Shifting relative importance of climatic constraints on land surface phenology

• Published in: Environmental research letters 2018-02, Vol.13 (2), p.24025
• Main Authors: Garonna, Irene, de Jong, Rogier, Stöckli, Reto, Schmid, Bernhard, Schenkel, David, Schimel, David, Schaepman, Michael E
• Format: Article
• Language: English
• Subjects: Climate change; Climate effects; climatic constraints; end of season; land surface phenology; minimum temperature; Moisture; Moisture availability; Phenology; photoperiod; Remote sensing; Seasonal variations; Seasons; start of season; vapour pressure deficit; Vegetation
• ISSN: 1748-9326; 1748-9326
• DOI: 10.1088/1748-9326/aaa17b

Land surface phenology (LSP), the study of seasonal dynamics of vegetated land surfaces from remote sensing, is a key indicator of global change, that both responds to and influences weather and climate. The effects of climatic changes on LSP depend on the relative importance of climatic constraints in specific regions-which are not well understood at global scale. Understanding the climatic constraints that underlie LSP is crucial for explaining climate change effects on global vegetation phenology. We used a combination of modelled and remotely-sensed vegetation activity records to quantify the interplay of three climatic constraints on land surface phenology (namely minimum temperature, moisture availability, and photoperiod), as well as the dynamic nature of these constraints. Our study examined trends and the relative importance of the three constrains at the start and the end of the growing season over eight global environmental zones, for the past three decades. Our analysis revealed widespread shifts in the relative importance of climatic constraints in the temperate and boreal biomes during the 1982-2011 period. These changes in the relative importance of the three climatic constraints, which ranged up to 8% since 1982 levels, varied with latitude and between start and end of the growing season. We found a reduced influence of minimum temperature on start and end of season in all environmental zones considered, with a biome-dependent effect on moisture and photoperiod constraints. For the end of season, we report that the influence of moisture has on average increased for both the temperate and boreal biomes over 8.99 million km2. A shifting relative importance of climatic constraints on LSP has implications both for understanding changes and for improving how they may be modelled at large scales.