Replication Data for: A technique for volumetric incoherent scatter radar analysisdoi:10.18710/ZM973LDataverseNO2022-10-251Stamm, Johann; Vierinen, Juha, 2022, "Replication Data for: A technique for volumetric incoherent scatter radar analysis", https://doi.org/10.18710/ZM973L, DataverseNO, V1Replication Data for: A technique for volumetric incoherent scatter radar analysisdoi:10.18710/ZM973LStamm, JohannVierinen, JuhaStamm, JohannVierinen, JuhaGustavsson, BjörnSpicher, AndresUiT The Arctic University of NorwayJuliaPythonRadar science with EISCAT3D326039DataverseNOUiT The Arctic University of NorwayStamm, JohannStamm, Johann2022-06-09Physicsneutral windelectric fieldincoherent scatter radarinverse problemsion momentum equationProgramming code and background files for article "A technique for volumetric incoherent scatter radar analysis". The code relates ion velocity to neutral velocity and electric field in the ionosphere. This is performed by solving the momentum equation in three dimensions and adding Mawells equations, continuity equation and other assumptions as constraints.Volumetric measurements of the ionosphere are important for investigating spatial variations of ionospheric features, like auroral arcs and energy deposition in the ionosphere. In addition, such measurements make it possible to distinguish between variations in space and time. While spatial variations in scalar quantities such as electron density or temperature have been investigated with ISR before, spatial variation in the ion velocity, which is a vector quantity, has been hard to measure. The upcoming EISCAT3D radar will be able to do volumetric measurements of ion velocity regularly for the first time. In this article, we present a technique for relating volumetric measurements of ion velocity to neutral wind and electric field. To regularize the estimates, we use Maxwell's equations and fluid-dynamic constraints. The study shows that accurate volumetric estimates of electric field can be achieved. Electric fields can be resolved at altitudes above 120 km which is the altitude range where auroral current closure occurs. Neutral wind can be resolved at altitudes below 120 km.Programming code and calculated examples<a href="http://creativecommons.org/publicdomain/zero/1.0">CC0 1.0</a>Submitted for reviewSubmitted for review00_readme.txttext/plainbasis.jlapplication/octet-streamionocalc.jlapplication/octet-streamkoordinaterhh.jlapplication/octet-streamkoordtrans.jlCoordinate transforms for ECEF, geodetic coordinates, the coordinate system used for the magnetic field and for transforms in general.application/octet-streamloaddata.jlFor loading IRI data or ISR dataapplication/octet-streampraktisk.jlapplication/octet-streamregul.jlapplication/octet-streamsim.jlapplication/octet-streamteom.jlapplication/octet-streamteom_test.jlapplication/octet-streamtest14-mT0-8.zipapplication/zip