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  • Two main kinds of thermal damp-out layers (TDL), occuring in Poland, have been investigated, namely: 1) the lower ones which begin directly above ground (irrespective of their depth)| 2) those elevated ones which are not higher than 1000m above
  • ground. Basing on radio soundings made at 11 and 23GMT, occurrence 1958-1967 of lower TDL (of radiation, radiation-advection, radiation-subsidence, advection and advection-subsidence type) has been examined as well as that of elevated TDL. For each kind