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mean annual precipitation

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  • This site falls partly with the isimagaliso wetland park as well as within forestry areas on its boundary. SAEON is beuiling onf a >40 year ground water record and has added rain gauges to the site. It is a cimplimentory site to teh SAEON MCP site assessing the realtive impacts of land use land cover and climate on the ecosystem services in the area. Threats to Lake St Lucia Ramsar Site from proposed open cast mining operations in 1992 (CES, 1992) prompted a national and international outcry culminating in an international petition to “Save St Lucia” that led to its declaration as a World Heritage Site. This culminated in the proclamation and development of the iSimangaliso Wetland Park that protects the marine and coastal environments from Cape St Lucia to the Mozambique Border. The conservation policy in terms of the 1992 Conservation Development Plan was to protect a diversity of habitats such as coastal dune forests, coastal grasslands, hygrophilous grassland, coastal woodlands and shrublands. This vegetation mix would allow for the required habitat and feeding area for priority St Lucia animal species ...” (CES, 1992). Consequently, the St Lucia system, with its rich diversity of habitats, will be protected by national and international legislation for long-term global prosperity.

  • The Srebarna Lake was designated as a Monument of World Cultural and Natural Heritage (1983), UNESCO biosphere reserve (1977), Ramsar site (1975) and Important Bird Area (1990) because of its extremely rich ornithofauna and mainly because of the breeding of globally threatened species Dalmatian Pelican (Pelecanus crispus), Pygmy Cormorant (Phalacrocorax pygmeus) and Ferruginous Duck (Aythya nyroca). During the last years the lake ecosystem underwent significant changes towards strong eutrophication and anthropogenically speeded-up succession. The main reasons were the interrupted connection with the Danube River (because of a dyke built in 1948) together with the pumping-out of the underground waters, as well as the agricultural changes and activities in the watershed basin. The restoration activities carried out in 1993-1994 and especially the canal which connected the lake with the Danube lead to the beginning of lake recovery. All these events influenced the biodiversity of the reserve. The dominant plant association is that of the Reed (Phragmites australis), which occupies about two-thirds (400 ha) of the Reserve's total surface area. Gray Willow (Salix cinerea) and Purple Willow (Salix purpurea) bushes grow in some places. The second widest spread plant species after the Reed is the Lesser Reedmace (Typha angustifolia), and it is more abundant than the Great Reedmace (Typha latifolia). Of all 139 vascular plant species hosted by the Reserve, 11 are rare or endangered. Some 19 fish species occurred in the lake until 1948. There are 21 reptile and amphibian species, and 41 mammal species. The avifauna numbered a total of 230 bird species. The nesting colony of Dalmatian Pelican (Pelecanus crispus) is the pearl of the Reserve.

  • Harvard Forest is a core site in Domain 01: Northeast. Located 73 miles from Boston in Petersham, Massachusetts The Harvard Forest site is spread across 49 km2 of land and is the core NEON site for the Northeast region. Representative habitats at Harvard Forest include northern, transition, and central forests; marshes, swamps, and conifer-dominated bogs; and forest plantations. NEON's meteorological/flux tower and tower sampling plots are located on land owned by Harvard Forest - Harvard University, LTER an forest with a rich history of scientific research. The distributed sampling plots are located along the edge of the Quabbin reservoir which is managed by the Massachusetts Department of Conservation and Recreation, Division of Water Supply Protection. For access to the area along the Quabbin, visitors must be accompanied by a NEON project employee. Total data products collected at this site is 119.

  • The Hallstätter Glacier is the largest glacier in the northern Limestone Alps. The Hallstätter Glacier is oriented to the northeast and is bordered by Rock walls. The Large plateau above 2550 m.a.s.l. is connected by three short tongues. The largest altitude zone in terms of area is between 2550 m and 2600m. The highest point of the glacier is at 2905 m, the lowest point is on 2240 m. With an area of 2.623 km² (glacier boundary 2020), the glacier lost half of its extent compared to the glacier peak in 1856. In the past 10years, the area has increased by around 13 %.

  • Mt Halla San is in Jeju Island, the only volcanic subtropical island, in South Korea. Every year the island is hit by several typhoons. It has shaped unique environmental characteristics and biodiversity. In addition the mountain is one of the most popular vacation sites with growing ecological concern.

  • The meteorological sensors are located on the roof of the main building of the Biological Station (N 47,7691; E 16,7662; Position (elevation): 122 msl) in the close vicinity of Lake Neusiedl. The parameters that are on-line recoded every 15 minutes are as follows: Air humidity (%RH), Global radiation (W/m²), Air temperature (°C), Wind speed ([Average] (km/h), Wind direction (°), Rain yearly (mm), Precipitation (mm); time resolution: 15 minutes. There are also two traditional weather stations at the station and on the jetty, which are maintained by the Hydrolographic Service Burgenland and enable parameters such as temperature, humidity, precipitation and water level to be recorded. In addition to the Adcon weather station on the roof of the station, there are currently 3 other stations in operation in Seewinkel. These positions are: • Unterer Stinkersee (N 47,8018; E 16,7842) • Neudegg (N 47,7029; E 16,8098) • Östliche Fuchslochlacke (N 47,7907; E 16,8624)

  • The Venedigerkees in the Hohe Tauern National Park is the easternmost tributary glacier to the former tongue of Obersulzbachkees. As a result of the strong retreat of Obersulzbachkees, the glacier disintegrated into several tributary glaciers, with a large lake remaining at the location of a famous serac zone, the 'Türkische Zeltstadt'. Mass balance of the Venedigerkees is measured since 2011/12 with the direct or glaciological method. Furthermore, an automatic weather station was built between Venedigerkees and Keeskogel in 2018.

  • The Mullwitzkees is located in the Venediger Group in the core zone of the National Park Hohe Tauern. The upper part of the glacier (outer Mullwitzkees) is oriented to the south.The lower part of the glacier, especially the tongue, is oriented to West-South-West.

  • The Třeboň Wet Meadows is an LTER site of a 1 hectare area. It is a part of a wetland with the total area of 450 hectares situated in the inundation area of a large human-made reservoir (Rožmberk fishpond, 5 km2). The Wet Meadows are a predominantly herbaceous wetland with an up to several meters thick layer of organic sediment, which is superimposed on quaternary alluvial sands and clays. The vegetation cover is formed mainly by tall sedges (Carex acuta, C. vesicaria) and reed Canarygrass (Phalaris arundinacea). During the last 50 years, after cessation of mowing, a distinct stand structure of hummocks and hollows has developed. The hummocks are formed by tussocks of Carex acuta. On the site, wide water level fluctuations are recorded in some years. The relatively regular spring floods and irregular summer floods occur as a consequence of snow melting and summer rains in the catchment area, respectively. Extreme floods occurred in the summer of 2002 and both spring and summer of 2006, when the water level culminated at 2 m above the soil surface. The most frequently recorded position of the water level is at about −0.1 m. From 1977 to 2006, meteorological measurements were executed in a meteorological screen. Starting from 2006, the measurements have been executed with electronic sensors connected to data-loggers. Since that time, the site has been equipped for measuring carbon exchange and fluxes of CO2 and H2O (eddy covariance system, Licor). Since the spring of 2011, the site has been equipped for measuring methane and CO2 emissions from the sedges (automatic static flow chamber with a laser gas analyzer, LGR).The Wet Meadows are included in the integrated carbon observation system (ICOS) as a wetland ecosystem station.