The main aim of the article is to fill the gap concerning the recognition of constructs of programme management supporting open innovations. Current knowledge on this subject is mainly limited to identifying success factors of open innovation and programme management. In the current literature, there are few publications indicating the use of the programme as a tool supporting innovation. In order to fill the identified knowledge gap, common factors of programme success and open innovations were compared and assessed successively. A quantitative study was conducted on an international group of experts, including 578 experts in programme management. As a result of applying cluster analysis and operationalising the obtained results, four programme constructs supporting open innovations were dimensioned, such as cooperation with the environment, transfer of knowledge and technology, organisational maturity, and ensuring and maintaining implementation capacity. Moreover, the discussion and the research revealed that the impact and scope of the structured approach to programme management not only allow for the implementation of the assumed outcomes and benefits at the strategic level, but also influence the shaping and adjustment of the whole organisation.

The ArcLight observatory provides hourly continuous time series of light regime data (intensity, spectral composition, and photoperiod) from the Arctic, Svalbard at 79° N. Until now, no complete annual time series of biologically relevant light has been provided from the high Arctic due to insufficient sensitivity of commercial light sensors during the Polar Night. We describe a camera system providing all-sky images and the corresponding integrated spectral irradiance ( E P A R ) in energy or quanta units, throughout a complete annual cycle. We present hourly–diel–annual dynamics from 2017 to 2020 of irradiance and its relation to weather conditions, sun and moon trajectories.

The light climate in the Arctic is primarily controlled by seasonal changes in solar elevation. The region experiences extended periods of 24-hr daylight (Polar Day) and 24-hr darkness (Polar Night), resulting in extreme variations in both the magnitude and spectral composition of irradiance entering the ocean throughout the year. Whilst the sun remains below the horizon during the Polar Night, solar elevation still significantly controls spectral irradiance during much of this period through atmospheric scattering of light from the sun. However, throughout the darkest periods of the winter season, irradiance from the moon becomes the dominant source of illumination (Johnsen, Zolich, et al., 2021).