Daily predictions based on meteorological forecast model - NetCDF

Air temperature at 2m measured in a raised bog ecosystem (treed bog community) by ROTRONIC HygroClip S3 (temperature logger), 2010-continues, 30 min frequency, several gaps in data, N60.89164 E68.67690, as part of meteorological monitoring in Mukhrino Field Station (https://mukhrinostation.com/).

Air temperature at 2m measured in a coniferous mixed forest ecosystem by DS18B20 (temperature logger), 2012-continues, 30 and 60 min frequency, several gaps in data, N60.89458 E68.70920, as part of meteorological monitoring in Mukhrino Field Station (https://mukhrinostation.com/).

Air temperature at 2m measured in a raised bog ecosystem (treed bog community) by ROTRONIC HygroClip S3 (temperature logger), 2010-continues, 30 min frequency, several gaps in data, N60.89164 E68.67690, as part of meteorological monitoring in Mukhrino Field Station (https://mukhrinostation.com/).

Air temperature at 2m measured in a coniferous mixed taiga forest by Thermochron (DS1921G-F5) (temperature logger), 2015-continues, 30, 60 or 180 min frequency depending on season, there one gap in data, N61.07960 E69.45287, as part of meteorological monitoring in Mukhrino Field Station (https://mukhrinostation.com/).

Air temperature at 2m measured in a raised bog ecosystem by DS18B20 (temperature logger), 2012-2018, 30 and 60 min frequency, several gaps in data, N60.89471 E68.68176, as part of meteorological monitoring in Mukhrino Field Station (https://mukhrinostation.com/).

Air temperature at 2m measured in a raised bog ecosystem (ridge) by Baro-Diver (DI 500), 2006-2016 (with several breaks) as part of meteorological monitoring in Mukhrino Field Station (https://mukhrinostation.com/).

Air temperature at 2m measured in a raised bog ecosystem (sphagnum lawn) by DS18B20 (temperature logger), 2016, 30 min frequency, N60.89325 E68.68311, OTC-wet experimental site, as part of meteorological monitoring in Mukhrino Field Station (https://mukhrinostation.com/).

Meteorology data provided for the H2020 eLTER project with a range from 1972 - 2018. These time series are inhomogeneous because of station relocations and changes in observation techniques. As a result, these series are not suitable for trend analysis. For climate change studies we refer to the homogenized series of monthly temperatures of De Bilt <http://www.knmi.nl/kennis-en-datacentrum/achtergrond/gehomogeniseerde-reeks-maandtemperaturen-de-bilt> or the Central Netherlands Temperature <http://www.knmi.nl/kennis-en-datacentrum/achtergrond/centraal-nederland-temperatuur-cnt>.

Air temperature of meteorological Station Rudolfshütte