SVK00139 - Quercus petraea

National gene conservation unit number: qpeG12TO-140

Population number: -

Target species for conservation in the GCU:
Quercus petraea

GCU

Date of collection of the field data entered: 2016

Date of the most recent visit: 2020

POPULATION

Year of Establishment of the GCU for the species: 2009

Date (or partial of date) of the most recent visit: 2018

Location

Unit province or state:
Nitra

Unit department or county:
Topoľčany

Unit municipality:
Topoľčany

Unit local name:
Myslíková

Unit elevation [m a.s.l.]:
330 - 335

Unit surface area [ha]:
170.42

Coordinates privacy:
Public

Ownership of the unit:
Public

Coordinates:
Latitude (Decimal):48.6852 | Longitude (Decimal): 18.0827

Map (Public coordinates)
Species

All tree species growing in the unit:
Quercus petraea

Target species for conservation in the GCU:
Quercus petraea

Unit Type
  • Gene reserve forest
GLOBAL ENVIRONMENT STRATIFICATION [GENS]

The global environment stratification identifier composed of the concatenation of the environmental zone code and the stratification code (ID):

Climatic zone (C):

Environmental zone (E):

Aggregated environmental zoning of Europe (AE):

HARMONIZED WORLD SOIL [HWSD]

This element represents the the harmonized world soil database, this attribute provides soil information in the 30 seconds grid, reference information can be found here:

CHELSA version 2.1

CHELSA version 2.1 is based on a mechanistical statistical downscaling of global reanalysis data or global circulation model output, it is a model that aims at representing reality as precise as possible. It provides high spatial resolution (30 arc seconds) global weather and climate data for historical data, 1981-2010, and future modelled climate scenarios.

Future climate scenarios come from the Max Plank Institute Earth System Model version MPI-ESM1-2-HR, a climate model developed as part of the internationally-coordinated Coupled Model Intercomparison Project Phase 6 (CMIP6). The values were averages over 3 20 year periods: 2011-2040, 2041-2070 and 2071-2100.

Shared Socioeconomic Pathways (SSPs) are climate change scenarios of projected socioeconomic global changes up to 2100 as defined in the IPCC Sixth Assessment Report on climate change in 2021. Of these the Shared Socioeconomic Pathway SSP3-RCP7 was selected: regional rivalry (a rocky road).

"The world follows a path in which social, economic, and technological trends do not shift markedly from historical patterns. Development and income growth proceeds unevenly, with some countries making relatively good progress while others fall short of expectations. Global and national institutions work toward but make slow progress in achieving sustainable development goals. Environmental systems experience degradation, although there are some improvements and overall the intensity of resource and energy use declines. Global population growth is moderate and levels off in the second half of the century. Income inequality persists or improves only slowly and challenges to reducing vulnerability to societal and environmental changes remain."

 

Project: EUFGIS

All values are averages for the selected period

No data

WorldClim version 2.1

WorldClim version 2.1 is a database of high spatial resolution (30 arc seconds) global weather and climate data, it provides historical data, 1970-2000, and future modelled climate scenarios ranging from 2021 to 2100.

Future climate scenarios come from the Max Plank Institute Earth System Model version MPI-ESM1-2-HR, a climate model developed as part of the internationally-coordinated Coupled Model Intercomparison Project Phase 6 (CMIP6). The monthly values were averages over 4 20 year periods, 2021-2040, 2041-2060, 2061-2080 and 2081-2100.

Shared Socioeconomic Pathways (SSPs) are climate change scenarios of projected socioeconomic global changes up to 2100 as defined in the IPCC Sixth Assessment Report on climate change in 2021. Of these the Shared Socioeconomic Pathway SSP3-RCP7 was selected: regional rivalry (a rocky road).

"The world follows a path in which social, economic, and technological trends do not shift markedly from historical patterns. Development and income growth proceeds unevenly, with some countries making relatively good progress while others fall short of expectations. Global and national institutions work toward but make slow progress in achieving sustainable development goals. Environmental systems experience degradation, although there are some improvements and overall the intensity of resource and energy use declines. Global population growth is moderate and levels off in the second half of the century. Income inequality persists or improves only slowly and challenges to reducing vulnerability to societal and environmental changes remain."

 

Project: EUFGIS

All values are averages for the selected period

No data

Soil moisture index

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SMI is an indicator of moisture conditions in the uppermost soil layers (skin layer and root zone). SMI is equal to 0 when the soil is severely dry (wilting point) and equal to 1 when the soil moisture is high (above field capacity)

Soil moisture anomaly

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The SMA indicator is used to detect and monitor agricultural drought, which is one of three main types of drought that are defined according to the variables of the hydrological cycle. SMA expresses the deviation of actual SMI from its long term mean . The baseline period for SMA is 1995 to the last available full year. SMA is negative when soil moisture is lower than the reference baseline. The following classification can be applied: SMA<-1.0: mild drought; SMA<-1.5: severe drought; SMA<-2: extreme drought

Fraction of Absorbed Photosynthetically Active Radiation (FAPAR).

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Monitors the impacts of agricultural drought on the growth and productivity of vegetation.

Fraction of Absorbed Photosynthetically Active Radiation Anomaly (FAPAN).

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Monitors the impacts of agricultural drought on the growth and productivity of vegetation.

Fraction of Photosynthetically Active Radiation [%]

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This biophysical variable is directly related to the primary productivity of forests and some models use it to estimate the assimilation of carbon dioxide in vegetation. FPAR can also be used as an indicator of the state and evolution of the vegetation cover

DATA

Average GCU Biomass
200.1

Dominant leaf type
Broadleaved

Average GCU canopy height
22.53

Map (Public coordinates)
Average GCU NDVI [-/month]

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Monthly average of the Normalized Difference Vegetation Index

Average GCU LAI [m2 Leaf/m2 Soil]

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Monthly average of the Leaf Area Index

GCU Land surface temperature

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Land Surface Temperature (skin temperature)of the GCU.

Average GCU NDWI

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Average Normalized Difference Water Index

Average GCU GPP [kg of C/m^2/day]

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Monthly average of the Gross Primary Productivity

Soil temperature from 0 to 7cm. [K]

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Temperature of the soil in layer 1 (0 - 7 cm) of the ECMWF Integrated Forecasting System.

Soil temperature from 7 to 28cm. [K]

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Temperature of the soil in layer 2 (7-28 cm) of the ECMWF Integrated Forecasting System.

Soil temperature from 28 to 100cm. [K]

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Temperature of the soil in layer 3 (28-100 cm) of the ECMWF Integrated Forecasting System.

Soil temperature from 100 to 289cm. [K]

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Temperature of the soil in layer 4 (100-289 cm) of the ECMWF Integrated Forecasting System.

Volumetric soil water layer from 0 to 7cm. [%]

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Volume of water in soil layer 1 (0 - 7 cm) of the ECMWF Integrated Forecasting System.

Volumetric soil water layer from 7 to 28cm. [%]

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Volume of water in soil layer 2 (7 - 28 cm) of the ECMWF Integrated Forecasting System.

Volumetric soil water layer from 28 to 100cm. [%]

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Volume of water in soil layer 3 (28 - 100 cm) of the ECMWF Integrated Forecasting System.

Volumetric soil water layer from 100 to 289cm. [%]

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Volume of water in soil layer 4 (100 - 289 cm) of the ECMWF Integrated Forecasting System.

Air temperature at 2 meters [K]

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Temperature of air at 2m above the surface of land, sea or in-land waters.

Total precipitation [kg m^2 month]

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Accumulated liquid and frozen water that falls to the Earth's surface.

Relative humidity [%]

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Relative humidity (RH) refers to the moisture content (i.e., water vapor) of the atmosphere, expressed as a percentage of the amount of moisture that can be retained by the atmosphere (moisture-holding capacity) at a given temperature and pressure without condensation.

Wind speed [m s]

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Wind speed in meters per second.

Surface latent heat flux [J/m^2]

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Exchange of latent heat with the surface through turbulent diffusion.

Surface net solar radiation [J m^2 day]

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Amount of solar radiation reaching the surface of the Earth minus the amount reflected by the Earth's surface.

Characteristics

Status of the target species in the GCU:
-

Category of the target species in the GCU:
In situ

Origin of the target species in the GCU :
Autochtonous

Justification for conserving the target species in the GCU:
To maintain genetic diversity in large tree populations

Estimated number of reproducing trees (interval):
500 - 4999

Justification for conserving the target species in the GCU:
To maintain genetic diversity in large tree populations

Number of reproducing trees:
-

Estimation method for number of reproducing trees:
-

Sex ratio of the target species in the GCU :
-

Status of long-term viable regeneration:
-

Distribution of reproducing trees of the target species in the GCU:
-

Population share (%):
147%

Management

Population management:
-

Predominant silvicultural system:
-

Population remarks:
-

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