key part of mission planning is the estimation of the radiation environment likely to be encountered by the spacecraft. This commonly consists of the solar proton fluence, cosmic rays, and any trapped particle environments likely to be encountered. Almost invariably overlooked are electrons in interplanetary space from solar particle events and other sources. This can be attributed to the relative Total Ionising Dose (TID) and Single Event Effect (SEE) damage that may be incurred by energetic protons over electrons [1]. However, in certain scenarios the dose deposited in lightly shielded regions of a spacecraft by electrons, as well as the potential for charging can be significant, particularly in the use of cryogenics, where lower temperatures can reduce the conductivity of common space polymers. In addition, the use of highly sensitive detectors in interplanetary space (e.g: Herschal, Planck at L2) requires a good understanding of all possible sources of noise and contamination. An extensive collection of electron flux data exists, dating back to the early 1970s. These data have been used for scientific studies of the environment, but has rarely been used to form an engineering model with predictive capabilities. Giuseppe Vacanti is with cosine Science and Computing BV, Niels Bohrweg 11, 2333 CA Leiden, The Netherlands (e-mail: gvacanti@cosine.nl).Dr. Erik Maddox is with cosine Science and Computing BV, Niels Bohrweg 11, 2333 CA Leiden, The Netherlands (e-mail: emaddox@cosine.nl).Dr. Craig Underwood is with the Surrey Space Centre, University of Surrey, Guildford, UK (e-mail: c.underwood@surrey.ac.uk) CMEs. Secondary sources include Jovian and galactic electrons, with solar wind electrons typically falling below the 200keV lower limit for the model.