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   Chen, Yi-Hsiang; Brun, Todd A. (June 2019, Physical Review A)
2. Decomposing qubit positive-operator-valued measurements into continuous destructive weak measurements

   https://doi.org/10.1103/PhysRevA.98.062113  

   Chen, Yi-Hsiang; Brun, Todd A. (December 2018, Physical Review A)
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   https://doi.org/10.1016/j.nima.2023.168458  

   Seidl, R.; Vladimirov, A.; Adkins, J.K.; Akiba, Y.; Albataineh, A.; Amaryan, M.; Arsene, I.C.; Gayoso, C. Ayerbe; Bae, J.; Bai, X.; et al (October 2023, Nuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment)
4. Internet measurements on EdgeNet

   Vermeulen, Kevin; Ljuma, Burim; Formaux, Olivier; Friedman, Timur; McGeer, Rick (April 2019, CNERT: COMPUTER AND NETWORKING EXPERIMENTAL RESEARCH USING TESTBEDS)

   We describe the deployment of an Internet measurement experiment to three testbeds that offer Linux containers hosted at widely distributed vantage points: the well-established PlanetLab Central and PlanetLab Europe platforms, and the new EdgeNet platform. The experiment results were published in the proceedings of ACM IMC 2018. We compare the capabilities of each testbed and their effect on the ease of deployment of the experiment. Because the software for this experiment has several library dependencies and requires a recent compiler, it was easiest to deploy on EdgeNet, which is based on Docker and Kubernetes. This extended abstract is accompanied by a demonstration of the reproducible deployment of a measurement tool on EdgeNet. 

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5. A comparison of Jason-2 plasmasphere electron content measurements with ground-based measurements

   https://doi.org/10.5194/angeo-41-269-2023  

   Mazzella_Jr, Andrew J; Yizengaw, Endawoke (January 2023, Annales Geophysicae)

   Abstract. Previous studies utilizing the Global Positioning System(GPS) receivers aboard Jason satellites have performed measurements ofplasmasphere electron content (PEC) by determining the total electroncontent (TEC) above these satellites, which are at altitudes of about 1340 km. This study uses similar methods to determine PEC for the Jason-2receiver for 24 July 2011. These PEC values are compared to previousdeterminations of PEC from a chain of ground-based GPS receivers in Africausing the SCORPION method, with a nominal ionosphere–plasmasphere boundaryat 1000 km. The Jason-2 PECs with elevations greater than 60∘were converted to equivalent vertical PEC and compared to SCORPION verticalPEC determinations. In addition, slant (off-vertical) PECs from Jason-2were compared to a small set of nearly co-aligned ground-based slant PECs.The latter comparison avoids any conversion of Jason-2 slant PEC toequivalent vertical PEC, and it can be considered a more representativecomparison. The mean difference between the vertical PEC (ground-basedminus Jason-2 measurements) values is 0.82 ± 0.28 TEC units (1 TEC unit=1016 electrons m−2). Similarly, the mean differencebetween slant PEC values is 0.168 ± 0.924 TEC units. The Jason-2 slantPEC comparison method may provide a reliable determination for theplasmasphere baseline value for the ground-based receivers, especially ifthe ground stations are confined to only midlatitude or low-latituderegions, which can be affected by a non-negligible PEC baseline. 

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