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M5_10min
"M5 is located in a wet fen area called 'Rylekæret', just 20 meters North of the Automatic Chamber site. The station was installed in 2009. In this file soil temperatures in 2,... -
M4_360min
"M4 is located on a well drained Cassiope heath, about 150 meters north of the 'Climate station' (operated by ClimateBasis). The station was installed in 2005. Soil moisture is... -
M3
M3 is one of six meteorological stations in the Zackenberg and Store Sødal Valley. Data from the station is found under meteorology (wind, temperature and relative humidity,... -
M2
M2 is one of six meteorological stations in the Zackenberg and Store Sødal Valley. Data from the station is found under meteorology (wind, temperature and relative humidity,... -
Zackenberg_River_Suspended_sediment
Water samples from the Zackenberg River is collected near the Hydrometric station at 08:00 and 20:00 o'clock every day in the period 1997-2011 and three times a week from... -
V1_Water_temperature_0m
Water temperature is measured on the bottom of the Zackenberg river, just west of the Zackenberg research station. The measurements were started in 1995. Initially the... -
River_water_chemistry
"Measurements started in 1997 and are still on going. From 1997-2011 water samples were taken everyday at 8 am and 8 pm. From 2012-present water samples are taken three times a... -
MM2_Water_level_automatic
Water level is monitored automatically at the fluxstation site 'MM2' in the continous fen 'Rylekæret'. Automatic measurements of the water level are recorded every 15th minute... -
Lindeman_Temperature
"From 2005 - 2010 discharge, conductivity and water temperature was monitored in the river Lindemans elven, the largest tributary to the Zackenberg river after Store Sødal (see... -
Lindeman_Discharge
"From 2005 - 2010 discharge, conductivity and water temperature was monitored in the river Lindemans elven, the largest tributary to the Zackenberg river after Store Sødal (see... -
Lindeman_Conductivity
"From 2005 - 2010 discharge, conductivity and water temperature was monitored in the river Lindemans elven, the largest tributary to the Zackenberg river after Store Sødal (see... -
AC_Water_level_manual
Water level is read both manually and automatically at the Automatic chamber site in the 'Rylekæret' fen. The measurements reported here are the manual measurements, that are... -
AC_Water_level_automatic
Water level is monitored automatically at the Automatic Chamber site in the 'Rylekæret' fen (see GeoBasis Zackenberg manual). Automatic measurements of the water level are... -
Recession
Coastal cliff recession has been monitored along four markers on the Southern coast towards Young Sound since 1996. Until 2011 the perpendicular distance between the four... -
Coastal_profile P2
The Coastal dynamics, sediment transport, are monitored in two detailed terrain profiles. Profile 2 is a c.140 m long profile in an aggrading coastal plain with beach ridges... -
Coastal_profile P1
The Coastal dynamics, sediment transport, are monitored in two detailed terrain profiles. Profile 1 is a c. 250 m long profile line crossing a curved spit near the old delta... -
MM2
Eddy covariance flux measurements has taken place at the site MM2 since 2007. The mast (3 m high) is located on a wet fen area called Rylekæret, about 1.5 km North of the... -
MM1
Micrometeorological monitoring has taken place at the site MM1 since 2000. In 2011 an energy balance mast was put up about five meters East of the existing eddy covariance mast.... -
AC
Automated chamber flux monitoring is conducted in the wet fen Rylekæret in the Zackenberg valley since 2006. An overview of the site and where the chambers are situated in... -
Zackenberg Valley
Zackenberg Valley
