Atlas of Microclimate Development for Bohemian Forest Ecosystem, including the Effect of Forest Stands
Authors/Creators
Description
The maps present estimated future microclimatic characteristics for 20-year periods (2021–2040 (“2030”), 2041–2060 (“2050”), 2061–2080 (“2070”), 2081–2100 (“2090”)) at 25 m resolution. They were produced by adding a multi-model anomaly to local microclimate maps of the reference period, which also incorporate future forest development simulated with the forest landscape growth model LANDIS-II (v7.1) using the PnET extension (v5.1).
The anomaly is defined as the difference between the climatology of a given future 20-year period and the reference climatology (October 2019–September 2024; hydrological year = October–September).
The multi-model estimate is reported as the median across models; model uncertainty is expressed as the interquartile range (IQR = Q75 − Q25).
Projection data source: CMIP6 projections from the Copernicus Climate Data Store (CDS), dataset CMIP6 climate projections (projections-cmip6, DOI: 10.24381/cds.c866074c).
SSP scenarios (Shared Socioeconomic Pathways) from the ScenarioMIP project: SSP2-4.5 (intermediate future emissions) and SSP5-8.5 (very high future emissions).
BFE_2020-2024_CLIM_yearly_mean_with_climate.rdata - Microclimate information from 288 microclimate sites covering October 2019 - September 2024.
BFE_landis.rdata - values of topographic parameters and forest structure information from LANDIS-II model with PnET extension for the 288 sites
Filename includes SSP, 20 year period code, climate variable and IQR layers have _iqr suffix
SSP245_2030_T.air_200cm.max95_iqr.tif
GeoTIFF format, coordinate system EPSG 31468, resolution 25 m
Other (Czech)
Mapy zobrazují odhad budoucí mikroklimatických charakteristik pro 20-letá období (2021–2040 (“2030”), 2041–2060 (“2050”), 2061–2080 (“2070”), 2081–2100 (“2090”) v rozlišení 25 m. Vznikly přičtením vícemodelové odchylky k lokálním mikroklimatickým mapám referenčního období, které zohledňují i budoucí vývoj lesních porostů modelovaný pomocí krajinného modelu růstu lesa LANDIS-II (v7.1) s využitím extenze PnET (v5.1).
Odchylka je definována jako rozdíl mezi klimatologií budoucího dvacetiletého období a referenční klimatologií (říjen 2019 – září 2024; hydrologický rok = říjen–září).
Vícemodelový odhad je uveden jako medián napříč modely; modelová nejistota je vyjádřena mezikvartilovým rozpětím (IQR = Q75 − Q25).
Datový zdroj projekcí: CMIP6 projekce z Copernicus Climate Data Store (CDS), dataset CMIP6 climate projections (projections-cmip6, DOI: 10.24381/cds.c866074c).
Scénáře SSP (Shared Socioeconomic Pathways) z projektu ScenarioMIP SSP2-4.5 (střední budoucí emise) a SSP5-8.5 (velmi vysoké budoucí emise).
BFE_2020-2024_CLIM_yearly_mean_with_climate.rdata - Mikroklimatické proměnné z 288 lokalit z období říjen 2019 - září 2024.
BFE_landis.rdata - hodnoty topografických parametrů a proměnných popisujích strukturu lesa z modelu LANDIS-II s extenzí PnET pro 288 lokalit
Názvy souborů jsou tvořeny SSP, kódem 20 letého období, klimatickou proměnnou a vrstvy IQR mají koncovku _iqr
SSP245_2030_T.air_200cm.max95_iqr.tif
formát GeoTIFF , EPSG 31468, rozlišení 25 m
Files
SSP245_2030_T.air_200cm.max95.tif
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Additional details
Additional titles
- Translated title (Czech)
- Atlas vývoje mikroklimatu Šumavy zohledňující vliv lesních porostů
Funding
- Technology Agency of the Czech Republic
- Forest microclimate in time and space: real impacts of climate change on selected protected areas SS06010011
References
- Copernicus Climate Change Service (C3S): CMIP6 climate projections (CDS dataset projections-cmip6), https://doi.org/10.24381/cds.c866074c
- Brůna, J. et al. High-resolution microclimatic grids for the Bohemian Forest Ecosystem based on in situ measurements. Sci. Data (2026). doi:10.1038/s41597-026-06566-z
- Brůna, J. et al. High-resolution microclimatic grids for the Bohemian Forest Ecosystem. (2025). doi:10.5281/zenodo.17671120