A. Stohl1, P. Seibert2, G. Wotawa3, D. Arnold2,4, J. F. Burkhart1, S. Eckhardt1, C. Tapia5, A. Vargas4, and T. J. Yasunari61NILU – Norwegian Institute for Air Research, Kjeller, Norway2Institute of Meteorology, University of Natural Resources and Life Sciences, Vienna, Austria3Central Institute for Meteorology and Geodynamics, Vienna, Austria4Institute of Energy Technologies (INTE), Technical University of Catalonia (UPC), Barcelona, Spain5Department of Physics and Nucelar Engineering (FEN),Technical University of Catalonia (UPC), Barcelona, Spain6Universities Space Research Association, Goddard Earth Sciences and Technology and Research, Columbia, MD 21044, USAAbstract. On 11 March 2011, an earthquake occurred about 130 km off the Pacific coast
of Japan's main island Honshu, followed by a large tsunami. The resulting
loss of electric power at the Fukushima Dai-ichi nuclear power plant (FD-NPP)
developed into a disaster causing massive release of radioactivity into the
atmosphere. In this study, we determine the emissions of two isotopes, the
noble gas xenon-133 (133Xe) and the aerosol-bound caesium-137
(137Cs), which have very different release characteristics as well as
behavior in the atmosphere. To determine radionuclide emissions as a function
of height and time until 20 April, we made a first guess of release rates
based on fuel inventories and documented accident events at the site.