
Anders Lindroth
Professor emeritus

Early snowmelt significantly enhances boreal springtime carbon uptake
Författare
Summary, in English
We determine the annual timing of spring recovery from spaceborne microwave radiometer observations across northern hemisphere boreal evergreen forests for 1979–2014. We find a trend of advanced spring recovery of carbon uptake for this period, with a total average shift of 8.1 d (2.3 d/decade). We use this trend to estimate the corresponding changes in gross primary production (GPP) by applying in situ carbon flux observations. Micrometeoro-logical CO2 measurements at four sites in northern Europe and North America indicate that such an advance in spring recovery would have increased the January–June GPP sum by 29 g·C·m−2 [8.4 g·C·m−2 (3.7%)/decade]. We find this sensitivity of the measured springtime GPP to the spring recovery to be in accordance with the corresponding sensitivity derived from simulations with a land ecosystem model coupled to a global circulation model. The model-predicted increase in springtime cumulative GPP was 0.035 Pg/decade [15.5 g·C·m−2 (6.8%)/decade] for Eurasian forests and 0.017 Pg/decade for forests in North America [9.8 g·C·m−2 (4.4%)/decade]. This change in the springtime sum of GPP related to the timing of spring snowmelt is quantified here for boreal evergreen forests.
Avdelning/ar
- Institutionen för naturgeografi och ekosystemvetenskap
- BECC: Biodiversity and Ecosystem services in a Changing Climate
Publiceringsår
2017-10-17
Språk
Engelska
Sidor
11081-11086
Publikation/Tidskrift/Serie
Proceedings of the National Academy of Sciences of the United States of America
Volym
114
Issue
42
Dokumenttyp
Artikel i tidskrift
Förlag
National Academy of Sciences
Ämne
- Physical Geography
Nyckelord
- Carbon uptake
- Earth observation
- Snowmelt
Aktiv
Published
ISBN/ISSN/Övrigt
- ISSN: 0027-8424