Место издания:The University of Auckland Auckland, New Zealand
Первая страница:138
Последняя страница:141
Аннотация:The complex scientific experiment was carried out in Dolgoprudnyi near Moscow since August till October of 1998. Thermal stratification type and margins of inversions were registered simultaneously by means of routine radiosondes, microwave radiometer and vertical sodar. Results were compared with account of temporal and spatial resolution differences between all three methods. Two criteria were used for inversion identification on profiles. It was noted that coincidence of stratification type data, received by various methods, is a good usually, as a contrast to estimations of inversion top heights. The connection between types of structures on sodar records and values of a temperature gradient was founded.