is explained with weather data of each respective year. Due to its concave form, winter snow didn’t melt until the late summer in the past few years. With such weather conditions and further increase in winter precipitation, the Triglav glacier will continue
The study is concerned with the temporal and spatial characterisation of atmospheric thaw variability in Poland. The phenomenon was described on the basis of mean daily values of air temperature for the winter months October-March over the period
are a constant element of the climate in Poland and occur with a frequency of 30-45% of the calendar winter (December-February) and 30% to almost 50% of the period of the thermic winter. Thaws are most common in the western part of Poland, particularly
Altitude ; China ; Climate extreme ; Drought ; Monsoon ; Mountain ; Southwest China ; Space time ; Summer ; Winter
to the data, the temporal and spatial characteristics of the extreme drought frequency in inter-annual, inter-decadal, summer monsoon period and winter monsoon period are analyzed. In general, it is shown that the southwestern Sichuan Basin, southern Hengduan
This article examines crop water productivity (CWP) of winter wheat and summer maize from 2003 to 2007 in the Haihe River Basin based on large-scale evapotranspiration (ET) and crop yield obtained by remote sensing technology. Results show both
variations in CWP of winter wheat and summer maize in most parts of the study area. They also show certain promotion potential to alleviate the water shortage. Correlation analysis of CWP, crop yield and ET shows that there is great potential for crop yield
. The orchard soils (0 to 15 and 15 to 30 cm depths) of summit, shoulder and backslope hill slopes were analysed during post-monsoon (October–November) at fruit ripening and post-winter (March–April) at flower initiation. Principal component analysis revealed
that hill slope position and soil moisture had significant influence on variability of soil biological pools. Sizes of biological pools were significantly higher in post-monsoon than post-winter. It is highlighted that hill slope position and soil moisture
the discovery of a Northeast Passage to the Far East. However, while caught in the grip of the ice for some two years, the expedition unexpectedly came upon Franz Josef Land, spending seven months of winter 1873–1874 there. Unsurprisingly, the expedition’s
Synoptic conditions of heavy snowfalls at 4 stations in Europe (Oslo, Bremen, Smolensk and Budapest) were analyzed using daily data of snow cover depth from 50 winter seasons (1960/1961-2009/2010). Composite maps of the sea level pressure and 500
Annual and seasonal quantities аnd trends of precipitation from 1949 to 2010 were analyzed for twelve stations in Serbia. The precipitation trends during winter and spring had decreased, while in summer and autumn increased. Tendencies of annual
This article examines the impact of climate changes on the development of tourism in the Alps. Based on activity in test areas, general adaptation strategies were designed with regard to the seasonal character of tourism centers: summer, winter
prospective increase of Fall and Winter stream flows as due to increased liquid precipitation. Lower discharges are projected during Spring and Summer, in view of decreased rainfall and snow cover at thaw, and the CCSM3 model provides shifting of thaw season
to one month earlier. Higher catchments are more impacted because Winter flows increase more proportionally.
in 3 seasons (spring–summer–winter) throughout the year in 1979–1980 and 1999–2000, with additional measurements in 1985. Electrical conductivity of saturation extracts (ECe) and the concentrations of major ions were measured in 400 soil samples for 5
to be maintained by a standing man hiking in the Łysogóry Range on a frosty and windy winter day. Summer sports clothing (Iclp = 1.00-1.50 clo) seems to offer sufficient protection for a standing man at the foot or on the slopes of the Łysogóry Range during a warm
environmental regimes. Significant variations were observed in the onset of branching across the populations by both age and height, likely related to the interplay between summer precipitation (and thus growth rate) and winter precipitation, which increases
by elevation, the AA. identified 3 distinct snow zones in the basin : persistent, transitional, and intermittent. The transitional snow zone represents an area that is sensitive to losing winter snowpack.