Climatic control of the high-latitude vegetation greening trend and Pinatubo effect

Wolfgang Lucht*, I. Colin Prentice, Ranga B. Myneni, Stephen Sitch, Pierre Friedlingstein, Wolfgang Cramer, Philippe Bousquet, Wolfgang Buermann, Benjamin Smith

*Corresponding author for this work

Research output: Contribution to journalArticle

492 Citations (Scopus)

Abstract

A biogeochemical model of vegetation using observed climate data predicts the high northern latitude greening trend over the past two decades observed by satellites and a marked setback in this trend after the Mount Pinatubo volcano eruption in 1991. The observed trend toward earlier spring budburst and increased maximum leaf area is produced by the model as a consequence of biogeochemical vegetation responses mainly to changes in temperature. The post-Pinatubo decline in vegetation in 1992-1993 is apparent as the effect of temporary cooling caused by the eruption. High-latitude CO2 uptake during these years is predicted as a consequence of the differentia[response of heterotrophic respiration and net primary production.

Original languageEnglish
Pages (from-to)1687-1689
Number of pages3
JournalScience
Volume296
Issue number5573
DOIs
Publication statusPublished - 31 May 2002
Externally publishedYes

    Fingerprint

Cite this

Lucht, W., Prentice, I. C., Myneni, R. B., Sitch, S., Friedlingstein, P., Cramer, W., ... Smith, B. (2002). Climatic control of the high-latitude vegetation greening trend and Pinatubo effect. Science, 296(5573), 1687-1689. https://doi.org/10.1126/science.1071828