4.7 Article

The influence of system heterogeneity on peat-surface temperature dynamics

期刊

ENVIRONMENTAL RESEARCH LETTERS
卷 16, 期 2, 页码 -

出版社

IOP PUBLISHING LTD
DOI: 10.1088/1748-9326/abd4ff

关键词

ecosystem heterogeneity; hot spots and moments; ecosystem resilience; peatland

资金

  1. Natural Environment Research Council [NE/L501712/1]
  2. Syncrude Canada Ltd
  3. Canadian Natural Resources Ltd [SCL4600100599]
  4. Natural Sciences and Engineering Research Council [NSERC-CRD CRDPJ477235-14]
  5. NERC [NE/L501712/1] Funding Source: UKRI

向作者/读者索取更多资源

Temperatures at the soil-atmosphere interface play a crucial role in ecosystem function by driving nonlinear processes. The complexity of thermal ecosystems created by interacting and heterogeneous layers remains unclear, especially in peatlands. System heterogeneity influences thermal regimes, with not all layers having equal impact, and changes in extremes may occur without significant alterations in overall temperatures, highlighting the need for further research on small-scale thermal dynamics and their impact on ecosystem function.
Temperatures at the soil-atmosphere interface influence ecosystem function by driving nonlinear terrestrial biogeochemical, ecohydrological, and micrometeorological processes. Whilst climate, soil and vegetation controls on spatially average ecosystem temperatures are recognised, how interacting and heterogeneous ecosystem layers create spatio-temporal complex thermal ecosystems has not been determined. Such thermal hot spots and hot moments may underpin the capability of ecosystems to support biological and biogeochemical diversity and control the likelihood of tipping points in system-regulating feedbacks being locally exceeded. This is of notable importance in peatlands, where soil temperatures control the storage of their associated globally important carbon stocks. Here, through the application of high spatio-temporal resolution surface temperature data and peat thermal modelling, we assess the impact of system heterogeneity (spatio-temporal impact of the following system layers: tree, shrubs, microtopography, groundcover species and sub-surface ice) on surface temperature regimes. We show (a) that peat-surface thermal hotspot intensity and longevity is linked to system heterogeneity and (b) that not all system layers have an equal influence over the peat-surface thermal regime and extreme temperatures; thermal heterogeneity increases up to a maximum of five layers of heterogeneity and decreases thereafter. The results crucially demonstrate that such changes in the spatio-temporal thermal dynamics and extremes may occur without significant changes in median temperatures. This is important to the conceptual understanding of peatland responses and ecosystem resilience to disturbance. It emphasises the need to determine the potential for transitions in magnitude, longevity and locality of small-scale thermal extremes to induce functional transitions that propagate through given ecosystems, and to characterise the impact of such small-scale spatio-temporal complexity on ecosystem scale biogeochemical and ecohydrological function.

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