Sentence examples for maximum snow cover from inspiring English sources

It can be observed that maximum snow cover area is found either in the month of January or in the month of April.

The maximum snow cover area has been observed in 2012 for the month of January with a value of 138,555 km2 and the minimum has been observed in 2007 for the month of July with a value of 7881 km2.

In the summer, the weather is mild and dry, but in the winter is cold and the powerful influence of the Aleutian Low allows for enormous snowfalls averaging 488 inches per year and maximum snow cover averaging 139 inches.

This database provides the information on air temperature (°C; daily mean, maximum and minimum), annual precipitation (mm), radiation (h), sunshine (MJ/m) and maximum snow cover (cm) at a 1-km scale, and is thus suitable for our sampling scale.

The simulated spatial distribution of snow cover was evaluated using the Moderate Resolution Imaging Spectroradiometer (MODIS) 8-day maximum snow-cover extent (MOD10A2) product, which revealed the model's capability for capturing the spatiotemporal variations in snow cover within the study area.

For the month of April, minimum snow cover was observed in the year 2004 (56,236 km2) and maximum was observed in the year 2002 (114,588 km2).

The minimum snow cover during this period was in the year 2008 with a value of 29,822 km2 and the maximum was in the year 2012 with a value of 138,555 km2.

We detected TBEV RNA in brain and other tissues from rodents in some of the northernmost TBEV-endemic areas in Europe, where the daily maximum temperatures and the snow cover in winter do not enable nymphal or larval activity.

Daily or 10-day-mean (dekadal) records of minimum and maximum air temperature, precipitation (mm) and snow cover (cm) recorded at 6 8 ground stations per country were acquired from national Meteorological Agencies (see map).

Figure 1 displays a map of months showing seasonal river runoff maxima in coastal regions, climatological areas of snow cover, and central lines of intertropical convergence zones (ITCZs).

Microthermal regimes, which are influenced by snow cover, include winter minima and summer maxima resulting from snowmelt and convectional rain; alternatively, spring meltwater maxima are accompanied by secondary fall maxima that are associated with late-season thunder rain, or spring snowmelt maxima can be followed by a summer glacier-melt maximum, as on the Amu Darya.