Causes of spring vegetation growth trends in the northern midhigh latitudes from 1982 to 2004

Research output: Contribution to journalArticlepeer-review

55 Scopus citations

Abstract

The Community Land Model version 4 (CLM4) is applied to explore the spatialtemporal patterns of spring (AprilMay) vegetation growth trends over the northern midhigh latitudes (NMH) (>25°N) between 1982 and 2004. During the spring season through the 23yr period, both the satellite-derived and simulated normalized difference vegetation index (NDVI) anomalies show a statistically significant correlation and an overall greening trend within the study area. Consistently with the observed NDVItemperature relation, the CLM4 NDVI shows a significant positive association with the spring temperature anomaly for the NMH, North America and Eurasia. Large study areas experience temperature discontinuity associated with contrasting NDVI trends. Before and after the turning point (TP) of the temperature trends, climatic variability plays a dominant role, while the other environmental factors exert minor effects on the NDVI tendencies. Simulated vegetation growth is broadly stimulated by the increasing atmospheric CO2. Trends show that nitrogen deposition increases NDVI mostly in southeastern China, and decreases NDVI mainly in western Russia after the temperature TP. Furthermore, land use-induced NDVI trends vary roughly with the respective changes in land management practices (crop areas and forest coverage). Our results highlight how non-climatic factors mitigate or exacerbate the impact of temperature on spring vegetation growth, particularly across regions with intensive human activity.

Original languageEnglish
Article number014010
JournalEnvironmental Research Letters
Volume7
Issue number1
DOIs
StatePublished - Mar 2012

Keywords

  • CLM4
  • NDVI
  • temperature turning point
  • vegetation growth trends

Fingerprint

Dive into the research topics of 'Causes of spring vegetation growth trends in the northern midhigh latitudes from 1982 to 2004'. Together they form a unique fingerprint.

Cite this