Unravel the changing contributions of abiotic vs. biotic drivers of exosystem gas exchange under weather extremes (EcoDrive), Davos Seehornwald ...

• Main Author: Bruggisser, Moritz
• Format: Dataset
• Language: unknown
• Published: ETH Zurich 2022
• Subjects: forest; alpine tundra; NDVI; NEE; extreme event; modelling; Norway; Tundra
• Online Access: https://dx.doi.org/10.5905/ethz-1002-22925; https://app.data-archive.ethz.ch/delivery/DeliveryManagerServlet?dps_pid=IE31910191

Site: Davos Seehornwald CH-DAV (canton Grisons, Switzerland) is situated close to the Davos town in the Eastern Alps. The vegetation of the Davos forest is typical for a subalpine mountain forest: it is dominated by Norway spruce (Picea abies (L.) Karst.). The patchy understory is dominated by dwarf shrubs of Vaccinium myrtillus L. and V. gaultherioides L., and moss mats (Sphagnum sp. Ehrh.).; Longitude (WGS 84): 9°51'21.3" E; Latitude (WGS 84): 46°48'55.2" N; Altitude (m.a.s.l.): 1639; Land cover (IGBP classification): Evergreen Needleleaf Forest; Soil type: The main soil types are rustic podsols and chromic cambisols according to the World Reference Base of Soil Resources (IUSS Working Group WRB, 2007) with a thick organic layer (4-10 cm).; Geology: Crystalline bedrock and dolomitic rocks of the Arosa nappe (lower eastern alpine). Moraine rubble. (Jörg 2008). ...