wfs_povpt
eng
utf8
National Meteorological Service of Slovenia at the Environmental Agency of RS (EARS)
2008-09-02
SIST EN ISO 19115:2005, Geographic information- Metadata.
ARSO- 2006
gauss-krueger_SLO(EPSG:16265)
Mean annual air temperature in Slovenia for 1971-2000 time period
2008-09-02
The temperature in Slovenia is characterized by daily and annual movment. The maximum daily temperature reaches the value of early afternoon, usually between 14 and 15 hour, the minimum value, just before sunrise. Most often, the warmest month in July, the lowest temperature is usually recorded in January with the exception of highlands, where the minimum temperature reached in February. The temperature in general with decreasing altitude, on average, the average annual air temperature for every 1000 m reduced by 5.3 ° C. In addition to altitude, the temperature effect in relief and micro-channels, the impact of large water surfaces and the impact of population. The impact of micro-is most pronounced at a minimum, indirectly, the average air temperature. On clear and calm nights in the basins and valleys common occurrence emergence of so-called cold air lake. The occurrence of temperature inversion is particularly noticeable in winter, often happens also that the cold air lake in the basin also persist for several days and thus also affect the average and maximum air temperature. In the warm half of the impact basin location less pronounced. Major impact on the water surface air temperature in Slovenia is limited primarily to the impact of the sea. The impact of the sea covered the whole Primorsko and extending over the valley of Trenta Soca all. Autumn and winter temperatures there are therefore higher than in places with a similar position in the interior of Slovenia. In the spring and the impact of sea warming slows somewhat, which is particularly evident at the highest daily temperaturah.Na air temperature also affects population density. On average air temperature in cities because of higher density heat sources (the firebox, transport, industry ...) and other physical properties of asphalt and concrete surfaces (lower albedo, higher heat capacity) is slightly higher than in the surrounding area. The bigger the city, the more apparent this effect. Maps of spatial distribution of values of variables related to air temperature are made based on measurements climatological meteorological stations that are during the period worked continuously for at least ten years. In calculating the values of variables related to air temperature in the correct grid with a resolution of 100 mx 100 m was used optimal spatial interpolation method, which takes into account the variable links with the altitude and the surrounding areas through selected also takes into account the impact of micro-. Because low-density network of observations, it is possible to consider the impact of micro-little.
Map is showing the temperature characteristics of the climate of Slovenia.
Mojca Dolinar
National Meteorological Service of Slovenia at the Enviromental Agency of RS
originator
Meteorological geographical features
theme
INSPIRE_SpatialThemes
2008-12-03
publication
Water.Drought prediction
water
Water
droughtPrediction
Drought prediction
theme
SBA_EuroGEOSS
2009-11-01
publication
otherRestrictions
otherRestrictions
Access constraints: the data are public avaliable.Data are avalible trough WFS service. Use constraints: compulsory indication of the source.(EARS)
Cartographic Numeric Base 1:1000 000
vector
1000000
slv
utf8
climatologyMeteorologyAtmosphere
0
2864
1971-01-01
2000-12-31
13.362634
16.613778
45.411504
46.883978
shp. or gml (version gml2)
http://gis.arso.gov.si/wfs?STORE=ARSOGIS or http://gis.arso.gov.si/arsogrs/arso_wfsclientui.jsp.
Metadata were produced from map.
2009-12-19T00:00:00
ULBF