Projected Changes in Terrestrial Vegetation and Carbon Fluxes under 1.5 °C and 2.0 °C Global Warming

Abstract

The terrestrial ecosystem plays a vital role in regulating the exchange of carbon between land and atmosphere. This study investigates how terrestrial vegetation coverage and carbon fluxes change in a world stabilizing at 1.5 °C and 2 °C warmer than pre-industrial level. Model results derived from 20 Earth System Models (ESMs) under low, middle, and high greenhouse emission scenarios from CMIP5 and CMIP6 are employed to supply the projected results. Although the ESMs show a large spread of uncertainties, the ensemble means of global LAI are projected to increase by 0.04 ± 0.02 and 0.08 ± 0.04 in the 1.5 and 2.0 °C warming worlds, respectively. Vegetation density is projected to decrease only in the Brazilian Highlands due to the decrease of precipitation there. The high latitudes in Eurasia are projected to have stronger increase of LAI in the 2.0 °C warming world compared to that in 1.5 °C warming level caused by the increase of tree coverage. The largest zonal LAI is projected around 70° N while the largest zonal NPP is projected around 60° N and equator. The zonally inhomogeneous increase of vegetation density and productivity relates to the zonally inhomogeneous increase of temperature, which in turn could amplify the latitudinal gradient of temperature with additional warming. Most of the ESMs show uniform increases of global averaged NPP by 10.68 ± 8.60 and 15.42 ± 10.90 PgC year−1 under 1.5 °C and 2.0 °C warming levels, respectively, except in some sparse vegetation areas. The ensemble averaged NEE is projected to increase by 3.80 ± 7.72 and 4.83 ± 10.13 PgC year−1 in the two warming worlds. The terrestrial ecosystem over most of the world could be a stronger carbon sink than at present. However, some dry areas in Amazon and Central Africa may convert to carbon sources in a world with additional 0.5 °C warming. The start of the growing season in the northern high latitudes is projected to advance by less than one month earlier. Five out of 10 CMIP6 ESMs, which use the Land Use Harmonization Project (LUH2) dataset or a prescribed potential vegetation distribution to constrain the future change of vegetation types, do not reduce the model uncertainties in projected LAI and terrestrial carbon fluxes. This may suggest the challenge in optimizing the carbon fluxes modeling in the future.

Projected changes of ecosystem productivity and their responses to extreme heat events in northern asia

“…However, high temperatures beyond the plant tolerance threshold can increase plant respiration and inhibit photosynthesis (Salvucci and Crafts-Brandner, 2004). Some studies have shown that temperature extremes may decrease the plant productivity and change the carbon cycle of the ecosystem through affecting plant physiological processes (Meehl et al, 2000;Smith et al, 2009;Frank et al, 2015;Piao et al, 2019;Peng et al, 2022). For example, the heat wave event occurring in western Russia in 2010 led to a significant decrease in local ecosystem productivity (Bastos et al, 2014).…”

Sixth Oregon climate assessment

“…Furthermore, in temperate regions, CMIP6 models overestimate tree height, which may lead to overestimating aboveground carbon storage and underestimating wind speed (Song et al 2021). However, in both CMIP5 and CMIP6 models, leaf area index is projected to increase in virtually all biomes worldwide under scenarios of 1.5˚C and 2˚C warming above pre-industrial levels (Peng et al 2022).…”