and Satellite Observations at $54^{\circ}$N and $69^{\circ}$N

We present the first seasonal cycle of gravity wave potential energy densities from ground-based lidar at high northern latitudes (Andenes/Norway, $69^{\circ}$N, $16^{\circ}$E) and compare with similar observations performed at middle latitudes (Kühlungsborn/Germany, $54^{\circ}$N, $12^{\circ}$E). Potential energy densities are derived from lidar temperature profiles observed with high vertical and temporal resolution at these sites. Both lidars have the unique capability of measuring during day and night, covering an altitude range from 30 to about 80 km. For the years 2012-2016 a total of $\sim$ 3000 and $\sim$ 6000 hours of observations were available at Andenes and Kühlungsborn, respectively. This data set was used to determine the seasonal variation of mean gravity wave potential energy densities, $E_{pot}$. We have applied wavelength and frequency filtering separately to account for potential influence of large scale waves such as tides. Despite the fact that both locations are rather different in terms of latitude, topography, and mean background conditions, the $E_{pot}$ values at both stations are rather similar, i.e. the monthly means deviate by less than a factor of 2. The mean potential energy densities show a clear seasonal variation at both locations with minimum (maximum) values in summer (winter). However, the winter/summer difference is only a factor of $\sim$ 3. We have compared these lidar results with observations from the SABER (Sounding of the Atmosphere using Broadband Emission Radiometry) satellite instrument and find satisfying agreement considering the differences in observational setup.

physics.ao-ph