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Evaluating the extent of implementation and variation of typical school provision of physical education, physical activity and sports in the Republic of Ireland is a public health priority. Therefore, a national audit into the different levels of typical school provision of physical education, physical activity and sports was conducted. To date, this has not been evaluated. A cross-sectional, nationally representative sample of 112 secondary schools were included. A school provision of physical education, physical activity and sports evaluation index, validated via a concept mapping methodology, was utilized to measure variation of provision in the context of school personnel, curriculum, facilities and equipment, budget, partnerships, ethos and prioritization. A proposed grade for each indicator of provision was established using an internationally standardized grading system. Overall, physical education was the indicator with the highest national average grade (B−); physical activity was the indicator with the lowest national average grade (D+); while the indicator for sports received a C− grade. An overview of the national averages in terms of provision, paralleled with national and international comparisons and recommendations to support provision, is illuminated for each indicator. Future country comparison and benchmarking on key components of provision is envisaged. [ABSTRACT FROM AUTHOR]

Peatland rewetting has been proposed as a vital climate change mitigation tool to reduce greenhouse gas emissions and to generate suitable conditions for the return of carbon (C) sequestration. In this study, we present annual C balances for a 5‐year period at a rewetted peatland in Ireland (rewetted at the start of the study) and compare the results with an adjacent drained area (represents business‐as‐usual). Hydrological modelling of the 230‐hectare site was carried out to determine the likely ecotopes (vegetation communities) that will develop post‐rewetting and was used to inform a radiative forcing modelling exercise to determine the climate impacts of rewetting this peatland under five high‐priority scenarios (SSP1‐1.9, SS1‐2.6, SSP2‐4.5, SSP3‐7.0 and SSP5‐8.5). The drained area (marginal ecotope) was a net C source throughout the study and emitted 157 ± 25.5 g C m−2 year−1. In contrast, the rewetted area (sub‐central ecotope) was a net C sink of 78.0 ± 37.6 g C m−2 year−1, despite relatively large annual methane emissions post‐rewetting (average 19.3 ± 5.2 g C m−2 year−1). Hydrological modelling predicted the development of three key ecotopes at the site, with the sub‐central ecotope predicted to cover 24% of the site, the sub‐marginal predicted to cover 59% and the marginal predicted to cover 16%. Using these areal estimates, our radiative forcing modelling projects that under the SSP1‐1.9 scenario, the site will have a warming effect on the climate until 2085 but will then have a strong cooling impact. In contrast, our modelling exercise shows that the site will never have a cooling impact under the SSP5‐8.5 scenario. Our results confirm the importance of rapid rewetting of drained peatland sites to (a) achieve strong C emissions reductions, (b) establish optimal conditions for C sequestration and (c) set the site on a climate cooling trajectory. [ABSTRACT FROM AUTHOR]

Drainage and conversion of natural peatlands to forestry increases soil CO2 emissions through decomposition of peat and modifies the quantity and quality of litter inputs and therefore the soil carbon balance. In organic soils, CO2 net emissions and removals are reported using carbon emission factors (EF). The choice of specific default Tier 1 EF values from the IPCC 2013 Wetlands supplement depends on land‐use categories and climate zones. However, Tier 1 EF for afforested peatlands in the temperate maritime climate zone are based on data from eight sites, mainly located in the hemiboreal zone, and the uncertainty associated with these default values is a concern. In addition, moving from Tier 1 to higher‐Tier carbon reporting values is highly desirable when large areas are affected by land‐use changes. In this study, we estimated site‐specific soil carbon balance for the development of Tier 2 soil CO2‐C EFs for afforested peatlands. Soil heterotrophic respiration and aboveground tree litterfall were measured during two years at eight afforested peatland sites in Ireland. In addition, fine‐root turnover rate and site‐specific fine‐root biomass were used to quantify belowground litter inputs. We found that drainage of peatlands and planting them with either Sitka spruce or lodgepole pine, resulted in soils being net carbon sources. The soil carbon balance at multi‐year sites varied between 63 ± 92 and 309 ± 67 g C m−2 year−1. Mean CO2‐C EF for afforested peatlands was 1.68 ± 0.33 t CO2‐C ha−1 year−1. The improved CO2‐C EFs presented here for afforested peatlands are proposed as a basis to update national CO2‐C emissions from this land‐use class in Ireland. Furthermore, new data from these sites will significantly contribute to the development of more reliable IPCC default Tier 1 CO2‐C EFs for afforested peatlands in the maritime temperate climate zone. [ABSTRACT FROM AUTHOR]