Weather on Drenas

On January 31st, 2013 by Admin | No Comments | Posted in Weather on Kosovo

Gllogoc (Kosovo)
Today
Sunny
Wind : 1 km/h
Humidity : 100%
8°C
  • Wednesday 6 - 18 °C
  • Thursday 6 - 15 °C
Weather Layer by www.BlogoVoyage.fr

Surface temperature differences in turn cause pressure differences. A hot surface heats the air above it and the air expands, lowering the air pressure and its density.[14] The resulting horizontal pressure gradient accelerates the air from high to low pressure, creating wind, and Earth’s rotation then causes curvature of the flow via the Coriolis effect.[15] The simple systems thus formed can then display emergent behaviour to produce more complex systems and thus other weather phenomena. Large scale examples include the Hadley cell while a smaller scale example would be coastal breezes.

Weather on Ferizaj

On January 31st, 2013 by Admin | No Comments | Posted in Weather on Kosovo

Ferizaj (Kosovo)
Today
Partly sunny
Wind : 6 km/h
Humidity : 85%
9°C
  • Wednesday 8 - 19 °C
  • Thursday 7 - 16 °C
Weather Layer by www.BlogoVoyage.fr

The uneven solar heating (the formation of zones of temperature and moisture gradients, or frontogenesis) can also be due to the weather itself in the form of cloudiness and precipitation.[11] Higher altitudes are cooler than lower altitudes, which is explained by the lapse rate.[12][13] On local scales, temperature differences can occur because different surfaces (such as oceans, forests, ice sheets, or man-made objects) have differing physical characteristics such as reflectivity, roughness, or moisture content.

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