Daily predictions based on meteorological forecast model - NetCDF

Daily standard meteorological data from Fülöpháza which are representative for the whole KISKUN LTER. The station is operated jointly by Centre for Ecological Research, Hungarian Academy of Sciences and Hungarian Meteorological Service. The measured data: air, ground, soil temperature, precipitation, air humidity, wind speed, soil moisture, atmospheric pressure and global radiation.

Monthly standard meteorological data from Fülöpháza which are representative for the whole KISKUN LTER. The station is operated jointly by Centre for Ecological Research, Hungarian Academy of Sciences and Hungarian Meteorological Service. The measured data: air, ground, soil temperature, precipitation, air humidity, wind speed, soil moisture, atmospheric pressure and global radiation.

Located 2 km east of the Science Campus of the University of Poitiers, the Hydrogeological Experimental Site (HES) occupies an area of 12 hectares on land belonging to the University. From the geologic viewpoint the SEH occupies the north flank of the “Seuil du Poitou”, a huge Mesozoic carbonate plateau marking the transition between the Aquitaine and Paris sedimentary basins. The studies conducted at the SEH focus mainly on the Dogger Aquifer. The experimental layout now comprises 35 boreholes, including two vertical and two inclined cored holes.

Monthly standard meteorological data from Fülöpháza which are representative for the whole KISKUN LTER. The station is operated jointly by Centre for Ecological Research, Hungarian Academy of Sciences and Hungarian Meteorological Service. The measured data: air, ground, soil temperature, precipitation, air humidity, wind speed, soil moisture, atmospheric pressure and global radiation.

Daily standard meteorological data from Fülöpháza which are representative for the whole KISKUN LTER. The station is operated jointly by Centre for Ecological Research, Hungarian Academy of Sciences and Hungarian Meteorological Service. The measured data: air, ground, soil temperature, precipitation, air humidity, wind speed, soil moisture, atmospheric pressure and global radiation.

The WegenerNet climate station network Feldbach region is a pioneering weather and climate observation experiment at very high resolution located in Eastern Styria near the city of Feldbach in Southeast Austria, a region characteristic for experiencing a rich variety of weather and climate patterns. The network comprises 156 meteorological stations measuring temperature, precipitation, and other parameters, in a tightly spaced grid within an area of 23 km x 18 km centered near the city of Feldbach (46.93°N, 15.90°E). With its stations every about two square-km (area of about 300 square-km in total), and each station with 5-min time sampling, the network provides regular measurements since January 2007. As of 2010 a complementary meteorological-hydrological network of several stations was added in the mountainous upper Styrian region of National Park Gesaeuse as contribution to the LTER site Johnsbachtal (the "sister site" LTER_EU_AT_029_001 of this site LTER_EU_AT_029_002, both affiliated with the LTSER Platform Eisenwurzen). As part of the Johnsbachtal site, the WegenerNet Johnsbachtal consists of fourteen mountain-proof stations within a region-scale of about 10 km, ranging from valley altitudes below 700 m to mountain tops higher than 2100 m. The WegenerNet at both sites together provides strong value for both alpine foreland and mountain region studies.

The research activities in the lagoon, as well as the understanding of natural phenomena, are directed to the study of the ecological effects of the major pressures acting on the system, including which the input of nutrients from agricultural and urban sources, industrial activity and port (Porto Marghera, Venice Maritime Station, the commercial port in Chioggia), the release of pollutants accumulated in sediments, the intense traffic ships and smaller boats,, the morphological trivialization. In recent decades the Tapes philippinarum has generated problems related to collection techniques. Is focusing attention to the increasing presence of alien species both plant that animals.

The Desert Ecology Plot Network is located in the Simpson Desert in central Australia. The vegetation in the study region is dominated by hard spinifex (Triodia basedowii E. Pritz), with scattered small woodlands of Georgina gidgee (Acacia georginae F.M. Bailey) interspersed throughout (Figure 9.1). The long-term plots for which data are provided as part of LTERN infrastructure are all located within the spinifex hummock grasslands, but additional survey plots, situated in gidgee woodlands, exist and have been surveyed since 2006 and are revisited whenever possible. Temporal visits are conducted annually. The Desert Ecology Plot Network was a member of Long Term Ecological Research Network (LTERN), Australia, a facility of the Australian Government's Terrestrial Ecosystem Research Network (TERN).

CARBON FLUXES IN TWO SUCCESSIONAL STAGES OF VEGETATION IN THE PODGORSKI KRAS. Research site represents karst grassland and different stages of secondary succession, occasionally affected from forest fires. It is located on karst plateau close to Podgorje village in the sub-mediterranean region of south-west Slovenia. The site is equipped with two Eddy Covariance towers which measure the carbon fluxes in two successional stages of vegetation. The area has undergone major human influences due to its position at the transition between the Mediterranean and central Europe. In fact, agricultural practices, such as overgrazing in the past centuries, led to pronounced destruction of the vegetation cover, causing severe soil erosion and resulting into a stony and bare landscape. However a succession is taking place and different vegetation types, ranging from grasslands to secondary oak forests, are now present. The bedrock is mainly composed of Paleocene and Eocene limestone. The chemical weathering known as karst phenomena led to the formation of Leptosols and Cambisols, which represent insoluble fractions of carbonates. As a result, the soil is superficial, with depths ranging from 0 cm to several decimeters in soil pockets between rocks. The organic matter represents about 12–15% of the topsoil. The climate is referred to as sub-mediterranean, with a mean annual temperature of 10.5 °C, a mean daily temperature of 1.8 °C and 19.9 °C in January and June respectively, and an average annual precipitation around 1370 mm. The growing season ranges from March or April to October.