AndreaBozzo/ceres-open-data-index huggingface dataset:
Monthly rainfall erosivity (R-factor) maps of Switzerland in MJ mm ha⁻¹ h⁻¹ month⁻¹, November

<p>Monthly rainfall erosivity maps (R-factor maps) of Switzerland with a spatial resolution of 100 m. The maps show the spatial and seasonal variability of rainfall erosivity in MJ mm ha⁻¹ h⁻¹ month⁻¹. Light shades of blue indicate a low erosive impact of rainfall and dark shades a high impact.</p> <p>The monthly R-factors are based on precipitation measurements from 87 automatic gauging stations with measurement intervals of 10 minutes (average measuring period of 19.5 years per station). The stations cover all agricultural zones in Switzerland. To exclude the influence of snow, temperatures are also recorded at an hourly resolution for 71 stations or are derived from the nearest station.</p> <p>A comparison of the 12 monthly R-factor maps shows that the summer months (June, July and August) have the highest rainfall erosivity values during the year. The Southern Alps (canton of Ticino), the mountain zones of the Northern Alps and parts of the valley zone have particularly high R-factors in this period. A proportion of 62% of Switzerland's annual rainfall erosivity is recorded between June and September. Identifying regions and periods in which rainfall with an increased erosive impact occurs enables targeted erosion control and a better understanding of the dynamics of erosion processes over the course of a year.</p> The development of monthly rainfall erosivity maps of Switzerland is described in detail in 'Regionalization of monthly rainfall erosivity patterns in Switzerland' by Schmidt et al. (Hydrology and Earth System Sciences: 20. 2016. pp. 4359–4373).
Invasive alien plants - map of the potential area Elodea nuttallii

The set of invasive alien plants shows the maps of the potential areas of 56 alien plants species present in Switzerland as well as some invasive species present in neighboring countries with the potential to reach Switzerland. The maps are the result of model-based tool to anticipate the spread of invasive alien plants listed on the Swiss Black and Watch list. The model is using occurrence data from GBIF (Global Biodiversity Information Facility), current climate data from Worldclim(1 km resolution) and occurrence data from InfoFlora combined with climate data from the WSL (100 m resolution).The maps with 100 m resolution utilize additional necessary variables including landuse and geology.
Thermal continentality at 1000 m a.s.l. in the year, period 1981-2010

The thermal continentality in °C was calculated as the difference between the highest and lowest value of the daily variation of the temperature of the year in the period under investigation (1981-2010). The map shows the thermal continentality at 1000 m a.s.l. in the year. The resulting map has a spatial resolution of 25 m x 25 m. It was used for modelling altitudinal belts of forest vegetation.
Tranquillity Areas

Based on the "Tranquillity Map of the Swiss Plateau" and its calculated "tranquillity" values, certain recreational areas were derived. For this purpose, areas that did not fall below a certain "tranquillity" index over at least 500 contiguous grid cells (5 km²) were selected. Using this procedure, 53 large-scale areas could be derived for the Swiss Plateau that are suitable for quiet recreation.
Forest ecoregions

The map shows the Forest Ecoregions. They differ in terms of climatic factors, forest vegetation and altitudinal vegetation belts. The southernmost tip of Ticino is considered to be similar to the Plateau region regarding climatological characteristics. The Forest Ecoregions were developed for "Sustainability and success monitoring in protection forests" (Frehner et al. 2005). Detailed information is available at https://www.gebirgswald.ch/de/nais-download.html In the regions "Northern intermediate Alps free from beech", "Continental Alps" and "Southern intermediate Alps" beech does not occur, in all other regions it occurs.
Nitrogen Deposition

The time series shows the modelled total deposition of nitrogen for the years 1990, 2000, 2005, 2010, 2015 and 2020 in a resolution of 500m as a sum of wet, dry and gaseous deposition. Nationwide deposition in 2020 amounted to a total of 59'000 tonnes of nitrogen. On average, reduced nitrogen compounds (NH₃, NH₄⁺) accounted for two thirds of the deposition. This percentage can strongly vary locally depending on the amount of wet deposition and nearby emission sources. The modelled values are based on average meteorological conditions. Detailed information about the model can be found in the report Critical Loads of Nitrogen and their Exceedances. Actual nitrogen deposition can deviate from the modelled grid data. Single pixels must not be used for assessing deposition at single sites.
Geochemical soil atlas of Switzerland: Uranium

Interpolierte Uran-Konzentrationen (mg/kg Feinerde) in den Oberböden (0–20 cm) der Schweiz. Für die Ordinary Kriging Interpolationen (1 km x 1 km) wurden Messdaten von insgesamt 1'201 Standorten des Biodiversitätsmonitorings Schweiz, der Nationalen Bodenbeobachtung und des europäischen geochemischen Bodenatlas berücksichtigt. Die Element-Konzentrationen wurden in Königswasser Aufschlüssen (HNO₃:HCl:H₂O) von getrockneten (40°C), gesiebten (< 2 mm) und anschliessend gemahlenen Bodenproben mittels induktiv gekoppelter Plasma Massenspektrometrie analysiert. Standorte mit bekannter anthropogener Überprägung der Element-Konzentrationen (Punktquellen) wurden vorgängig ausgeschlossen. Bei den Ergebnissen des geochemischen Bodenatlas handelt es sich um eine Momentaufnahme der Element-Konzentrationen in den Oberböden der Schweiz (Probenahmezeitraum 2011–2015). Die interpolierten Karten dienen der verbesserten Visualisierung von Regionen mit erhöhten resp. tiefen Konzentrationen. Es können daraus jedoch keine parzellenscharfen Informationen oder definitive Rückschlüsse auf die Geologie, die Bioverfügbarkeit, die prozentualen Verteilung der geogenen und anthropogenen Quellen sowie die Belastung des Bodens abgeleitet werden. Zitat Publikation: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope, Zürich, 2023.
Verkehrsberuhigte Zonen: Begegnungszone

Dieser Datensatz beinhaltet die signalisierten Fussgängerzonen.
Die verkehrsberuhigten Zonen setzen sich aus Fussgängerzonen, Begegnungszonen und Tempo 30-Zonen zusammen. Ebenso ist der Perimeter des Verkehrskonzepts Innenstadt mit der Kernzone mit eingeschränktem Motorfahrzeugverkehr dargestellt.
Weitere Daten zu "Verkehrsberuhigte Zonen": [https://data.bs.ch/explore/?refine.tags=Verkehrsberuhigte+Zonen](https://data.bs.ch/explore/?refine.tags=Verkehrsberuhigte+Zonen)

Tags: fussganger, fussgangerzonen, geschwindigkeitsbeschrankun
Geochemical soil atlas of Switzerland: Thallium

Interpolierte Element-Konzentrationen (mg/kg Feinerde) in den Oberböden (0–20 cm) der Schweiz. Für die Ordinary Kriging Interpolationen (1 km x 1 km) wurden Messdaten von insgesamt 1'201 Standorten des Biodiversitätsmonitorings Schweiz, der Nationalen Bodenbeobachtung und des europäischen geochemischen Bodenatlas berücksichtigt. Die Element-Konzentrationen wurden in Königswasser Aufschlüssen (HNO₃:HCl:H₂O) von getrockneten (40°C), gesiebten (< 2 mm) und anschliessend gemahlenen Bodenproben mittels induktiv gekoppelter Plasma Massenspektrometrie analysiert. Standorte mit bekannter anthropogener Überprägung der Element-Konzentrationen (Punktquellen) wurden vorgängig ausgeschlossen. Bei den Ergebnissen des geochemischen Bodenatlas handelt es sich um eine Momentaufnahme der Element-Konzentrationen in den Oberböden der Schweiz (Probenahmezeitraum 2011–2015). Die interpolierten Karten dienen der verbesserten Visualisierung von Regionen mit erhöhten resp. tiefen Konzentrationen. Es können daraus jedoch keine parzellenscharfen Informationen oder definitive Rückschlüsse auf die Geologie, die Bioverfügbarkeit, die prozentualen Verteilung der geogenen und anthropogenen Quellen sowie die Belastung des Bodens abgeleitet werden. Zitat Publikation: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope; Zürich, 2023.
Catchments in karst regions

The Karst catchments layer depicts those areas where seepage water flows into a specific spring and feeds it. Catchments can occasionally overlap, namely where sections of them drain towards different karst springs simultaneously (diffluence). The karst catchments are linked to the Karst springs: when a catchment is selected, the karst springs fed by it are highlighted. The information in the categories Karst regions and Karst groundwater, respectively, is based on hydrogeological 3D models (KARSYS approach). It was developed, with the support of the cantons, by the Swiss Institute for Speleology and Karst Studies SISKA and is published by the Federal Office for the Environment FOEN.
Invasive alien plants - map of the potential area Lonicera henryi

The set of invasive alien plants shows the maps of the potential areas of 56 alien plants species present in Switzerland as well as some invasive species present in neighboring countries with the potential to reach Switzerland. The maps are the result of model-based tool to anticipate the spread of invasive alien plants listed on the Swiss Black and Watch list. The model is using occurrence data from GBIF (Global Biodiversity Information Facility), current climate data from Worldclim(1 km resolution) and occurrence data from InfoFlora combined with climate data from the WSL (100 m resolution).The maps with 100 m resolution utilize additional necessary variables including landuse and geology.
Geochemical soil atlas of Switzerland: Sulfur

Interpolierte Element-Konzentrationen (mg/kg Feinerde) in den Oberböden (0–20 cm) der Schweiz. Für die Ordinary Kriging Interpolationen (1 km x 1 km) wurden Messdaten von insgesamt 1'201 Standorten des Biodiversitätsmonitorings Schweiz, der Nationalen Bodenbeobachtung und des europäischen geochemischen Bodenatlas berücksichtigt. Die Element-Konzentrationen wurden in Königswasser Aufschlüssen (HNO₃:HCl:H₂O) von getrockneten (40°C), gesiebten (< 2 mm) und anschliessend gemahlenen Bodenproben mittels induktiv gekoppelter Plasma Massenspektrometrie analysiert. Standorte mit bekannter anthropogener Überprägung der Element-Konzentrationen (Punktquellen) wurden vorgängig ausgeschlossen. Bei den Ergebnissen des geochemischen Bodenatlas handelt es sich um eine Momentaufnahme der Element-Konzentrationen in den Oberböden der Schweiz (Probenahmezeitraum 2011–2015). Die interpolierten Karten dienen der verbesserten Visualisierung von Regionen mit erhöhten resp. tiefen Konzentrationen. Es können daraus jedoch keine parzellenscharfen Informationen oder definitive Rückschlüsse auf die Geologie, die Bioverfügbarkeit, die prozentualen Verteilung der geogenen und anthropogenen Quellen sowie die Belastung des Bodens abgeleitet werden. Zitat Publikation: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope; Zürich, 2023.
Windstorm: Gusts at return period 300 years

The Windstorm Risk Maps show peak wind gusts and their dynamic pressure and the corresponding uncertainties. The maps provide a country-wide basis for the estimation of the regional windstorm risk, however they do not replace the Dynamic Pressure Reference (Standard SIA 261 Annex E). The windstorm risk is calculated on the basis of 83 winter storm periods between 1871 and 2011 and the 20th Century Reanalysis global data. Local influences, summer storms and thunder squalls were not taken into account in the calculations. The values specified for the peak wind gusts should not, therefore, be interpreted as absolutely accurate values and do not replace any location-specific reports. The peak wind gusts are underestimated for exposed Alpine locations (e.g. Jungfraujoch), in particular.
Durchschnittliche Rente nach Typ und Geschlecht

Durchschnittliche Rente nach Typ und Geschlecht, Jahre 2001 bis 2025, jeweils im Dezember.

Die Zusatzrente für Ehepartner wurde mit der AHV-Revision abgeschafft und durch Ergänzungsleistungen ersetzt. Personen die zum Zeitpunkt der Revision bereits eine Zusatzrente bezogen haben, erhalten diese jedoch weiterhin.

(QUELLE: Bundesamt für Sozialversicherungen, AHV-Statistik)

Tags: sozialhilfe
Aquaprotect” areas of flooding: 100-year recurrence period

The areas of flooding included in “Aquaprotect” take the form of a rough overview (prepared with the aid of basic methods) of areas of Switzerland that are susceptible to damage caused by occasional and very infrequent flooding. This is intended as a rough overview of the risks and hazards, and therefore does not replace the detailed risk maps (<http://www.bafu.admin.ch/gefahrenkarten>). For example, it does not take existing flood protection measures into account, and in the event of not yet available risk maps it merely permits an approximate assessment of potential flood damage.The areas of flooding included in “Aquaprotect” concern floods in recurrence periods of 50, 100, 250 and 500 years. For example, a flood with a recurrence period of 100 years refers to a level of flooding which, viewed over a very lengthy timeframe, is reached on average once every 100 years. The fact that a given area is not included in “Aquaprotect” does not mean that there is no risk of flooding in that area. Due to the simplified method that is applied, only a rough overview is provided. At more detailed scales than 1:50,000, areas susceptible to flooding are only depicted with the aid of shading. The aim here is to avoid misinterpretation due to insufficiently accurate depiction.
Monthly rainfall erosivity (R-factor) maps of Switzerland in MJ mm ha⁻¹ h⁻¹ month⁻¹, May

<p>Monthly rainfall erosivity maps (R-factor maps) of Switzerland with a spatial resolution of 100 m. The maps show the spatial and seasonal variability of rainfall erosivity in MJ mm ha⁻¹ h⁻¹ month⁻¹. Light shades of blue indicate a low erosive impact of rainfall and dark shades a high impact.</p> <p>The monthly R-factors are based on precipitation measurements from 87 automatic gauging stations with measurement intervals of 10 minutes (average measuring period of 19.5 years per station). The stations cover all agricultural zones in Switzerland. To exclude the influence of snow, temperatures are also recorded at an hourly resolution for 71 stations or are derived from the nearest station.</p> <p>A comparison of the 12 monthly R-factor maps shows that the summer months (June, July and August) have the highest rainfall erosivity values during the year. The Southern Alps (canton of Ticino), the mountain zones of the Northern Alps and parts of the valley zone have particularly high R-factors in this period. A proportion of 62% of Switzerland's annual rainfall erosivity is recorded between June and September. Identifying regions and periods in which rainfall with an increased erosive impact occurs enables targeted erosion control and a better understanding of the dynamics of erosion processes over the course of a year.</p> The development of monthly rainfall erosivity maps of Switzerland is described in detail in 'Regionalization of monthly rainfall erosivity patterns in Switzerland' by Schmidt et al. (Hydrology and Earth System Sciences: 20. 2016. pp. 4359–4373).
Residual flow map of Switzerland: catchment

The Federal Act of 24 January 1991 on the Protection of Water against Pollution (LPEP) and its provisions on residual flows came into force on November 1, 1992 in Kraft getreten. Under Article 80 ff LPEP, remedial measures must be taken, where possible, on existing residual flows by order of the authorities. The first step in the remedial process for cantons is to build an inventory of existing water catchments and submit it to the federal government. Cantons evaluate the indexed water catchments and decide whether and how necessary it is to take remedial actions. They record the results of their analysis and submit the report to the federal government. In order to review enforcement of the LPEP as concerns residual flows / remedial measures and provide information to the public and other interested bodies, the data on the water catchments submitted by the cantons is presented in a national residual flow map (Scale 1 : 200,000).
Geochemical soil atlas of Switzerland: Iron

Interpolierte Element-Konzentrationen (mg/kg Feinerde) in den Oberböden (0–20 cm) der Schweiz. Für die Ordinary Kriging Interpolationen (1 km x 1 km) wurden Messdaten von insgesamt 1'201 Standorten des Biodiversitätsmonitorings Schweiz, der Nationalen Bodenbeobachtung und des europäischen geochemischen Bodenatlas berücksichtigt. Die Element-Konzentrationen wurden in Königswasser Aufschlüssen (HNO₃:HCl:H₂O) von getrockneten (40°C), gesiebten (< 2 mm) und anschliessend gemahlenen Bodenproben mittels induktiv gekoppelter Plasma Massenspektrometrie analysiert. Standorte mit bekannter anthropogener Überprägung der Element-Konzentrationen (Punktquellen) wurden vorgängig ausgeschlossen. Bei den Ergebnissen des geochemischen Bodenatlas handelt es sich um eine Momentaufnahme der Element-Konzentrationen in den Oberböden der Schweiz (Probenahmezeitraum 2011–2015). Die interpolierten Karten dienen der verbesserten Visualisierung von Regionen mit erhöhten resp. tiefen Konzentrationen. Es können daraus jedoch keine parzellenscharfen Informationen oder definitive Rückschlüsse auf die Geologie, die Bioverfügbarkeit, die prozentualen Verteilung der geogenen und anthropogenen Quellen sowie die Belastung des Bodens abgeleitet werden. Zitat Publikation: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope; Zürich, 2023.
Mean daily temperature high in July, period 2070-2099, Scenario RCP 4.5

Mean daily temperature high in July (period 2070-2099). The temperature increase of the climate scenario was added to the map «Air temperature July 1981-2010». Among the representative concentration pathways, RCP 4.5 with the model combination SMHI-RCA_MPIESM_EUR44 was selected as a projection for moderate climate change (NCCS 2018; Provision of the data by Remund et al. 2020) to calculate the temperature increase in the future. The resulting map has a spatial resolution of 25 m x 25 m. It was used for modelling altitudinal belts of forest vegetation.
Anzahl invalider Rentner/innen nach Invaliditätsursache

Anzahl invalider Rentner/innen an der Bevölkerung nach Invaliditätsursache,  1995 bis 2025, jeweils im Monat Dezember.

(QUELLE: Bundesamt für Sozialversicherungen, IV-Statistik)

Tags: invalidenversicherung, sozialhilfe
NAQUA-QUANT Monitoring sites (NAQUA National groundwater monitoring)

Groundwater is the result of the percolation of rainfall and the infiltration of river water. Groundwater levels and spring discharges therefore respond – though possibly with a delay – to precipitation events and dry spells. The state and variation of groundwater and spring discharges are recorded within the framework of the QUANT module of the NAQUA National Groundwater Monitoring. The monitoring network of the QUANT module consists of some 100 monitoring sites and is operated by the FOEN in close collaboration with cantonal authorities. Source: NAQUA National Groundwater Monitoring, Federal Office for the Environment.
Monthly soil erosion risk maps for Swiss permanent grassland, with average soil loss in tons/(ha*month), April

Monthly soil erosion risk maps for Swiss permanent grassland with a spatial resolution of 100m. The maps show the average soil loss in tonnes per hectare and month. Shades of green, yellow and red mean a low, average and high risk of erosion, respectively.The monthly soil erosion risk maps were calculated using the Revised Universal Soil Loss Equation (RUSLE). For this RUSLE application, the monthly dynamic of the rainfall erosivity factor (R-factor) and cover and management factor (C-factor) was considered as follows: A(month)= R(month)*K*C(month)*L*S*P where A(month) is the soil loss in tons per hectare and month and R(month) and C(month) are the monthly R-factor (MJ mm ha⁻¹ h⁻¹ month⁻¹) and C-factor (dimensionless). The other erosion factors are soil erodibility (K-factor), slope length (L-factor), slope steepness (S-factor) and support practices (P-factor). The RUSLE factors were tailored to the specific environmental conditions of Swiss permanent grassland. The P-factor was included in the calculation as a constant with value 1 due to a lack of spatial information on grazing management and its effect on soil erosion.
Monthly rainfall erosivity (R-factor) maps of Switzerland in MJ mm ha⁻¹ h⁻¹ month⁻¹, September

<p>Monthly rainfall erosivity maps (R-factor maps) of Switzerland with a spatial resolution of 100 m. The maps show the spatial and seasonal variability of rainfall erosivity in MJ mm ha⁻¹ h⁻¹ month⁻¹. Light shades of blue indicate a low erosive impact of rainfall and dark shades a high impact.</p> <p>The monthly R-factors are based on precipitation measurements from 87 automatic gauging stations with measurement intervals of 10 minutes (average measuring period of 19.5 years per station). The stations cover all agricultural zones in Switzerland. To exclude the influence of snow, temperatures are also recorded at an hourly resolution for 71 stations or are derived from the nearest station.</p> <p>A comparison of the 12 monthly R-factor maps shows that the summer months (June, July and August) have the highest rainfall erosivity values during the year. The Southern Alps (canton of Ticino), the mountain zones of the Northern Alps and parts of the valley zone have particularly high R-factors in this period. A proportion of 62% of Switzerland's annual rainfall erosivity is recorded between June and September. Identifying regions and periods in which rainfall with an increased erosive impact occurs enables targeted erosion control and a better understanding of the dynamics of erosion processes over the course of a year.</p> The development of monthly rainfall erosivity maps of Switzerland is described in detail in 'Regionalization of monthly rainfall erosivity patterns in Switzerland' by Schmidt et al. (Hydrology and Earth System Sciences: 20. 2016. pp. 4359–4373).
Points fixes altimétriques catégorie 3

Points fixes altimétriques de la mensuration officielle catégorie 3 (PFA3). Art. 46 à 48 de l'OTEMO. Ils sont matérialisés durablement sur le terrain, généralement par des repères scellés horizontalement ou verticalement et portant un numéro. Leurs fiches signalétiques sont disponibles sous forme de pdf à la Direction de l'information du territoire - Mensuration officielle. Toutes personnes à l'origine de travaux susceptibles de porter atteinte sous quelque forme que ce soit aux points fixes et aux signes de repérage, sont tenues d'en informer préalablement la Direction de l'information du territoire - Mensuration officielle et de suivre ses instructions. Loi cantonale sur les repères de la mensuration cadastrale E 1 46 article 4. Par ailleurs, toutes personnes constatant l'absence ou une détermination erronée d'un point sont priées d'en informer la Direction de l'information du territoire - Mensuration officielle afin de garantir l'intégrité du réseau.
Aménagements cyclables

La couche des aménagements cyclables recense tous les éléments construits ou matérialisés délimitant l'espace réservé au cyclistes sur la voie publique. Ces données ne doivent pas être confondues avec les itinéraires vélos, tels qu'ils apparaissent sur la carte Vélo. Elle est constituée des: - pistes cyclables (séparées physiquement de la chaussée), - bandes cyclables (marquages sur la chaussée), - sas cyclistes aux feux rouges, - contresens cyclables, - etc. Les aménagements transports en commun ouverts aux 2 roues ne sont pas présents dans cette couche, mais figurent dans la couche "AMENAGEMENTS TC". La plupart des modifications de ces aménagements font l'objet d'une approbation d'un plan de marquage, qui servent également à la mise à jour des données. La ville de Genève fournit certains aménagements spécifiques, échappant à cette règle.