Charakterystyka termiczna wklęsłej formy terenowej w okresie letnim 2010 r. na przykładzie zagłębienia międzywydmowego w Słowińskim Parku Narodowym

Abstract

The study is based on the measurements carried out on the Łeba Sandbar in the vicinity of the terrain station of the Department of Climatology, Adam Mickiewicz University in the period from 5 July 2010 to 6 August 2010. The interdune concave, close to the seashore, was chosen to recognize the microclimatic features of the hollow terrain form. Five measurement points were established within this hollow form: on the western, southern, eastern and northern slope and at the bottom of the concave. Thermal characteristic of each point was accomplished and thermal conditions within the hollow terrain form were described. At the same time, a description of weather conditions at standard surface has been performed, on the basis of the data from the automatic meteorological station located in the vicinity. The analysis has been made for the whole period and, separately, for the days with radiant weather.