ANALYSIS OF THE SPATIAL AND TEMPORAL CONNECTIONS OF SURFACE PRESSURE FIELD WITH THE UPPER LAYERS OF THE ATMOSPHERE
The article is devoted to analysis of the connections of pair correlation coefficients between the actual values of the geopotential on standard isobaric surfaces: 1000, 850, 700, 500, 300, 200 and 100 hPa in the grid with a step10°, at latitudes 40, 50, 60, 70 and 80° n.l. In each latitudinal zone special features have been revealed, as well as their importance for the restoration of the fields of higher levels and for the development and adjustment of long-term weather forecasts.