Contrasting responses of terrestrial ecosystem production to hot temperature extreme regimes between grassland and forest

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Abstract

During the past several decades, observational data have shown a faster increase in hot temperature extremes than the change in mean temperature. Increasingly high extreme temperatures are expected to affect terrestrial ecosystem function. The ecological impact of hot extremes on vegetation production, however, remains uncertain across biomes in natural climatic conditions. In this study, we investigated the effects of hot temperature extremes on vegetation production by combining the MODIS enhanced vegetation index (EVI) data set and in situ climatic records during the period 2000 to 2009 from 12 long-term experimental sites across biomes and climate. Our results show that higher mean annual maximum temperatures (Tmax) greatly reduced grassland production, and yet enhanced forest production after removing the effect of precipitation. The relative decrease in vegetation production was 16% for arid grassland and 7% for mesic grassland, and the increase was 5% for forest. We also observed a significantly positive relationship between interannual aboveground net primary production (ANPP) and Tmax for the forest biome (R2 Combining double low line 0.79, P < 0.001). This line of evidence suggests that hot temperature extremes lead to contrasting ecosystem-level responses of vegetation production between grassland and forest biomes. Given that many terrestrial ecosystem models use average daily temperature as input, predictions of ecosystem production should consider such contrasting responses to increasingly hot temperature extreme regimes associated with climate change.

Figures

  • Table 1. Descriptions of the sites in this studya.
  • Figure 1. Relationship between annual ground measurements of ANPP (ANPPG) and the corresponding iEVI derived from MODIS data during the period between 2000 and 2009 for nine selected sites across biomes (R2 = 0.90, P < 0.0001; Table 2). The upper inset shows the relationship at two sites of CP and JE (R2 = 0.63 and 0.74, respectively, P < 0.01). The lower inset shows the relationship between ANPPG and iEVI for the year 2001 across the 9 sites (R2 = 0.88, P < 0.001).
  • Table 2. Sites with “in-situ” ANPP measurements within the period of 2000–2009 for validation with iEVI.
  • Figure 2. Long-term trends of the anomaly of Tmax during 1970– 2009 for different biome types. DG, arid grassland sites (DE, JE, WG, SR, and CP in Table 1); MG, mesic grassland sites (SP and LW in Table 1); TF, temperate forested sites (LR, MC, BC, and CF in Table 1); MF, Mediterranean forested site (CC). The dotted line shows the year of 2000 for the starting year of the MODIS EVI data set.
  • Figure 3. Relationship between iEVI and Tmax and their maximumyear Tmax–iEVI relationship for five forested sites. The dotted line shows the linear relationship between maximum-year Tmax and the relevant iEVI for all the sites.
  • Figure 4. Comparison of iEVI differences between the extreme years and average of all other years of Tmax across sites. Extreme years mean that the years of Tmax anomaly are ≥ 1. The inset denotes the average differences by biome type. DG, arid grassland sites (DE, JE, WG, and SR in Table 1); MG, mesic grassland sites (CP, SP, and LW in Table 1); TF, temperate forested sites (LR, MC, BC, and CF in Table 1); MF, Mediterranean forested site (CC). Different letters indicate significant differences at P < 0.05.
  • Figure 5. Partial correlations between iEVI and Tmax after controlling the effects of Tmin and precipitation across sites. (1) Statistically significant at the 95 % (P < 0.05) level; (2) statistically significant at the 99.9 % (P < 0.001) level.

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APA

Zhang, Y., Voigt, M., & Liu, H. (2015). Contrasting responses of terrestrial ecosystem production to hot temperature extreme regimes between grassland and forest. Biogeosciences, 12(2), 549–556. https://doi.org/10.5194/bg-12-549-2015

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