EVALUATION OF LONG-TERM AIR AND SOIL TEMPERATURE CHANGES ON THE FAR NORTH-EAST OF RUSSIA
The temperature regime is investigated according to observations of temperature data of soil and air in the meteorological stations of the Far Northeast of Russia in the period 1966-2014 years: distribution characteristics are calculated, extreme and significant areal temperature anomaly (by the N. A. Bagrov) in the central months of the season are identified and studied. Repeatability of extremely abnormal temperature fields is highest in the spring, about 80% of the cases occurred in the 80s of the last century. Zoning with similar dynamics of air temperature is produced according the correlation between the temperature series: 4 areas in the winter and 3 in the summer are received. A steady increase in air temperature, especially in the transitional seasons is revealed. It is not so much in summer and observed on the background of increasing of areal air temperature abnormality. The winter season is characterized by cooling, which is well expressed in January. At the same time in January a reduction of significant areal air temperature anomalies is observed. The average territorial air temperature steadily increased in all months except January, the highest rate of temperature rise is observed in March - April and October - December. It is found that the soil temperature is also increase and besides in all seasons. The correlation relationship between the soil and the air temperature is investigated.