2013 №12 | Ukrainian Hydrometeorological Journal

Ukrainian Hydrometeorological Journal

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Title Page

Year: 2013

Issue: 12

Articles of this issue

Numerical prognosis of three-dimensional distribution of meteorological and turbulent variables
Renorm-group and fractal approach to turbulence spectrum in planetary atmosphere system, “cosmic plasma – galactic cosmic rays”
Integrated multi-scale models of interacting urban meteorology/climate and air quality: outcomes from Megapoli
Analysis of the conditions of low cloudiness over the Barents Sea
Estimation of influence of relief changeability on thermal balance of mountain slope
The evaluation of urban heat island characteristics over Odessa
Some aspects of research of features, changeability and extremality of the climate in the aspect of region (illustrated by research of certain characteristics of moistening for the Ural region)
To the problem of modelling of low-level jets
Airborne risk, regional vulnerability and possible accidental consequences from nuclear sites in the European Arctic and Sub-Arctic
Mezoscale changeability of ozone concentration in the surface layer in the Tomsk region (2010-2012)
Influence of macrocirculation processes on transfer of seawater aerosol in the internal areas of East Antarctica
The universal iterative method of clusterization data
Features teleсonneсtion surface temperature between tropical and high latitudes in the western sector of southern hemisphere
Autumn low jet over the Northwest Black Sea Coast
The research of heat waves of summer period, which observed in Kiev during 1911–2010
Estimation of statistical characteristics of the wind regime in the station Yuzhny-port and Ilyichevsk-port
Major trends in agro-climatic conditions of winter wheat growing in the Ukrainian part of the sub-basin of the Danube Delta
Agro-climatic conditions for growing spring barley in the Ukrainian part of the sub-basin of the Danube Delta in a changing climate
Metodological approaches for differently scaled agroclimatic zoning of territories
About relationship between circulation intensity in the Black sea and the wind field vorticity