WORLD METEOROLOGICAL ORGANIZATION |
UNITED NATIONS ENVIRONMENT PROGRAMME |
The DMI is engaged in the following research and monitoring projects, relevant to stratospheric ozone depletion:
-"Stratospheric climatology using UV/Visible spectroscopy". The DMI carries out UV/Visible measurements of O3, NO2, and possibly OCIO and BrO at Thule.
-"Ozone soundings as a tool for detecting ozone change". The DMI carries out ozone soundings from Thule and Scoresbysund (70 °N, 22 °W) .
-"Ultraviolet radiation in the arctic: past, present and future". The DMI measures UV radiation at Thule with a spectroradiometer.
-"Ozone as a climate gas". The DMI performs ozone soundings from Scoresbysund, investigates trends and carries out GCM-modelling with the purpose of detecting climate changes.
-"Gravity waves in the stratosphere". The DMI makes observations of 3-D winds with a radar at Sondre Stromfjord (67 °N, 51 °W) with the purpose of investigating gravity waves which may produce polar stratospheric clouds. The PSCs are observed by lidar and backscatter sondes. The experimental observations are compared with modelling of the waves.
-Observations of O3 and UV-B radiation are made with Brewer spectrometers at Copenhagen (56 °N, 12 °E) and Søndre Strømfjord.
-Based on meteorological analysis from ECMWF, the DMI performs trajectory model calculations of transport of ozone and other trace gases.
University of Copenhagen
-"Laboratory studies and modelling of heterogeneous chemistry in the stratosphere" are made by the Institute of Chemistry, Chemical Laboratory V. Results from this combined laboratory and modelling study will provide detailed information on the impact of heterogeneous chemical reactions on the stratospheric ozone depletion. The study addresses reactions relevant to both the middle and high latitudes. The objective is to obtain new information on the heterogeneous chemical processes taking place on the stratospheric sulphuric acid aerosol and which influence the partitioning of hydrogen, halogen and nitrogen species in the lower stratosphere over middle to high latitudes.
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