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CHRONOMETRIC ANALYSIS OF HEALTH CONDITION OF SYKTYVKAR POPULATION IN CONNECTION WITH "SUMMER" AND "WINTER" TIME time change demonstrate the negative influence of this state measure. More pronounced this influence

Late Quaternary vegetation and lake system dynamics in north-eastern Siberia: Implications for seasonal climate variability the mid to late Holocene as well as lacking differentiation between summer and winter trends

Late Quaternary vegetation and lake system dynamics in north-eastern Siberia: Implications for seasonal climate variability the mid to late Holocene as well as lacking differentiation between summer and winter trends

About effect of weeds on spectral reflectance properties of winter wheat canopy was estimated. It has been found that despite the rather high weedness of winter wheat canopy in the spring-summer

Microbial metabolic response to winter warming stabilizes soil carbon changes in winter than summer in the Northern Hemisphere at high latitudes. Moderate increases in soil

Microbial metabolic response to winter warming stabilizes soil carbon changes in winter than summer in the Northern Hemisphere at high latitudes. Moderate increases in soil

The spectra of long-period variations in the semidiurnal tide and predominant wind at altitudes of the upper mesosphere and lower thermosphere in altitude are ~90 m2 s~2 in winter and 55-60 m2 s-2 in summer. The correlation between the semidiurnal tide

The spectra of long-period variations in the semidiurnal tide and predominant wind at altitudes of the upper mesosphere and lower thermosphere in altitude are ~90 m2 s~2 in winter and 55-60 m2 s-2 in summer. The correlation between the semidiurnal tide

POSSIBILITIES OF THE WINTER EDUCATIONAL SCHOOL IN THE DEVELOPMENT OF SELF-DETERMINATION OF THE PROFESSIONAL ACTIVITY OF CITIZENS AND TO INCREASE INTEREST IN SCIENTIFIC ACTIVITY FOREIGN STUDENTSPOSSIBILITIES OF THE WINTER EDUCATIONAL SCHOOL IN THE DEVELOPMENT OF SELF

Wind regime at 80-110 km at mid-latitudes of the northern hemisphere). The mean prevailing zonal winds at both locations are dominated by eastward/westward circulations in winter/summer

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