Soil temperature is measured at various depths below the soil surface from approximately 2 cm down to 200 cm at non-permafrost sites (down to 300 cm at Alaskan sites). Soil temperature influences the
Additionally, at four shallow water stations (Booknis Eck, Buelk, Behrensdorf and Katharinenhof) temperature, salinity and dissolved oxygen are continuously logged at 2-3 m depth by self-contained dat
