DOI,IST REx ID,Research Group,Title of publication
10.1126/sciadv.abc8895,8986,JiFr,Functional innovations of PIN auxin transporters mark crucial evolutionary transitions during rise of flowering plants
10.1007/978-3-030-65277-7_1,8987,KrPi,Delayed authentication: Preventing replay and relay attacks in private contact tracing
10.1073/pnas.2006731117,9000,GaTk,Nonequilibrium models of optimal enhancer function
10.1109/RadarConf2043947.2020.9266397,9001,JoFi,Microwave quantum illumination with a digital phase-conjugated receiver
10.4171/CMH/499,9007,TiBr,Free rational points on smooth hypersurfaces
10.14778/3436905.3436917,9011,ElKo,CALYPSO: Private data management for decentralized ledgers
10.1137/20M1322182,9039,JuFi,Convergence rates of the Allen-Cahn equation to mean curvature flow: A short proof based on relative entropies
10.34727/2020/isbn.978-3-85448-042-6_21,9040,ToHe,Formal methods with a touch of magic
10.1039/c9sm01850f,9054,,Rapid characterization of neutral polymer brush with a conventional zetameter and a variable pinch of salt
10.1038/s41586-020-2205-0,9059,,Ionic solids from common colloids
10.1039/d0ra05394e,9067,,Size-dependent magnetic and magnetothermal properties of gadolinium silicide nanoparticles
10.1088/2053-1591/ab6886,9069,,Synthesis of ternary electrocatalysts for exploration of methanol electro-oxidation in alkaline media
10.1007/978-3-319-90306-4_94-1,9096,SyCr,Parasites and Pathogens
10.1109/CDC42340.2020.9304042,9103,ToHe,Lagrangian reachtubes: The next generation
10.1007/s11854-020-0135-2,9104,LaEr,On the support of the free additive convolution
10.1103/prxquantum.1.020315,9114,JoFi,Bidirectional electro-optic wavelength conversion in the quantum ground state
10.1002/9780470015902.a0029007,9123,NiBa,Inversions and Evolution
10.5194/essd-2020-269,9124,,Atmospheric radiative profiles during EUREC4A
10.1029/2020ms002164,9125,,"Self‐aggregation of convective clouds with interactive sea surface temperature"
10.1029/2020ms002106,9126,,"What controls the water vapor isotopic composition near the surface of tropical oceans? Results from an analytical model constrained by large‐eddy simulations"