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Lower River Clyde - United Kingdom
UK ECN site. The catchment area of the River Clyde is about 2000km2 and the river changes in character a great deal in its 121km journey to the tidal weir in Glasgow. In its... -
Ore estuary (Orefjarden), Umea Marine Sciences Centre (LTER) - Sweden
Umeå Marine Sciences Centre produces long term marine time series in the coastal and off-shore environments of the Gulf of Bothnia. The Ore estuary is proposed as the primary... -
Loch Leven - United Kingdom
UK ECN site. Loch Leven is the largest, shallow, relatively nutrient-rich, lowland loch (lake) in Scotland. It lies at an altitude of 107m. It has a surface area of 13.3km2 and... -
Oulanka Research Station (Oulanka LTER) - Finland
Oulanka Research Station is part of the Infrastructure Platform and is situated in Kuusamo as a regional unit of the University of Oulu. The station is located in the Oulanka... -
Krofdorf - Germany
Krofdorf Forest hydrological research area 4 catchments: A1 (9 ha), A2 (20 ha), B1 (11 ha), B2 (14 ha) -
LTER Observatory HAUSGARTEN - Germany
HAUSGARTEN comprises 21 permanent stations covering a depth range of 300 to 5.500 m water depth. Repeated water and sediment sampling and the deployment of moorings and... -
Scheldt Estuary and its alluvial plains - Belgium
The study site starts at the mouth of the river (Vlissingen, the Netherlands) and extends to Gent, 160 km from the mouth, where tidal influence is stopped by sluices. The... -
River Cree - United Kingdom
UK ECN site. The River Cree has a catchment area of 515.7km2, much of which is afforested, and a total river length of 57.5km. It has become one of the most acidic catchments in... -
Lago Maggiore - Italy
Lake Maggiore was studied since the beginning of last century although not systematically. Regular research started by the foundation in 1938 of the Italian Institute of... -
Gulf of Trieste - Slovenia
The separation line of the semi-enclosed northern basin from the rest of the Adriatic Sea is conventionally defined at the 100 m isobath, at about 43°20’N, from where the bottom... -
Curonian Spit National Park - Lithuania
Kuršių nerija, the Curonian Spit, is a narrow strip of sand stretching 98 kilometres along the Baltic Sea in western Lithuania. The Curonian Spit is a unique and vulnerable,... -
NINA Aquatic Research Station, Ims - Norway
NINA Aquatic Research Station, Ims provides advanced research facilities on aquatic research, primarily focused on fish ecology -
Rimov reservoir - Czechia
The Římov Reservoir was constructed in 1971–1978 at 21.85 km of the Malše River (tributary of the Vltava River), downstream its confluence with the Černá stream. The reservoir... -
Niwot Ridge - United States of America
The Niwot Ridge Long Term Ecological Research (LTER) site was established in 1980 with support from the National Science Foundation. The topography, climate and biota of the... -
OZCAR-RI ObsErA - Bras-David - Maison de la Forêt - Guadeloupe
The Bras-David river is located on Basse-Terre Island (Guadeloupe archipelago, lesser Antilles arc). This volcanic island results from the ongoing subduction of the Atlantic... -
Beagh's Burn - United Kingdom
UK Upland Waters Monitoring Network (UK UWMN) site. Beagh's Burn lies in the Glens of Antrim in north-eastern Northern Ireland. The catchment area is 302 ha and rises steeply... -
Piburger See - Austria
Piburger See is a small mountain lake in the Eastern Alps (Austria) and was part of the OECD study on eutrophication (OECD, 1980). This lake experienced cultural eutrophication... -
LTSER Zone Atelier Seine - Estuaire de la Seine - France
The Seine estuary is a megatidal estuary located in northern France. It is the third largest estuarine ecosystem in the country after the Gironde and Loire along the French... -
Ravels Forest - Belgium
This LTER-site corresponds with a 0.25 ha intensive forest monitoring plot (ICP Forests Level II) including a 0.25 ha buffer zone. The site is located in a homogeneous stand of... -
River Coquet - United Kingdom
UK ECN site. The River Coquet rises at Coquet Head on the Scottish border and flows generally eastward, draining the southern flanks of the Cheviot Hills, finally discharging...
